# bib

id: giw-34
author: Carpenter, Kenneth
date: 2018
pages: 9
extension: .pdf
mime: application/pdf
words: 4481
sentence: 180
flesch: 51
cache: cache/giw-34.pdf
txt: txt/giw-34.txt
title:
  Soft-bodied fossil of a lizard from the Parachute Creek Member, Green River Formation (Eocene), Utah

summary:
  Soft-bodied fossil of a lizard from the Parachute Creek Member, Green River Formation (Eocene), Utah GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association ISSN 2380-7601 Volume 5 2018 © 2018 Utah Geological Association. Soft-Bodied Fossil of a Lizard From the Parachute Creek Member, Green River Formation (Eocene), Utah Kenneth Carpenter Prehistoric Museum, Utah State University Eastern, 155 Main St., Price, UT 84501; and Museum of Natural History, University of Colorado, Boulder, CO 80302; Ken.Carpenter@usu.edu Citation for this article.


id: giw-39
author: Carpenter, Kenneth; Itano, Wayne
date: 2019
pages: 8
extension: .pdf
mime: application/pdf
words: 3780
sentence: 130
flesch: 43
cache: cache/giw-39.pdf
txt: txt/giw-39.txt
title:
  Taxonomic validity of Petalodus ohioensis (Chondrichthyes, Petalodontidae) based on a cast of the lost holotype

summary:
  BASED ON A CAST OF THE LOST HOLOTYPE Kenneth Carpenter and Wayne M. Itano GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association ISSN 2380-7601 Production Cover Design and Desktop Publishing Douglas A. Sprinkel Cover Two views of a cast of the long-lost holotype of Petalodus ohioensis Safford, 1853 and hypo- thetic restoration of the shark. 801.364.6613 Outreach Greg Nielson gnielson@weber.edu 801.626.6394 Membership Rick Ford rford@weber.edu 801.626.6942 Public Education Paul Jewell pwjewell@mines.utah.edu 801.581.6636 Matt Affolter gfl247@yahoo.com Publications Paul Inkenbrandt paulinkenbrandt@utah.gov 801.537.3361 Publicity Paul Inkenbrandt paulinkenbrandt@utah.gov 801.537.3361 Social/Recreation Roger Bon rogerbon@xmission.com 801.942.0533 AAPG House of Delegates 2017–2020 Term Tom Chidsey tomchidsey@utah.gov 801.537.3364 State Mapping Advisory Committe UGA Representative Jason Blake blake-j@comcast.net 435.658.3423 UGA Newsletter Newsletter Editor Bill Lund uga.newsletter@gmail.com 435.590.1338 UGA Website www.utahgeology.org Webmasters Paul Inkenbrandt paulinkenbrandt@utah.gov 801.537.3361 Earthquake Safety Committe Chair Grant Willis gwillis@utah.gov 801.537.3355 Douglas A. Sprinkel Utah Geological Survey 801.391.1977 GIW@utahgeology.org Bart J. Kowallis Brigham Young University 801.422.2467 bkowallis@gmail.com Thomas C. Chidsey, Jr. Utah Geological Survey 801.537.3364 tomchidsey@utah.gov Steven Schamel GeoX Consulting, Inc. 801.583-1146 geox-slc@comcast.net Society of Vertebrate Paleontology Editors Kelli C. Trujillo — University of Wyoming John Foster — Utah Field House of Natural History State Park Museum Cary Woodruff — University of Toronto Octavio Mateus — Universidade Nova de Lisboa GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association Volume 6 2019 55 ABSTRACT Only a crude line drawing of the holotype tooth of the shark Petalodus ohioensis Safford, 1853 has ever been published, and the location of that specimen has long been unknown.


id: giw-36
author: Foster, John
title: A new atoposaurid crocodylomorph from the Morrison Formation (Upper Jurassic) of Wyoming, USA
date: 2018
pages: 11
extension: .pdf
mime: application/pdf
words: 4803
sentence: 161
flesch: 41
cache: cache/giw-36.pdf
txt: txt/giw-36.txt
summary:
  295 A New Atoposaurid Crocodylomorph from the Morrison Formation (Upper Jurassic) of Wyoming, USA Foster, J.R. Geology of the Intermountain West 2018 Volume 5 Clark, J.M., 2011, A new shartegosuchid crocodyliform from the Upper Jurassic Morrison Formation of western Colorado: Zo- ological Journal of the Linnean Society, v. 163, p. S152–S172. Mateus, O., 2006, Late Jurassic dinosaurs from the Morrison For- mation, the Lourinhã and Alcobaça Formations (Portugal), and the Tendaguru Beds (Tanzania)—a comparison, in Foster, J.R., and Lucas, S.G., editors, Paleontology and geology of the Upper Jurassic Morrison Formation: New Mexico Museum of Natural History and Science Bulletin 36, p. 223–231.


id: giw-20
author: Davis, Brian; Cifelli, Richard; Rougier, Guillermo
date: 2018
pages: 10
extension: .pdf
mime: application/pdf
words: 5304
sentence: 207
flesch: 44
cache: cache/giw-20.pdf
txt: txt/giw-20.txt
title:
  A preliminary report of the fossil mammals from a new microvertebrate locality in the Upper Jurassic Morrison Formation, Grand County, Utah

summary:
  Examples of high-quality preservation of small mammalian fossils from the Cisco Mammal Quarry (OMNH locality V1728, Upper Jurassic Morrison Formation, Grand County, Utah). Foster and others (2006) proposed east-west paleoenvironmen- tal partitioning of Morrison mammal localities based on facies analysis and the distribution of the possibly burrowing mammaliaform Docodon; a similar trend has been found for semiaquatic turtles and crocodyli- forms (Foster and McMullen, 2017).


id: giw-6
author: Trujillo, Kelli; Kowallis, Bart
date: 2015
pages: 10
extension: .pdf
mime: application/pdf
words: 5702
sentence: 179
flesch: 53
cache: cache/giw-6.pdf
txt: txt/giw-6.txt
title:
  Recalibrated legacy 40Ar/39Ar ages for the Upper Jurassic Morrison Formation, Western Interior, U.S.A.

summary:
  As a result, it would seem that using the new recalibrated legacy 40Ar/39Ar ages along with new 238U/206Pb ages obtained for the Morrison For- mation could be fraught with error. Rainbow Draw Uintah UT converted age uncertainties Location of top of section Long.


id: giw-28
author: Lucas, Spencer
date: 2018
pages: 15
extension: .pdf
mime: application/pdf
words: 6454
sentence: 227
flesch: 46
cache: cache/giw-28.pdf
txt: txt/giw-28.txt
title:
  The Upper Jurassic Morrison Formation in north-central New Mexico–Linking Colorado Plateau stratigraphy to the stratigraphy of the High Plains

summary:
  Overview photographs of Morrison Formation sections at Hub Canyon (A) and Hub Mesa (B). REFERENCES Anderson, O.J., and Lucas, S.G., 1995, Base of the Morrison For- mation, Upper Jurassic, of northwestern New Mexico and ad- jacent areas: New Mexico Geology, v. 17, p. 44–53.


id: giw-19
author: Jenkins, Xavier; Foster, John; Gay, Robert
title: First unambiguous dinosaur specimen from the Upper Triassic Chinle Formation in Utah
date: 2017
pages: 14
extension: .pdf
mime: application/pdf
words: 8349
sentence: 281
flesch: 45
cache: cache/giw-19.pdf
txt: txt/giw-19.txt
summary:
  Colbert, E.H., 1989, �e Triassic dinosaur Coelophysis: Museum of Northern Arizona Bulletin 57, 160 p. Dzik, J., 2003, A beaked herbivorous archosaur with dinosaur af- �nities from the early Late Triassic of Poland: Journal of Ver- tebrate Paleontology, v. 23, p. 556–574. Based on a literature review and examination of specimens available to us, we restrict the Triassic Utah dinosaurian record to �eropoda from the Chinle Formation.


id: giw-30
author: Carpenter, Kenneth; Galton, Peter
date: 2018
pages: 1
extension: .pdf
mime: application/pdf
words: 104
sentence: 5
flesch: 33
cache: cache/giw-30.pdf
txt: txt/giw-30.txt
title:
  A photo documentation of bipedal ornithischian dinosaurs from the Upper Jurassic Morrison Formation, USA

summary:
  A PHOTO DOCUMENTATION OF BIPEDAL ORNITHISCHIAN DINOSAURS FROM THE UPPER JURASSIC MORRISON FORMATION, USA Kenneth Carpenter and Peter M. Galton Theme Issue An Ecosystem We Thought We Knew— The Emerging Complexities of the Morrison Formation SOCIETY OF VERTEBRATE PALEONTOLOGY Annual Meeting, October 26 – 29, 2016 Grand America Hotel Salt Lake City, Utah, USA GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association ISSN 2380-7601 Volume 5 2018 © 2018 Utah Geological Association.


id: giw-33
author: Tschopp, Emanuel; Brinkman, Daniel; Henderson, Jaime; Turner, Mary Ann; Mateus, Octávio
date: 2018
pages: 20
extension: .pdf
mime: application/pdf
words: 10099
sentence: 296
flesch: 40
cache: cache/giw-33.pdf
txt: txt/giw-33.txt
title:
  Considerations on the replacement of a type species in the case of the sauropod dinosaur Diplodocus Marsh, 1878

summary:
  YPM VP.001920, the holotype of the type spe- cies of Diplodocus, D. longus Marsh, 1878, was briefly described by Marsh (1878) and reassessed by McIn- tosh and Carpenter (1998). Whereas it is true that Tschopp and others (2015) found YPM VP.001920 to belong to the genus Diplod- ocus, it is also true that highly incomplete specimens like YPM VP.001920 are more prone to phylogenetic instability (Wilkinson, 1995; Wiens, 2006; Butler and Upchurch, 2007).


id: giw-26
author: McHugh, Julia
date: 2018
pages: 11
extension: .pdf
mime: application/pdf
words: 4785
sentence: 180
flesch: 38
cache: cache/giw-26.pdf
txt: txt/giw-26.txt
title:
  Evidence for niche partitioning among ground-height browsing sauropods from the Upper Jurassic Morrison Formation of North America

summary:
  However, this mesial increase in tooth replacement po- sitions may not be characteristic of all sauropods, for example in the titanosaur Euhelopus zdanskyi, the max- imum number of tooth replacement positions is located within the maxilla and not the premaxilla (Poropat and Figure 2. The high number of replacement teeth in a close relative to the contemporaneous Diplodocus provides evidence for niche partitioning among the contemporary ground-height browsing diplodocid sauropods of the Late Jurassic Period in North America.


id: giw-41
author: Gee, Carole; Sprinkel, Douglas; Bennis, Mary Beth; Gray, Dale
date: 2019
pages: 18
extension: .pdf
mime: application/pdf
words: 10296
sentence: 367
flesch: 55
cache: cache/giw-41.pdf
txt: txt/giw-41.txt
title:
  Silicified logs of Agathoxylon hoodii (Tidwell et Medlyn) comb. nov. from Rainbow Draw, near Dinosaur National Monument, Uintah County, Utah, USA, and their implications for araucariaceous conifer forests in the Upper Jurassic Morrison Formation

summary:
  In the single specimen of Agathoxylon hoodii wood from its type locality on Mt. Ellen (Tidwell and Medlyn, 1993), the resin plugs are so plentiful in the rays that it is difficult to observe the crossfield pitting in the ray cells; many axial tracheids in the holotype also contain resin plugs. If the Morrison trees with Agathoxylon hoodii wood were similar in habit to living Araucaria spp., they would have also formed forests, especially given the optimal growth conditions in the warm, humid, climatically equable, water-unlimited environment.


id: giw-4
author: Nieminski, Nora; Johnson, Cari
title: A guide to the bedrock geology of Range Creek Canyon, Book Cliffs, Utah
date: 2014
pages: 28
extension: .pdf
mime: application/pdf
words: 12029
sentence: 421
flesch: 54
cache: cache/giw-4.pdf
txt: txt/giw-4.txt
summary:
  Flagstaff Limestone The Flagstaff Limestone, partially equivalent to the North Horn Formation, is late Paleocene to early 9 A Guide to the Bedrock Geology of Range Creek Canyon, Book Cliffs, Utah Nieminski, N.M., and Johnson, C.L. Geology of the Intermountain West 2014 Volume 1 Eocene in age (beginning ~58 million years ago) and is exposed north of Range Creek, along the drive up Horse Canyon and at the southern end of Range Creek Canyon (figure 2; Stanley and Collinson, 1979; Wells, 1983; Franczyk and Pitman, 1991). The previous channel deposits of a migrating channel represent what comprises the sandstone cliffs in Range Creek. 12 A Guide to the Bedrock Geology of Range Creek Canyon, Book Cliffs, Utah Nieminski, N.M., and Johnson, C.L. Geology of the Intermountain West 2014 Volume 1 GEOLOGIC EVOLUTION OF PALEO- GENE STRATA OF RANGE CREEK Just as the Fremont history reveals conditions of prehistoric human life in Range Creek Canyon, the geologic layers indicate changing environmental condi- tions of the area before the canyon cut by Range Creek ever existed.


id: giw-84
author: Armour Smith, Elliott; Loewen, Mark A.; Kirkland, James I.
title: New social insect nests from the Upper Jurassic Morrison Formation of Utah
date: 2020
pages: 21
extension: .pdf
mime: application/pdf
words: 11014
sentence: 437
flesch: 46
cache: cache/giw-84.pdf
txt: txt/giw-84.txt
summary:
  Ichnofossils created by the activity of plant roots are known as rhizoliths, and they are cited as an alter- native tracemaker to reported fossil social insect nests (Genise, 2016). These findings demonstrate a new occurrence of social insect nest ichnofossils from the Morrison For- mation, morphologically distinct from reported so- cial insect ichnofossils both within and outside of the Morrison.


id: giw-35
author: Warnock, Jonathan; Peterson, Joseph; Clawson, Steven; Matthews, Neffra; Breithaupt, Brent
date: 2018
pages: 17
extension: .pdf
mime: application/pdf
words: 9711
sentence: 319
flesch: 46
cache: cache/giw-35.pdf
txt: txt/giw-35.txt
title:
  Close-range photogrammetry of the Cleveland-Lloyd Dinosaur Quarry, Upper Jurassic Morrison Formation, Emery County, Utah

summary:
  Final- ly, we present a “living” photogrammetric map of the quarry which contains 3D bone orientation data. Hence, bone distribution data don’t currently support bloat and float processes at Mygatt- Moore.


id: giw-31
author: Sato, Takashi; Chan, Marjorie; Ekdale, Allan
date: 2018
pages: 20
extension: .pdf
mime: application/pdf
words: 7522
sentence: 303
flesch: 44
cache: cache/giw-31.pdf
txt: txt/giw-31.txt
title:
  Trace fossils and fluvial-lacustrine ichnofacies of the Eocene Uinta and Duchesne River Formations, northern Uinta Basin, Utah

summary:
  226 Trace Fossils and Fluvial-Lacustrine Ichnofacies of the Eocene Uinta and Duchesne River Formations, Northern Uinta Basin, Utah Sato, T., Chan, M.A., and Ekdale, A.A. Geology of the Intermountain West 2018 Volume 5 Sato, T., and Chan, M.A., 2015, Fluvial facies architecture and se- quence stratigraphy of the Tertiary Duchesne River Formation, Uinta Basin, Utah, U.S.A.: Journal of Sedimentary Research, v. 85, p. 1438–1454. Sato, T., Chan, M.A., and Ekdale, A.A., 2018, Trace fossils and fluvial-lacustrine ichnofacies of the Eocene Uinta and Duchesne River Formations, north- ern Uinta Basin, Utah: Geology of the Intermountain West, v. 5, p. 209–226.


id: giw-96
author: Rowley, Peter; Biek, Robert; Hacker, David
date: 2022
pages: 13
extension: .pdf
mime: application/pdf
words: 7283
sentence: 248
flesch: 58
cache: cache/giw-96.pdf
txt: txt/giw-96.txt
title:
  Basin-range uplift and canyon cutting in 3 million years, Kingston Canyon, Piute County, southwestern Utah

summary:
  This age is in the same timeframe as the cutting of Kingston Canyon, and because the Sevier River cur- rently is only a couple hundred yards from the base of Big Rock Candy Mountain, it is reasonable to conclude that much of the dissection to create Marysvale Canyon was by the ancestral Sevier River, as the Tushar Moun- tains and the rock obstruction to Sevier Valley (beneath Marysvale Canyon) were rising along their own faults. Phonolite Hill, a rhyolite dome, erupted 5 million years ago at the bottom of Kingston Canyon.


id: giw-32
author: Carpenter, Kenneth
date: 2018
pages: 20
extension: .pdf
mime: application/pdf
words: 10503
sentence: 374
flesch: 47
cache: cache/giw-32.pdf
txt: txt/giw-32.txt
title:
  Maraapunisaurus fragillimus, N.G. (formerly Amphicoelias fragillimus), a basal Rebbachisaurid from the Morrison Formation (Upper Jurassic) of Colorado

summary:
  Anonymous, 1899, Cope collection lost: The Philadelphia Record, December 30, no. 10,166, p. 10, https://news.google.com/ newspapers?nid=QDEWnZBrHwAC&dat=18991230&print- sec=frontpage&hl=en (accessed August 29, 2018). I have previous- ly hypothesized that the specimen crumbled and was disposed of by Cope years before the collection was sold (Carpenter, 2006a, p. 134).


id: giw-69
author: Foster, John; Pagnac, Darrin; Hunt-Foster, ReBecca
date: 2020
pages: 41
extension: .pdf
mime: application/pdf
words: 18193
sentence: 690
flesch: 48
cache: cache/giw-69.pdf
txt: txt/giw-69.txt
title:
  An unusually diverse northern biota from the Morrison Formation (Upper Jurassic), Black Hills, Wyoming

summary:
  62 An Unusually Diverse Northern Biota from the Morrison Formation (Upper Jurassic), Black Hills, Wyoming Foster, J.R., Pagnac, D.C., and Hunt-Foster, R.K. Geology of the Intermountain West 2020 Volume 7 Carpenter, K., and Galton, P.M., 2018, A photo documentation of bipedal ornithischian dinosaurs from the Upper Jurassic Morrison Formation, USA: Geology of the Intermountain West, v. 5, p. 167–207. Chure, D.J., 1994, Koparion douglassi, a new dinosaur from the Morrison Formation (Upper Jurassic) of Dinosaur National Monument—the oldest troodontid (Theropoda: Manirap- tora): Brigham Young University Geology Studies, v. 40, p. 11–15.


id: giw-37
author: Carpenter, Kenneth; Lindsey, Eugene
date: 2019
pages: 32
extension: .pdf
mime: application/pdf
words: 18595
sentence: 646
flesch: 46
cache: cache/giw-37.pdf
txt: txt/giw-37.txt
title:
  Redefining the Upper Jurassic Morrison Formation in Garden Park National Natural Landmark and vicinity, eastern Colorado: Geology of the Intermountain West

summary:
  Retallack, G., 1990, Soils of the past: Boston, Unwin Hyman, 520 p. Richardson, J.L., 1987, Analysis of the sedimentary geology of the Jurassic Ralston Creek Formation as it is exposed in the vicin- ity of Cañon City, Colorado: Stillwater, Oklahoma State Uni- versity, M.S. thesis, 147 p. Rogers, J., Burchfiel, B., Abbott, E., Anepohl, J., Ewing, A., Koehnk- en, P., Novitsky-Evans, J., and Talukdars, S., 1974, Paleozoic and lower Mesozoic volcanism and continental growth in the Western United States: Geological Society of America Bulle- tin, v. 85, p. 1913–1924. Thus, the K-1 unconformity between the Morrison and overlying Lytle rests on the uppermost occurrence of the Morrison Formation mudstone-sandstone-limestone complex and beneath the blocky, cliff-forming Lytle Formation.


id: giw-38
author: Carpenter, Kenneth
date: 2019
pages: 25
extension: .pdf
mime: application/pdf
words: 13926
sentence: 531
flesch: 57
cache: cache/giw-38.pdf
txt: txt/giw-38.txt
title:
  History and geology of the Cope’s Nipple Quarries in Garden Park, Colorado—type locality of giant sauropods in the Upper Jurassic Morrison Formation

summary:
  Axtell reported to Hatcher that: “The work in Cope quarries has so far been more of a prospecting nature. The first Jurassic “Dinosaur Rush” began with the near simultaneous discovery of dinosaur bones close to the towns of Morrison and Cañon City, Colorado, in 1877 (figure 1).


id: giw-15
author: Springer, Kathleen; Pigati, Jeffrey; Scott, Eric
date: 2017
pages: 46
extension: .pdf
mime: application/pdf
words: 20399
sentence: 676
flesch: 51
cache: cache/giw-15.pdf
txt: txt/giw-15.txt
title:
  Vertebrate paleontology, stratigraphy, and paleohydrology of Tule Springs Fossil Beds National Monument, Nevada (USA)

summary:
  Earthquake Safety Committe Chair Grant Willis gwillis@utah.gov 801.537.3355 Douglas A. Sprinkel Utah Geological Survey 801.391.1977 GIW@utahgeology.org Bart J. Kowallis Brigham Young University 801.422.2467 bkowallis@gmail.com Thomas C. Chidsey, Jr. Utah Geological Survey 801.537.3364 tomchidsey@utah.gov Steven Schamel GeoX Consulting, Inc. 801.583-1146 geox-slc@comcast.net Society of Vertebrate Paleontology Editors James I. Kirkland (Editor-in-Chief) — Utah Geological Survey ReBecca Hunt-Foster — Bureau of Land Management Greg McDonald — Bureau of Land Management Martha Hayden — Utah Geological Survey Editors GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association Volume 4 2017 55 ABSTRACT Tule Springs Fossil Beds National Monument (TUSK) preserves 22,650 acres of the upper Las Vegas Wash in the northern Las Vegas Valley (Nevada, USA). De Narvaez, C., 1995, Paleohydrology and paleotopography of a Las Vegas spring: Flagstaff, Northern Arizona University, M.S. thesis, 89 p. Donovan, D.J., 1996, Hydrostratigraphy and allostratigraphy of the Cenozoic alluvium in the northwestern part of Las Vegas Val- ley, Clark County, Nevada: Las Vegas, University of Nevada– Las Vegas, M.S. thesis, 199 p. Fleck, R.J., 1970, Age and possible origin of the Las Vegas Valley shear zone, Clark and Nye Counties, Nevada [abs.]: Geological Society of America Abstracts with Programs, v. 2, no. 5, p. 333. Harrington, M.R., 1955, A new Tule Springs expedition: The Mas- terkey, v. 29, no. 4, p. 112–114.


id: giw-7
author: Grazul, Kendall; Huntoon, Jacqueline; O’Keefe, Jennifer
date: 2015
pages: 21
extension: .pdf
mime: application/pdf
words: 10164
sentence: 427
flesch: 49
cache: cache/giw-7.pdf
txt: txt/giw-7.txt
title:
  Stratigraphy and fossil plants from the Cutler Formation (Late Paleozoic) and their paleoclimatic implications, eastern Paradox Basin, Colorado

summary:
  Locations of fossil plant sites are indicated with the red box. DESCRIPTION OF PLANT FOSSIL SITES The plant fossils were described and collected from two sites (figure 3) located near the faulted contact be- tween the Cutler Formation and the Precambrian gran- ite and gneiss that formed the core of the Uncompahgre uplift of the Ancestral Rocky Mountains (figure 4).


id: giw-71
author: Carpenter, Kenneth
title: Hydraulic modeling and computational fluid dynamics of bone burial in a sandy river channel
date: 2020
pages: 26
extension: .pdf
mime: application/pdf
words: 13804
sentence: 589
flesch: 55
cache: cache/giw-71.pdf
txt: txt/giw-71.txt
summary:
  That study used casts of bones in a creek to better understand the effects of bone obstruction (not transport) to water flow and how that may influence burial. HYDRAULIC MODELING AND COMPUTATIONAL FLUID DYNAMICS OF BONE BURIAL IN A SANDY RIVER CHANNEL Kenneth Carpenter Theme Issue An Ecosystem We Thought We Knew— The Emerging Complexities of the Morrison Formation SOCIETY OF VERTEBRATE PALEONTOLOGY Annual Meeting, October 26 – 29, 2016 Grand America Hotel Salt Lake City, Utah, USA GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association ISSN 2380-7601 Production Cover Design and Desktop Publishing Douglas A. Sprinkel Cover A partial Camarasaurus skeleton about to be buried by an advancing subaquatic dune.


id: giw-72
title: Methane emissions from muds during low water-level stages of Lake Powell, southern Utah, USA
date: 2020
pages: 18
extension: .pdf
mime: application/pdf
words: 11563
sentence: 356
flesch: 48
cache: cache/giw-72.pdf
txt: txt/giw-72.txt
author:
  Malenda, Margariete; Betts, Thomas; Simpson, Wendy; Wizevich, Michael; Simpson, Edward; Sherrod, Laura

summary:
  CH4 CO2 CH4 CO2 CH4 CO2 Day 1 2 3 Max % (v/v) 91.09 3.04 93.34 4.79 80.25 7.68 They observed that CH4 fluxes increased with ini- tially falling water levels (0 to 20 cm depth) and then a decrease in fluxes upon further falling water levels (20 to 50 cm depth).


id: giw-13
author: Titus, Alan; Eaton, Jeffrey; Sertich, Joseph
date: 2016
pages: 65
extension: .pdf
mime: application/pdf
words: 24963
sentence: 1119
flesch: 54
cache: cache/giw-13.pdf
txt: txt/giw-13.txt
title:
  Late Cretaceous stratigraphy and vertebrate faunas of the Markagunt, Paunsaugunt, and Kaiparowits plateaus, southern Utah

summary:
  DeCourten, F.L., and Russell, D.A., 1985, A specimen of Ornitho- mimus velox (Therapoda, Ornithomimidae) from the terminal Cretaceous Kaiparowits Formation of southern Utah: Journal of Paleontology, v. 59, p. 1091–1099. 266 Late Cretaceous Stratigraphy and Vertebrate Faunas of the Markagunt, Paunsaugunt, and Kaiparowits Plateaus, Southern Utah Titus, A.L., Eaton, J.G., and Sertich, J. Geology of the Intermountain West 2016 Volume 3 Gates, T.A., Lund, E.K., Boyd, C.A., DeBlieux, D.D., Titus, A.L., Evans, D.C., Getty, M.A., Kirkland, J.I., and Eaton, J.G., 2013, Ornithopod dinosaurs from the Grand Staircase-Escalante National Monument region, Utah, and their role in paleobio- geographic and macroevolutionary studies, in Titus, A.L., and Loewen, M.A. editors, At the top of the Grand Staircase—the Late Cretaceous of southern Utah: Bloomington, Indiana Uni- versity Press, p. 237–272.


id: giw-9
author: Foster, John; McHugh, Julia; Peterson, Joseph; Leschin, Michael
date: 2016
pages: 36
extension: .pdf
mime: application/pdf
words: 13983
sentence: 486
flesch: 44
cache: cache/giw-9.pdf
txt: txt/giw-9.txt
title:
  Major bonebeds in mudrocks of the Morrison Formation (Upper Jurassic), northern Colorado Plateau of Utah and Colorado

summary:
  from the Late Jurassic of North America (Mygatt-Moore Quarry, Morrison Formation): Journal of Vertebrate Paleontology, v. 31, p. 717–721. Foster, J.R., Hunt, R.K., and King, L.R., 2007, Taphonomy of the Mygatt-Moore Quarry, a larged dinosaur bonebed in the Upper Jurassic Morrison Formation of western Colorado Chure, D.J., Litwin, R., Hasiotis, S.T., Evanoff, E., and Carpenter, K., 2006, The fauna and flora of the Morrison Formation, in Foster, J.R., and Lucas, S.G., editors, Paleontology and geology of the Upper Jurassic Morrison Formation: New Mexico Museum of Natural History and Science Bulletin 36, p. 233–249.


id: giw-85
author: Oviatt, Charles G.
title: G.K. Gilbert and the Bonneville shoreline
date: 2020
pages: 22
extension: .pdf
mime: application/pdf
words: 11223
sentence: 367
flesch: 53
cache: cache/giw-85.pdf
txt: txt/giw-85.txt
summary:
  Johnson, J.W., 1956, Dynamics of nearshore sediment movement: American Association of Petroleum Geologists Bulletin, v. 40, p. 2211–2232. Laabs, B.J., Oviatt, C.G., and Jewell, P.W., 2019, Cosmogenic 10Be exposure dating of erosional landforms of the Provo shore- line, Lake Bonneville basin [abs.]: Geological Society of America Abstracts with Programs, v. 51, no. 5, doi:10.1130/ abs/2019AM-337212. Oviatt, C.G., 1991, Quaternary geology of the Black Rock Desert, Millard County, Utah: Utah Geological and Mineral Survey Special Studies 73, 23 p. Oviatt, C.G., 1997, Lake Bonneville fluctuations and global climate change: Geology, v. 25, p. 155–158.


id: giw-8
author: Britt, Brooks; Chure, Daniel
date: 2016
pages: 34
extension: .pdf
mime: application/pdf
words: 16448
sentence: 685
flesch: 55
cache: cache/giw-8.pdf
txt: txt/giw-8.txt
title:
  Rise of the Erg—Paleontology and paleoenvironments of the Triassic-Jurassic transition in Northeastern Utah

summary:
  Sprinkel and others (2011) propose using the term Nugget Sandstone in ar- eas where the Kayenta Formation, a fluvial unit present between the Wingate and Navajo Sandstones farther south, is absent. Nugget Sandstone ex- posures at Stop 1, Cub Creek petroglyph site.


id: giw-3
author: Clark, David; Derenthal, Drew ; Kowallis, Bart; Ritter, Scott
title: The major pre-Mississippian unconformity in Rock Canyon, central Wasatch Range, Utah
date: 2014
pages: 7
extension: .pdf
mime: application/pdf
words: 3031
sentence: 101
flesch: 42
cache: cache/giw-3.pdf
txt: txt/giw-3.txt
summary:
  The major pre-Mississippian unconformity in Rock Canyon, central Wasatch Range, Utah GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association Volume 1 2014 The Major Pre-Mississippian Unconformity in Rock Canyon, Central Wasatch Range, Utah David L. Clark1,, Drew Derenthal2, Bart J. Kowallis2, and Scott M. Ritter2 1Department of Geosciences, University of Wisconsin, Madison, WI; dlclark15@gmail.com 2Department of Geological Sciences, Brigham Young University, Provo, UT © 2014 Utah Geological Association. Utah Geological Association formed in 1970 from a merger of the Utah Geological Society, founded in 1946, and the Intermountain Association of Geologists, founded in 1949.


id: giw-29
date: 2018
pages: 37
extension: .pdf
mime: application/pdf
words: 27089
sentence: 674
flesch: 47
cache: cache/giw-29.pdf
txt: txt/giw-29.txt
author:
  Zuchuat, Valentin; Sleveland, Arve; Sprinkel, Douglas; Rimkus, Algirdas; Braathen, Alvar; Midtkandal, Ivar

title:
  New Insights on the Impact of Tidal Currents on a Low-gradient, Semi-enclosed, Epicontinental Basin—the Curtis Formation, East-central Utah, USA

summary:
  (B) Green dots represent visited localities where the Curtis Formation crops out, where- as red dots (not numbered) illustrate its absence. The overlying tidally influenced Curtis Formation of Early Oxfordian age (Kreisa and Moiola, 1986; Ca- puto and Pryor, 1991; Wilcox and Currie, 2008; Ogg and others, 2016) was first formally defined by Gilluly and Reeside (1928), and its type section of Curtis Point is located about 5.3 km south of Dry Mesa, along the northeastern margin of the San Rafael Swell (UTM coordinates: 12S 547430/4331169).


id: giw-18
author: Hudson, Samuel; Tuttle, Trevor; Wood, Matthew
date: 2017
pages: 17
extension: .pdf
mime: application/pdf
words: 9102
sentence: 282
flesch: 45
cache: cache/giw-18.pdf
txt: txt/giw-18.txt
title:
  Source within the seal—Distribution and implications of organic shale-bearing stringers within the Onion Creek diapir, northern Paradox Basin, Utah

summary:
  Hydrocarbon staining of strata within the Onion Creek diapir is similar in ap- pearance to other instances of hydrocarbon migration associated with salt diapirs, such as documented within and proximal to the La Popa diapir in Mexico (Hud- son and Hanson, 2010). Callot, J.P., Letouzey, J., and Rigollet, C., 2006, Stringers evolution in salt diapirs, insight from analogue models [abs.]: American Asso- ciation of Petroleum Geologists International Conference and Ex- hibition, Perth, Australia, Search and Discovery Article #90061.


id: giw-14
author: Murphey, Paul; Townsend, K.E.; Friscia, Anthony; Westgate, James; Evanoff, Emmett; Gunnell, Gregg
date: 2017
pages: 55
extension: .pdf
mime: application/pdf
words: 32890
sentence: 1192
flesch: 55
cache: cache/giw-14.pdf
txt: txt/giw-14.txt
title:
  Paleontology and stratigraphy of Middle Eocene rock units in the southern Green River and Uinta Basins, Wyoming and Utah

summary:
  Murphey, P.C., and Townsend, K.E., 2005, Ecological diversity analysis applied to facies faunas in the Twin Buttes Member, middle Eocene Bridger Formation, southwestern Wyoming, USA [abs]: Society of Vertebrate Paleontology, v. 25, no. 3, p. 95A. Nichols, D.J., 1987, Palynology of the Vermillion Creek coal bed and associated strata: U.S. Geological Survey Professional Paper 1314-D, p. 47–73. This visit infuriat- ed Marsh, who, at the time, considered the Green River Basin and Bridger Formation his exclusive fossil-col- lecting territory.


id: giw-94
author: Phillips, Stephen; Hudson, Hudson
date: 2022
pages: 29
extension: .pdf
mime: application/pdf
words: 14100
sentence: 533
flesch: 48
cache: cache/giw-94.pdf
txt: txt/giw-94.txt
title:
  The Upper Cretaceous Rock Springs Formation of northwest Colorado: A previously undescribed key deltaic outcrop

summary:
  Stratigraphy The name “Rock Springs Formation” has its origins in a report by Schultz (1920) where coal-rich continen- tal deposits of the Rock Springs uplift were termed the “Rock Springs coal group.” Sears (1925) first used the name “Rock Springs Formation” and Burger (1965) es- tablished the eastern flank of the Rock Springs uplift as the type locality for the formation.


id: giw-40
author: Sprinkel, Douglas; Bennis, Mary Beth; Gray, Dale; Gee, Carole
date: 2019
pages: 23
extension: .pdf
mime: application/pdf
words: 11764
sentence: 395
flesch: 54
cache: cache/giw-40.pdf
txt: txt/giw-40.txt
title:
  Stratigraphic Setting of Fossil Log Sites in the Morrison Formation (Upper Jurassic) near Dinosaur National Monument, Uintah County, Utah, USA

summary:
  Morgan, S.K., Lindsay, B.W., and Hoffman, A.P., 2012, Geologic trail guide for Escalante State Park, Utah, in Anderson, P.B., and Sprinkel, D.A., editors, Geologic road, trail, and lake guides of Utah’s parks and monuments: Utah Geological As- sociation Publication 29 (third edition), p. 8. 801.364.6613 Outreach Greg Nielson gnielson@weber.edu 801.626.6394 Membership Rick Ford rford@weber.edu 801.626.6942 Public Education Paul Jewell pwjewell@mines.utah.edu 801.581.6636 Matt Affolter gfl247@yahoo.com Publications Paul Inkenbrandt paulinkenbrandt@utah.gov 801.537.3361 Publicity Paul Inkenbrandt paulinkenbrandt@utah.gov 801.537.3361 Social/Recreation Roger Bon rogerbon@xmission.com 801.942.0533 AAPG House of Delegates 2017–2020 Term Tom Chidsey tomchidsey@utah.gov 801.537.3364 State Mapping Advisory Committe UGA Representative Jason Blake blake-j@comcast.net 435.658.3423 UGA Newsletter Newsletter Editor Bill Lund uga.newsletter@gmail.com 435.590.1338 UGA Website www.utahgeology.org Webmasters Paul Inkenbrandt paulinkenbrandt@utah.gov 801.537.3361 Earthquake Safety Committe Chair Grant Willis gwillis@utah.gov 801.537.3355 Douglas A. Sprinkel Utah Geological Survey 801.391.1977 GIW@utahgeology.org Bart J. Kowallis Brigham Young University 801.422.2467 bkowallis@gmail.com Thomas C. Chidsey, Jr. Utah Geological Survey 801.537.3364 tomchidsey@utah.gov Steven Schamel GeoX Consulting, Inc. 801.583-1146 geox-slc@comcast.net Society of Vertebrate Paleontology Editors Kelli C. Trujillo — University of Wyoming John Foster — Utah Field House of Natural History State Park Museum Cary Woodruff — University of Toronto Octavio Mateus — Universidade Nova de Lisboa GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association Volume 6 2019 61 ABSTRACT The outcrop belt of the Upper Jurassic Morrison Formation in the northeastern Uinta Basin and southeastern flank of the Uinta Mountains is particularly rich in dinosaurian and non-dinosaurian faunas, as well as in fossil plants.


id: giw-68
date: 2020
pages: 33
extension: .pdf
mime: application/pdf
words: 31172
sentence: 692
flesch: 52
cache: cache/giw-68.pdf
txt: txt/giw-68.txt
author:
  Jensen, Michael; Kowallis, Bart; Christiansen, Eric; Webb, Casey; Dorais, Michael; Sprinkel, Douglas; Jicha, Brian

title:
  Fallout tuffs in the Eocene Duchesne River Formation, northeastern Utah—ages, compositions, and likely source

summary:
  Allanite in Duchesne River Formation tuffs has Ti concentrations between 0.0 to 0.06 apfu compared with 0.06 to 0.12 for allanite in the Toba Tuff and 0.16 and 0.19 for the Bishop Tuff. In this regard, allanite from Duchesne River Formation tuffs contains more Al than the other silicic tuffs used for comparison (>1.8 vs. 1.2–1.6 apfu).


id: giw-147
author: Judge, Shelley; Elliot, David; Wilson, Terry; Foland, Kenneth
title: The Wasatch monocline, central Utah—a pre-Basin and Range extensional structure
date: 2024
pages: 21
extension: .pdf
mime: application/pdf
words: 11260
sentence: 371
flesch: 48
cache: cache/giw-147.pdf
txt: txt/giw-147.txt
summary:
  The timing of formation of the monocline and its tectonic significance has been the subject of debate because it is an anomalous structural style for central Utah. Judge, S.A., Elliot, D.H., Wilson, T.J., and Foland, K.A., 2024, The Wasatch monocline, central Utah—a pre-Basin and Range extensional structure: Geology of the Intermountain West, v. 11, p. 1–19, https://doi.org/10.31711/giw.v11.pp1-19.


id: giw-42
author: Woodruff, D.
title: What factors influence our reconstructions of Morrison Formation sauropod diversity?
date: 2019
pages: 22
extension: .pdf
mime: application/pdf
words: 12407
sentence: 436
flesch: 40
cache: cache/giw-42.pdf
txt: txt/giw-42.txt
summary:
  Descriptions of imma- ture Morrison Formation sauropods (Gilmore, 1925; Carpenter and McIntosh, 1994; Foster, 1995; Perhaps the predominance of small- er body sized Morrison Formation sauropods, such as Camarasaurus (approximately 12,530 kg for C. grandis; specimen GMNH 101 – this analysis) versus the rarity of larger body sized taxa, such as Supersaurus (36,287 kg; Lovelace and others, 2008) may be analogous to the pattern seen in the African savanna.


id: giw-149
author: Marsh, Adam; De Blieux, Donald; Kirkland, James
title: The first dinosaur postcranial body fossils from the Lower Jurassic Kayenta Formation of Utah
date: 2024
pages: 15
extension: .pdf
mime: application/pdf
words: 8734
sentence: 239
flesch: 37
cache: cache/giw-149.pdf
txt: txt/giw-149.txt
summary:
  (A) Map of northern Arizona and southern Utah showing localities and Arches National Park, the extent of Kayenta Formation facies is shown as brown and tan; (B) Stratigraphic context of the Glen Canyon Group near Arches National Park. Donohoo-Hurley, L.L., Geissman, J.W., and Lucas, S.G., 2010, Magnetostratigraphy of the uppermost Triassic and low- ermost Jurassic Moenave Formation, Western United States—correlation with strata in the United Kingdom, Morocco, Turkey, Italy, and Eastern United States: Geolog- ical Society of America Bulletin, v. 122, p. 2005–2019, doi: 10.1130/B30136.1.


id: giw-97
author: Rowley, Peter; Biek, Robert; Hacker, David
date: 2022
pages: 14
extension: .pdf
mime: application/pdf
words: 7133
sentence: 222
flesch: 54
cache: cache/giw-97.pdf
txt: txt/giw-97.txt
title:
  An unconformity in the Pole Creek area (Sevier Plateau) west of Antimony, western Garfield County, Utah, and its bearing on the Sevier gravity slide

summary:
  Biek, R.F., Hacker, D.B., and Rowley, P.D., 2014, New constraints on the extent, age, and emplacement history of the early Mio- cene Markagunt Megabreccia, southwest Utah—the deposit of one of the world’s largest subaerial gravity slides, in MacLean, J.S., Biek, R.F., and Huntoon, J.E., editors, Geology of Utah’s far south: Utah Geological Association Publication 43, 565–598 Biek, R.F., Hacker, D.B., and Rowley, P.D., 2017, Catastrophic me- ga-scale landslide failure of large volcanic fields (Thompson Field Forums report): GSA Today, v. 27, no. 12, 435.649.4005 UGA Newsletter Newsletter Editor Bill Lund uga.newsletter@gmail.com 435.590.1338 UGA Website — www.utahgeology.org Webmaster Paul Inkenbrandt paulinkenbrandt@utah.gov 801.537.3361 Earthquake Safety Committee Chair Grant Willis gwillis@utah.gov 801.537.3355 Douglas A. Sprinkel Azteca Geosolutions 801.391.1977 GIW@utahgeology.org dsprinkel@gmail.com Bart J. Kowallis Brigham Young University 801.380.2736 bkowallis@gmail.com Steven Schamel GeoX Consulting, Inc. 801.583-1146 geox-slc@comcast.net Thomas C. Chidsey, Jr. Utah Geological Survey 801.824.0738 tomchidsey@gmail.com John R. Foster Utah Field House of Natural History State Park Museum 435.789.3799 eutretauranosuchus@ gmail.com Editors GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association Volume 9 2022 13 ABSTRACT Pole Canyon is cut into the western backslope of the Sevier Plateau of southwestern Utah, a gently-tilt- ed, block-faulted range that extends north from Bryce Canyon National Park through the eastern part of the Marysvale volcanic field.


id: giw-70
author: Kowallis, Bart; Sprinkel, Douglas; Christiansen, Eric; Steed, Skylor; Wheatley, David
date: 2020
pages: 30
extension: .pdf
mime: application/pdf
words: 20248
sentence: 529
flesch: 51
cache: cache/giw-70.pdf
txt: txt/giw-70.txt
title:
  Rhyolite ignimbrite boulders and cobbles in the Middle Jurassic Carmel Formation of Utah and Arizona—age, composition, transport, and stratigraphic setting

summary:
  CONCLUSIONS The source for coarse volcanic detritus in the Mid- dle Jurassic Carmel Formation of southern Utah has been problematic. X-ray fluorescence analyses (major and trace ele- ments) for Carmel Formation clasts.


id: giw-83
author: Chidsey, Thomas C.; Eby, David; Sprinkel, Douglas
date: 2020
pages: 40
extension: .pdf
mime: application/pdf
words: 15752
sentence: 696
flesch: 50
cache: cache/giw-83.pdf
txt: txt/giw-83.txt
title:
  A tale of two breccia types in the Mississippian Leadville Limestone of Lisbon and other fields, Paradox Basin, southeastern Utah

summary:
  Morgan, C.D., 1993, Mississippian Leadville Limestone, in Hjellm- ing, C.A., editor, Atlas of major Rocky Mountain gas reservoirs: New Mexico Bureau of Mines and Mineral Resources, p. 94. Thus, tar- geting Leadville Limestone areas for potential hydrothermal dolomite and enhanced reservoir quality due to hydrofracturing may require an aquifer below as a necessary ingredient (i.e., the Devonian McCracken Sandstone).


id: giw-27
author: Carpenter, Kenneth; Ottinger, Lin
title: Permo-Pennsylvanian shark teeth from the Lower Cutler beds near Moab, Utah
date: 2018
pages: 14
extension: .pdf
mime: application/pdf
words: 7475
sentence: 289
flesch: 55
cache: cache/giw-27.pdf
txt: txt/giw-27.txt
summary:
  Petalodus tooth illustrated by Portlock (1843, plate 14, figure 10) a few years after Agassiz’s descriptions (scale unknown) in (W) labial view. Possible serial stacking of replacement teeth in lat- eral view (A) of Petalodus to explain the convexo-concave crown (A, lower teeth only), versus the dental occlusion (B, lower and upper teeth) advocated by Lucas and others (2011) for the same convexo-concave feature.


id: giw-104
author: Henderson, Stacy; Rivera, Tiffany; Lippert, Peter; Jicha, Brian
date: 2022
pages: 18
extension: .pdf
mime: application/pdf
words: 10523
sentence: 373
flesch: 56
cache: cache/giw-104.pdf
txt: txt/giw-104.txt
title:
  Geomorphic and tectonic development of Swan Valley, southeast Idaho, since the eruption of the Basalt of Antelope Flat—new 40Ar/39Ar, geochemical, and paleomagnetic data

summary:
  Email inquiries to GIW@utahgeology.org. GEOMORPHIC AND TECTONIC DEVELOPMENT OF SWAN VALLEY, SOUTHEAST IDAHO, SINCE THE ERUPTION OF THE BASALT OF ANTELOPE FLAT—NEW 40AR/39AR, GEOCHEMICAL, AND PALEOMAGNETIC DATA Stacy Henderson, Tiffany Rivera, Peter C. Lippert, and Brian R. Jicha GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association ISSN 2380-7601 Production Cover Design and Desktop Publishing Douglas A. Sprinkel Cover The Pleistocene Basalt of Antelope Flat dammed the Snake River in Swan Valley, southeast Idaho, producing hyaloclastite visible along US Highway 26. For example, the South Fork of the Boise River was dammed multiple times over a 2-million-year period (Howard and others, 1982) and basalts erupted from McKinney Butte dammed the Snake River near Bliss, Idaho, generating a lava del- ta with abundant pillow basalts (Malde, 1971,1982).


id: giw-127
author: Judge, Shelley; Werthmann, Emmett; Millan, Cristina; Braunagel, Michael; Maletic, Erica
title: Utah geosite—the Salina Canyon unconformity, a classic example of missing time
date: 2023
pages: 17
extension: .pdf
mime: application/pdf
words: 8753
sentence: 344
flesch: 50
cache: cache/giw-127.pdf
txt: txt/giw-127.txt
summary:
  Department of the Interior U.S. Geographical and Geological Survey of the Rocky Mountain Region, 408 p. Fouch, T.D., Lawton, T.F., Nichols, D.J., Cashion, W.B., and Cobban, W.A., 1982, Chart showing preliminary correla- tion of major Albian to middle Eocene rock units from the Sanpete Valley in central Utah to the Book Cliffs in eastern Utah, in Nielson, D.L., editor, Overthrust belt of Utah: Utah Geological Association Publication 10, p. 267–272. Spieker, E.M., 1949, The transition between the Colorado Plateaus and the Great Basin in central Utah, Guidebook to the geology of Utah 4: Utah Geological Society, 106 p. Sprinkel, D.A., Weiss, M.P., Fleming, R.W., and Waanders, G.L., 1999, Redefining the Lower Cretaceous stratigra- phy within the central Utah foreland basin: Utah Geo- logical Survey Special Study 97, 21 p. Sprinkel, D.A., Doelling, H.H., Kowallis, B.J., Waanders, G., and Kuehne, P.A., 2011, Early results of a study of Middle Jurassic strata in the Sevier fold and thrust belt, Utah, in Sprinkel, D.A., Yonkee, W.A., and Chidsey, T.C., Jr., edi- tors, Sevier thrust belt—northern and central Utah and adjacent areas: Utah Geological Association Publication 40, p. 151–172.


id: giw-124
author: Mueller, Erich; Sudweeks, Garrett; Ashton, Shadrach; Olson, Micah
date: 2023
pages: 21
extension: .pdf
mime: application/pdf
words: 8929
sentence: 299
flesch: 48
cache: cache/giw-124.pdf
txt: txt/giw-124.txt
title:
  Snow drought and monsoon floods—hydrological extremes in the Cedar Valley watershed during water year 2021, southwestern Utah

summary:
  Mueller, E.R., Sudweeks, G.P., Ashston, S.A., and Olson, M.C., 2023, Snow drought and monsoon floods—hydrological extremes in the Cedar Valley watershed during water year 2021, southwestern Utah: Geology of the Intermountain West, v. 10, p. 93–111, https://doi.org/10.31711/giw.v10.pp93-111. We consid- er the March 1st through June 30th period as generally associated with snowmelt, and the July 1st through Sep- tember 30th period as reflecting monsoon floods over- printed on the baseflow.


id: giw-125
date: 2023
pages: 19
extension: .pdf
mime: application/pdf
words: 7948
sentence: 280
flesch: 47
cache: cache/giw-125.pdf
txt: txt/giw-125.txt
author:
  Hiscock, Adam; Kleber, Emily; McKean, Adam; Erickson, Ben; McDonald, Greg; Giraud, Richard; Castleton, Jessica; Bowman, Steve

title:
  The March 2020, Mw 5.7 Magna, Utah, earthquake—documentation of geologic effects and summary of new research

summary:
  THE MARCH 2020, MW 5.7 MAGNA, UTAH, EARTHQUAKE—DOCUMENTATION OF GEOLOGIC EFFECTS AND SUMMARY OF NEW RESEARCH Adam I. Hiscock, Emily J. Kleber, Adam P. McKean, Ben A. Erickson, Greg N. McDonald, Richard E. Giraud, Jessica J. Castleton, and Steve D. Bowman Theme Issue Engineering Geology and Geohazards of Utah Utah Geological Association Annual Field Conference October 22, 2022 Salt Lake City, Utah, USA GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association ISSN 2380-7601 Production Cover Design and Desktop Publishing Douglas A. Sprinkel Cover Subsidence features on the salt flats near the Great Saltair likely caused by liquefaction from the 2020 M5.7 Magna, Utah earthquake. CONCLUSIONS Documenting ground effects from the March 18, 2020, Mw 5.7 Magna, Utah earthquake and establishing a digital clearinghouse was critical in the aftermath of the earthquake.


id: giw-17
author: Milligan, Mark; McDonald, H.
title: Shorelines and vertebrate fauna of Pleistocene Lake Bonneville, Utah, Idaho, and Nevada
date: 2017
pages: 36
extension: .pdf
mime: application/pdf
words: 16093
sentence: 631
flesch: 58
cache: cache/giw-17.pdf
txt: txt/giw-17.txt
summary:
  Nelson, M.E., and Madsen J.H., Jr., 1987, A review of Lake Bonne- ville shoreline faunas (Late Pleistocene) of northern Utah, in Kopp, R.S., and Cohenour, R.E., editors, Cenozoic geology of western Utah—sites for precious metal and hydrocarbon ac- cumulations: Utah Geological Association Publication 16, p. 319–333. O’Connor, J.E., 1993, Hydrology, hydraulics, and geomorphology of the Bonneville �ood: Geological Society of America Special Paper 274, 83 p. O’Connor, J., 2016, �e Bonneville �ood—a veritable débâcle, in Oviatt, C.G., and Shroder, J.F., Jr., editors, Lake Bonneville—a scienti�c update: Cambridge, Elsevier, p. 105–126. �e Bonneville basin has been a region of internal drainage for the past 15 m.y. and lakes of varying sizes have occupied part of the basin throughout most of this Figure 1.


id: giw-122
author: Taylor, Michael; Sroka, Steven; Carpenter, Kenneth
title: The concrete Diplodocus of Vernal—a cultural icon of Utah
date: 2023
pages: 29
extension: .pdf
mime: application/pdf
words: 15706
sentence: 567
flesch: 56
cache: cache/giw-122.pdf
txt: txt/giw-122.txt
summary:
  This table represents a synthesis of three sources of information: (1) a list maintained by Dinolab and forwarded by Brian D. Curtice, (2) James H. Madsen’s (1993) memorandum to Mary Dawson (Carnegie Museum) and Alden H. Hamlin (Utah Field House), and (3) an accounting made by Dinolab to Steve Sroka shortly after he started work at the Field House (Dinolab, 2001). Top left: Field House Museum Director G. Ernest Untermann and Staff Scientist Billie Untermann preparing concrete dorsal vertebrae (24 January 1957).


id: giw-118
author: Simpson, Edward; Wizevich, Michael; Pittinger, Dakota; Rogers, Garrett; Lazer, Kayla
date: 2022
pages: 23
extension: .pdf
mime: application/pdf
words: 9812
sentence: 400
flesch: 49
cache: cache/giw-118.pdf
txt: txt/giw-118.txt
title:
  Microbially induced sedimentary structures and the preservation of vertebrate tracks on the Colorado River delta in Lake Powell, Hite, Utah

summary:
  Destruction by wind action of the pustular mat is limited because the interior is filled with sediment as opposed to the void- like nature of blister mats. August 2021 field photographs of blister mats after partial destruction.


id: giw-82
author: Gay, Robert J.; Huttenlocker, Adam K.; Irmis, Randall B.; Stegner, M. Allison; Uglesich, Jessica
date: 2020
pages: 39
extension: .pdf
mime: application/pdf
words: 26820
sentence: 824
flesch: 40
cache: cache/giw-82.pdf
txt: txt/giw-82.txt
title:
  Paleontology of Bears Ears National Monument (Utah, USA): History of exploration, study, and designation 

summary:
  Martz, J.W., Irmis, R.G., and Milner, A.R.C., 2014, Lithostratig- raphy and biostratigraphy of the Chinle Formation (Upper Triassic) in southern Lisbon Valley, southeastern Utah, in Ma- cLean, J.S., Biek, R.F., and Huntoon, J.E., editors, Geology of Utah’s far south: Utah Geological Association Publication 43, p. 397–446. Doelling, H.H., Oviatt, C.G., and Huntoon, P.W., 1988, Salt defor- mation in the Paradox region: Utah Geological and Mineral Survey Bulletin 122, p. 1–93.


id: giw-98
author: Rowley, Peter; Hacker, David; Biek, Robert
date: 2022
pages: 15
extension: .pdf
mime: application/pdf
words: 7795
sentence: 264
flesch: 54
cache: cache/giw-98.pdf
txt: txt/giw-98.txt
title:
  A site bearing on the origin of iron deposits in the Iron Springs Mining District, Iron County, Utah

summary:
  435.649.4005 UGA Newsletter Newsletter Editor Bill Lund uga.newsletter@gmail.com 435.590.1338 UGA Website — www.utahgeology.org Webmaster Paul Inkenbrandt paulinkenbrandt@utah.gov 801.537.3361 Earthquake Safety Committee Chair Grant Willis gwillis@utah.gov 801.537.3355 Douglas A. Sprinkel Azteca Geosolutions 801.391.1977 GIW@utahgeology.org dsprinkel@gmail.com Bart J. Kowallis Brigham Young University 801.380.2736 bkowallis@gmail.com Steven Schamel GeoX Consulting, Inc. 801.583-1146 geox-slc@comcast.net Thomas C. Chidsey, Jr. Utah Geological Survey 801.824.0738 tomchidsey@gmail.com John R. Foster Utah Field House of Natural History State Park Museum 435.789.3799 eutretauranosuchus@ gmail.com Editors GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association Volume 9 2022 25 ABSTRACT The discovery of the origin of iron in the Iron Springs mining district of southwestern Utah is a story of unconventional thinking based on detailed geologic mapping. Bullock, K.C., 1970, Iron deposits of Utah: Utah Geological and Figure 7.


id: giw-101
author: Peterson, Joseph; Warnock, Jonathan; Coenen, Jason; Bills, Charles; Denoto, Mateo
date: 2022
pages: 11
extension: .pdf
mime: application/pdf
words: 5008
sentence: 169
flesch: 39
cache: cache/giw-101.pdf
txt: txt/giw-101.txt
title:
  A Review of charophytes of the Cleveland-Lloyd Dinosaur Quarry at Jurassic National Monument in the upper part of the Morrison Formation (Late Jurassic), Emery County, Utah, USA

summary:
  These observations help to characterize the depositional envi- ronment of the CLDQ, a necessary step for understand- ing its uniqueness and place in the Morrison ecosystem, while providing an ecological metric for comparison to other Morrison Formation deposits. INTRODUCTION The Cleveland-Lloyd Dinosaur Quarry (CLDQ) at Jurassic National Monument (JNM) is an Upper Juras- sic Morrison Formation fossil locality in central Utah where over 10,000 dinosaur bones have been discovered since the 1920s, including over 70 individuals of 10 dif- ferent genera of dinosaur (Gates, 2005).


id: giw-24
date: 2018
pages: 73
extension: .pdf
mime: application/pdf
words: 38157
sentence: 1238
flesch: 48
cache: cache/giw-24.pdf
txt: txt/giw-24.txt
author:
  Foster, John; Hunt-Foster, ReBecca; Gorman, Mark; Trujillo, Kelli; Suarez, Celina; McHugh, Julia; Peterson, Joseph; Warnock, Jonathan; Schoenstein, Heidi

title:
  Paleontology, taphonomy, and sedimentology of the Mygatt-Moore Quarry, a large dinosaur bonebed in the Morrison Formation, western Colorado—Implications for Upper Jurassic dinosaur preservation modes

summary:
  Hubert, J.F., Panish, P.T., Chure, D.J., and Prostak, K.S., 1996, Chemistry, microstructure, petrology, and diagenetic model of Jurassic dinosaur bones, Dinosaur National Monument, Utah: Journal of Sedimentary Research, v. 66, p. 531–547. The excavated m3 is thought to be typical of the deposit overall because it is from an area close to where large dinosaur bones have been ex- cavated.


id: giw-126
author: Chidsey, Thomas
date: 2023
pages: 78
extension: .pdf
mime: application/pdf
words: 23118
sentence: 834
flesch: 51
cache: cache/giw-126.pdf
txt: txt/giw-126.txt
title:
  Potential drilling hazards for wells targeting the Cane Creek shale, Pennsylvanian Paradox Formation, Paradox fold and fault belt, southeastern Utah and southwestern Colorado

summary:
  Chidsey, T.C., Jr., Morgan, C.D., and Eby, D.E., 2016, Chap- ter 10—Pennsylvanian Paradox Formation Paradox Ba- sin play, in Chidsey, T.C., Jr., editor, Major oil plays in https://doi.org/10.34191/OG-21 163 Potential Drilling Hazards for Wells Targeting the Cane Creek Shale, Pennsylvanian Paradox Formation, Paradox Fold and Fault Belt, Southeastern Utah and Southwestern Colorado Chidsey, T.C., Jr. Geology of the Intermountain West 2023 Volume 10 Utah and vicinity: Utah Geological Survey Bulletin 137, p. 159–206, https://doi.org/10.34191/B-137. Entrada Sandstone 60–500 sandstone well deviation due to jointing & contorted bedding, loss of circulation or water flow in porous units Carmel Formation 20–300 sandstone, siltstone, mud- stone washouts Navajo Sandstone 0–510 sandstone loss of circulation or water flow in porous units, thin limestone beds, possible carbon dioxide Kayenta Formation 60–360 sandstone loss of circulation in porous units Wingate Sandstone 70–450 sandstone loss of circulation or water flow in porous units & jointing & fracture zones Chinle Formation 150–630 mudstone, shale sticking and bit balling due to swelling clays, wash- outs, drilling problems due to contorted bedding, radioactive zones Moenkopi Formation 240–910 sandstone, siltstone, mud- stone washouts, well deviation issues Black Box Dolomite 60–160 dolomite, limestone loss of circulation in fractured zones White Rim Ss. 0–500 sandstone loss of circulation & sticking due to mudcake buildup in porous units, water flow in porous units Organ Rock Fm. 0–300 sandstone, shale washouts Elephant Canyon Fm. 1000–1200 sandstone, limestone loss of circulation in porous & fractured zones, ex- cessive bit wear due to chert Cutler Formation 900–1200 arkosic sandstone, siltstone, limestone loss of circulation or water flow in porous & frac- tured zones Honaker Trail Fm. 1600–5000 sandstone, limestone, silt- stone loss of circulation or water flow in porous & frac- tured zones, excessive bit wear due to chert, possi- ble gas-bearing zones Paradox Formation ±14,000 sandstone, siltstone, lime- stone & dolomite mudstone, shale, anhydrite, halite washouts, sticking, salt flowage, gas kicks, overpres-


id: giw-150
author: Boisvert, Colin; Bivens, Gunnar; Curtice, Brian; Wilhite, Ray; Wedel, Mathew
date: 2025
pages: 25
extension: .pdf
mime: application/pdf
words: 11377
sentence: 385
flesch: 40
cache: cache/giw-150.pdf
txt: txt/giw-150.txt
title:
  Census of currently known specimens of the Late Jurassic sauropod Haplocanthosaurus from the Morrison Formation, USA

summary:
  CENSUS OF CURRENTLY KNOWN SPECIMENS OF THE LATE JURASSIC SAUROPOD HAPLOCANTHOSAURUS FROM THE MORRISON FORMATION, USA Colin Boisvert, Gunnar T. Bivens, Brian Curtice, Ray Wilhite, Mathew Wedel GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association ISSN 2380-7601 Production Cover Design and Desktop Publishing Douglas A. Sprinkel Cover A skeletal reconstruction and life restoration of the enigmatic Late Jurassic Morrison Formation sauropod Haplocanthosaurus (scale is 2 m). Haplocanthosaurus has been characterized as a ‘primitive’ sau- ropod restricted to the lower half of the Morrison Formation, but the identification of Haplocanthosaurus in the Dry Mesa Dinosaur Quarry confirms that the genus was also present within the upper part of the Morrison Formation.


id: giw-10
title: Tracking dinosaurs in BLM canyon country, Utah
date: 2016
pages: 36
extension: .pdf
mime: application/pdf
words: 15746
sentence: 717
flesch: 57
cache: cache/giw-10.pdf
txt: txt/giw-10.txt
author:
  Hunt-Foster, ReBecca; Lockley, Martin; Milner, Andrew; Foster, John; Matthews, Neffra; Breithaupt, Brent; Smith, Joshua

summary:
  Lockley, M.G., and Conrad, K., 1989, The paleoenvironmental con- text, preservation and paleoecological significance of dinosaur tracksites in the western USA, in Gillette, D.D., and Lockley, M.G., editors, Dinosaur tracks and traces: New York, Cambridge University Press, p. 121–134. Lockley, M.G., Gierlinski, G., Dubicka, Z., Breithaupt, B.H., and Matthews, N.A., 2014b, A new dinosaur tracksite in the Cedar Mountain Formation (Cretaceous) of eastern Utah, in Lockley, M.G., and Lucas, S.G., editors, Fossil footprints of western North America: New Mexico Museum of Natural History and Science Bulletin 62, p. 279–285. Lockley, M.G., and Hunt, A.P., 1995, Dinosaur tracks and other fos- sil footprints of the western United States: New York, Columbia University Press, 338 p. Lockley, M.G., and Hunt, A.P., 1998, A probable stegosaur tracks from the Morrison Formation of Utah, in Carpenter, K., Chure, 99 Tracking Dinosaurs in BLM Canyon Country, Utah Hunt-Foster, R.K., Lockley, M.G., Milner, A.R.C., Foster, J.R., Matthews, N.A., Breithaupt, B.H., and Smith, J.A. Geology of the Intermountain West 2016 Volume 3 D., and Kirkland, J.I., editors, The Upper Jurassic Morrison Formation—an interdisciplinary study: Modern Geology, v. 23, p. 331–342.


id: giw-158
author: Gee, Carole; Xie, Aowei; Howell, Mariah
date: 2025
pages: 24
extension: .pdf
mime: application/pdf
words: 11999
sentence: 360
flesch: 48
cache: cache/giw-158.pdf
txt: txt/giw-158.txt
title:
  The whole plant of Araucaria delevoryasii and Agathoxylon hoodii—giant trees with silicified wood, gently tapering trunks, araucarian seed and pollen cones, and Brachyphyllum-type leaves with cuticle from the Upper Jurassic Morrison Formation of the Howe-

summary:
  Plant parts pertaining to an ancient species of conifer, for example, can be found as separate organ fossils such as seed cones, pollen cones, twigs with leaves, pieces of wood, and tree trunks. However, now that our current investigation has identified the silicified wood as pertaining to the Araucariaceae and that the morphology and taper of the two coalified trunks in the quarry are consistent with living Araucaria trunks, the likelihood of the fossil reproductive material, foliage, wood, and tree trunks representing the different parts of the same Upper Jurassic plant species is high.


id: giw-148
author: Morrison, Kate; Usachenko, Natalya; Erdman, Jonathan; Waters, Shilah; Love, Renee
date: 2024
pages: 38
extension: .pdf
mime: application/pdf
words: 15665
sentence: 554
flesch: 54
cache: cache/giw-148.pdf
txt: txt/giw-148.txt
title:
  Piecing together a prehistoric puzzle—regional inferences of micro- and macroscopic analyses of possibly one of the last hybrid mammoths in mainland Western North America

summary:
  Using the following equation: A = B x C where: A = length of the specimen’s frontal limb bone. B = established percentage that the length of the respective limb bone is of the animal’s total height. A, p. 14–31. 


id: giw-25
author: Whitlock, John; Trujillo, Kelli; Hanik, Gina
title: Assemblage-level structure in Morrison Formation dinosaurs, Western Interior, USA
date: 2018
pages: 16
extension: .pdf
mime: application/pdf
words: 38863
sentence: 300
flesch: -26
cache: cache/giw-25.pdf
txt: txt/giw-25.txt
summary:
  Assemblage-level Structure in Morrison Formation Dinosaurs, Western Interior, USA John A. Whitlock1, Kelli C. Trujillo2, and Gina M. Hanik1 1Department of Science and Mathematics, Mount Aloysius College, Cresson, PA 16630; jwhitlock@mtaloy.edu; gmhst4@student.mtaloy.edu 2Haub School of Environmental and Natural Resources, �e University of Wyoming, Laramie, WY 82071; kellitrujillo@icloud.com Citation for this article. www.utahgeology.org 10 Assemblage-level Structure in Morrison Formation Dinosaurs, Western Interior, USA Whitlock, J.A., Trujillo, K.C., and Hanik, G.M. Geology of the Intermountain West 2018 Volume 5 Here, we show contrasting patterns in distribution be- tween the largest bodied herbivores and all other dino- saurian taxa, and interpret the low degrees of endemism and connectivity as evidence for a ‘mosaic’ type land- scape throughout most of the depositional basin repre- sented by the Morrison Formation.


id: giw-81
author: Itano, Wayne; Carpenter, Kenneth
date: 2020
pages: 9
extension: .pdf
mime: application/pdf
words: 3523
sentence: 139
flesch: 48
cache: cache/giw-81.pdf
txt: txt/giw-81.txt
title:
  High-quality casts of the missing holotype of Petalodus ohioensis Safford 1853 (Chondrichthyes, Petalodontidae) at the Field Museum of Natural History and their bearing on the validity and priority of the species

summary:
  Hay later reconsid- ered the status of P. ohioensis, since P. alleghaniensis, P. destructor, and P. securiger (as P. securis) are all listed as 198 High-quality Casts of the Missing Holotype of Petalodus ohioensis Safford 1853 (Chondrichthyes, Petalodontidae) at the Field Museum of Natural History and their Bearing on the Validity and Priority of the Species Itano, W.M., and Carpenter, K. Geology of the Intermountain West 2020 Volume 7 junior synonyms of P. ohioensis in the bibliography of fossil vertebrates of North America (Hay, 1902). That the Field Mu- seum and Yale Peabody Museum casts are of the same tooth is clear by observation.


id: giw-120
author: Chandonia, William; Hogan, John
date: 2023
pages: 66
extension: .pdf
mime: application/pdf
words: 38008
sentence: 1233
flesch: 56
cache: cache/giw-120.pdf
txt: txt/giw-120.txt
title:
  The Kanarra fold-thrust structure—the leading edge of the Sevier fold-thrust belt, southwestern Utah:

summary:
  SCT–Spring Creek thrust; KCT–Kanarra Creek thrust; HCT–Hicks Creek thrust; TCT–Taylor Creek thrust; RRTT–Red Rock Trail thrust. Structure initializations: HF–Hurricane fault; KCT– Kanarra Creek thrust; SCT–Spring Creek thrust; HCT–Hicks Creek thrust; TCT–Taylor Creek thrust; MCT1, 2–Murie Creek thrust system; RRTT–Red Rock Trail thrust.


id: giw-152
author: Carpenter, Kenneth; Taylor, Louis
title: A river runs through it—the Quarry Sandstone and adjacent strata, Dinosaur National Monument, Utah
date: 2025
pages: 52
extension: .pdf
mime: application/pdf
words: 30906
sentence: 1374
flesch: 56
cache: cache/giw-152.pdf
txt: txt/giw-152.txt
summary:
  Bilbey, S.A., 1992, Stratigraphy and sedimentary petrology of the Upper Jurassic–Lower Cretaceous rocks at Cleve- 67 A River Runs Through It—The Quarry Sandstone and Adjacent Strata, Dinosaur National Monument, Utah Carpenter, K., and Taylor, L.H. Geology of the Intermountain West 2025 Volume 12 land–Lloyd Dinosaur Quarry with a comparison to the Dinosaur National Monument Quarry, Utah: Salt Lake City, University of Utah, Ph.D. dissertation, 295 p. 59 A River Runs Through It—The Quarry Sandstone and Adjacent Strata, Dinosaur National Monument, Utah Carpenter, K., and Taylor, L.H. Geology of the Intermountain West 2025 Volume 12 To test the hypothesis that the Quarry Sandstone resulted from a loss of accommodation space due to the activity of a proto-Split Mountain anticline, we ex- amined sandstone beds along the western periphery of Split Mountain, which provides a nearly continuous exposure of the Morrison Formation from the QEH (Figure 30A).


id: giw-119
author: Webb, Casey; Jensen, Michael; Kowallis, Bart; Christiansen, Eric; Sprinkel, Douglas; Hudson, Sam
date: 2022
pages: 29
extension: .pdf
mime: application/pdf
words: 15594
sentence: 529
flesch: 47
cache: cache/giw-119.pdf
txt: txt/giw-119.txt
title:
  Stratigraphic relationships of the Eocene Duchesne River Formation and Oligocene Bishop Conglomerate, northeastern Utah—pulsed sedimentary response to rollback of the subducted Farallon slab

summary:
  Stratigraphic and structural relationships between the Duchesne River Formation and Bishop Conglomerate reveal evidence of at least three episodes of Laramide-age uplift of the Uinta Mountains during the deposition of these formations: (1) deposition of fining upward sequences beginning with a basal coarse-grained unit within the Brennan Basin, Dry Gulch Creek, and Lapoint Members; (2) progradation of alluvial fans to the south form the younger Starr Flat Member resulted from an increase in sediment supply likely associated with renewed uplift; and (3) tilting and truncation of Duchesne River Formation to form the Gilbert Peak erosional surface, and prograding alluvial fans of the Bishop Conglomerate. The Duchesne River Formation unconformably overlies Cretaceous units.


id: giw-89
author: Richmond, Dean; Pigott, John; Lupia, Richard; Behm, Michael; Hein, David
date: 2021
pages: 28
extension: .pdf
mime: application/pdf
words: 16966
sentence: 659
flesch: 48
cache: cache/giw-89.pdf
txt: txt/giw-89.txt
title:
  Carbonate mound springs of the Upper Jurassic Morrison Formation of central Montana and their paleoclimatic significance for the northern foreland basin

summary:
  XRF comparison of several Morrison Formation carbonate mounds. To distinguish between the two types of buildups, they will be referred to as siderite buildups (SB) and carbonate mounds (CM).


id: giw-155
author: Hockett, Bryan; Goebel, Ted; Graf, Kelly
date: 2025
pages: 34
extension: .pdf
mime: application/pdf
words: 18961
sentence: 670
flesch: 56
cache: cache/giw-155.pdf
txt: txt/giw-155.txt
title:
  Faunal extirpations, range shifts, and extinctions in the western Bonneville basin, 17,500 to 5500 cal yr BP: Paleobiogeography of Bonneville Estates Rockshelter and Siblings East Shelter

summary:
  General location of Bonneville Estates Rockshelter, Siblings East Shelter, and other sites mentioned in the text in relation to the Bonneville basin and the high stand of Pleistocene Lake Bonneville. SETTING Bonneville Estates Rockshelter and Siblings East Shelter rest upon relic Bonneville-era and Provo-era shorelines, respectively, of Pleistocene Lake Bonneville in the far western Bonneville basin of eastern Nevada (Figure 1).


id: giw-103
author: Carpenter, Kenneth
date: 2022
pages: 68
extension: .pdf
mime: application/pdf
words: 35629
sentence: 1299
flesch: 49
cache: cache/giw-103.pdf
txt: txt/giw-103.txt
title:
  The lithostratigraphic Tidwell Member of the Morrison or Summerville Formations (Upper Jurassic)—who, what, where, when?

summary:
  Demko, T.M., Currie, B.S., and Nicoll, K.A., 2004, Region- al paleoclimatic and stratigraphic implications of pa- leosols and fluvial/overbank architecture in the Mor- rison Formation (Upper Jurassic), Western Interior, USA, in Turner, C.E., Peterson, F., and Dunagan, S., editors, Reconstruction of the extinct ecosystem of the Upper Jurassic Morrison Formation: Sedimentary Ge- ology, v. 167, p. 115–135. Hasiotis, S.T., 2004, Reconnaissance of Upper Jurassic Mor- rison Formation ichnofossils, Rocky Mountain region, 105 The Lithostratigraphic Tidwell Member of the Morrison or Summerville Formations (Upper Jurassic)—Who, What, Where, When? Carpenter, K. Geology of the Intermountain West 2022 Volume 9 USA—paleoenvironmental, stratigraphic, and paleocli- matic significance of terrestrial and freshwater ichno- coenoses, in Turner, C.E., Peterson, F., and Dunagan, S., editors, Reconstruction of the extinct ecosystem of the Upper Jurassic Morrison Formation: Sedimentary Geol- ogy, v. 167, p. 177–268.


id: giw-91
author: Priddy, Charlotte; Regis, Amy; Clarke, Stuart; Leslie, A.; Dodd, Thomas
date: 2021
pages: 20
extension: .pdf
mime: application/pdf
words: 10728
sentence: 316
flesch: 36
cache: cache/giw-91.pdf
txt: txt/giw-91.txt
title:
  Localized bank collapse or regional event? A study of distinct contorted heterolithic facies observed in the Lower Jurassic Kayenta Formation, Utah and Arizona

summary:
  Doelling, H.H., 2010, Geology of Arches National Park, Utah, in Sprinkel, D.A., Chidsey, T.C., Jr., and Anderson, P.B., editors, Geology of Utah’s parks and monuments (third edition): Utah Geological Association Publication 28, p. 11–36. Doelling, H.H., Sprinkel, D.A., Kowallis, B.J., and Kuehne, P.A., 2013, Temple Cap and Carmel Formations in the Henry Mountains Basin, Wayne and Garfield Counties, Utah, in Morris, T.H., and Ressetar, R., editors, The San Rafael Swell and Henry Mountains Basin—geologic centerpiece of Utah: Utah Geological Association Publication 42, p. 279–318.


id: giw-16
author: Martz, Jeffrey; Kirkland, James; Milner, Andrew; Parker, William; Santucci, Vincent
date: 2017
pages: 84
extension: .pdf
mime: application/pdf
words: 48355
sentence: 1415
flesch: 43
cache: cache/giw-16.pdf
txt: txt/giw-16.txt
title:
  Upper Triassic lithostratigraphy, depositional systems, and vertebrate paleontology across southern Utah

summary:
  Southwest-dipping exposures (figures 12C and 12D) of the Middle Pennsylvanian Hermosa Group, Upper Pennsylvanian-Lower Permian Cutler Group, Upper Triassic Chinle Formation, and the Upper Tri- assic-Lower Jurassic Wingate, Kayenta, and Navajo Formations occur on the southwestern side of the fault in Lisbon Valley (e.g., Doelling, 2004). Dubiel, R.F., 1992, Sedimentology and depositional history of the 171 Upper Triassic Lithostratigraphy, Depositional Systems, and Vertebrate Paleontology Across Southern Utah Martz, J.W., Kirkland, J.I., Milner, A.R.C., Parker, W.G., and Santucci, V.L. Geology of the Intermountain West 2017 Volume 4 Upper Triassic Chinle Formation in the Uinta, Piceance, and Ea- gle Basins, northwestern Colorado and northeastern Utah: U.S. Geological Survey Bulletin 1787-W, p. 1–25.


id: giw-129
author: Richmond, Dean
date: 2023
pages: 56
extension: .pdf
mime: application/pdf
words: 32710
sentence: 1352
flesch: 50
cache: cache/giw-129.pdf
txt: txt/giw-129.txt
title:
  Stratigraphy, sedimentology, and paleoclimatic proxies of the Upper Jurassic Morrison Formation of central Montana: Geology of the Intermountain West

summary:
  STRATIGRAPHY, SEDIMENTOLOGY, AND PALEOCLIMATIC PROXIES OF THE UPPER JURASSIC MORRISON FORMATION OF CENTRAL MONTANA Dean R. Richmond GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association ISSN 2380-7601 Production Cover Design and Desktop Publishing Douglas A. Sprinkel Cover Fossil dinosaur bones were first discovered in the Upper Jurassic Morrison Formation near the town of Grass Range, Montana, in 1987. Foster, J.R., Hunt, A.P., and Kirkland, J.I., 2022, Significance of a small regurgitalite containing lissamphibian bones from the Morrison Formation Upper Jurassic), within a diverse plant locality deposit in southeastern Utah, USA: PALAIOS, v. 37, p. 433‒442.


id: giw-153
author: Kirkland, James; King, Ryan; Bylund, Kevin
date: 2025
pages: 82
extension: .pdf
mime: application/pdf
words: 37772
sentence: 1358
flesch: 54
cache: cache/giw-153.pdf
txt: txt/giw-153.txt
title:
  Revisiting the Cretaceous Mancos Group in Utah—problems, previous methods, and new perspectives on a world-class Cretaceous marine section

summary:
  Ryer, T.A., 1976, Cretaceous stratigraphy of the Coalville and Rockport areas, Utah: Utah Geology, v. 3, p. 71–83. 801.915.3188 Co-Chair John South jsouth@utah.gov 385.266.2113 Earthquake Safety Committee Chair Grant Willis gwillisgeol@gmail.com 801.537.3355 Douglas A. Sprinkel Azteca Geosolutions 801.391.1977 GIW@utahgeology.org dsprinkel@gmail.com Thomas C. Chidsey, Jr. Utah Geological Survey, Emeritus 801.824.0738 tomchidsey@gmail.com Bart J. Kowallis Brigham Young University 801.380.2736 bkowallis@gmail.com Steven Schamel GeoX Consulting, Inc. 801.583.1146 geox-slc@comcast.net John R. Foster Utah Field House of Natural History State Park Museum 435.789.3799 johnfoster@utah.gov William R. Lund Utah Geological Survey, Emeritus 435.590.1338 williamlundugs@gmail.com Editors GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association Volume 12 2025 75 ABSTRACT The Mancos Group is an upper Cenomanian-middle Campanian lithostratigraphic unit that records large-scale changes in sedimentation patterns associated with the incursion of the Western Interior seaway across western Colorado into central Utah.


id: giw-128
author: Milner, Andrew; Santucci, Vincent; Wood, John; Birthisel, Tylor; Clites, Erica; Lockley, Martin
date: 2023
pages: 40
extension: .pdf
mime: application/pdf
words: 20894
sentence: 655
flesch: 50
cache: cache/giw-128.pdf
txt: txt/giw-128.txt
title:
  The John Wesley Powell Fossil Track Block—theropod tracks with ornithopod-like morphology from the Early Jurassic Navajo Sandstone, Glen Canyon National Recreation Area, Utah-Arizona

summary:
  Belvedere, M., and Farlow, J.O., 2016, A numerical scale for quantifying the quality of preservation of vertebrate tracks, in Falkingham, P.L., Marty, D., and Richter, A., ed- itors, Dinosaur tracks—the next steps: Bloomington and Indianapolis, indiana University Press, p. 92–99. Dai, H., Xing, L., Marty, D., Zhang, J., Persons IV, W.S., Hu, H., and Wang, F., 2015, Microbially-induced sedimenta- ry wrinkle structures and possible impact of microbial mats for the enhanced preservation of dinosaur tracks from the Lower Cretaceous Jiaguan Formation near Qi- jiang (Chongqing, China): Cretaceous Research, v. 53, p. 98–109.


id: giw-11
author: Kirkland, James; Suarez, Marina; Suarez, Celina; Hunt-Foster, ReBecca
title: The Lower Cretaceous in east-central Utah—The Cedar Mountain Formation and its bounding strata
date: 2016
pages: 130
extension: .pdf
mime: application/pdf
words: 64578
sentence: 2277
flesch: 51
cache: cache/giw-11.pdf
txt: txt/giw-11.txt
summary:
  (H) Iron-stained nodules in basal Cedar Mountain Formation. (B) Exposure of basal Cedar Mountain Formation at the south end of Caineville Reef (38°16'27.56N, 111°3'58.48W) looking west.


id: giw-73
date: 2020
pages: 76
extension: .pdf
mime: application/pdf
words: 46801
sentence: 1529
flesch: 55
cache: cache/giw-73.pdf
txt: txt/giw-73.txt
author:
  Kirkland, James; DeBlieux, Donald; Hunt-Foster, ReBecca; Foster, John; Trujillo, Kelli; Finzel, Emily

title:
  The Morrison Formation and its bounding strata on the western side of the Blanding basin, San Juan County, Utah

summary:
  Tanner, L.H., Galli, K.G., and Lucas, S.G., 2014, Pedogenic and lacustrine features of the Brushy Basin Member of the Up- per Jurassic Morrison Formation in western Colorado— reassessing the paleoclimatic interpretations: Volumina Jurassica, v. XII (2): p. 115–130, doi:10.5604/17313708 .1130134. (B) Simplified diagram of relationships of Morrison Formation units, along with bounding strata, for east side of Comb Ridge.


id: giw-156
author: Paul, Gregory
date: 2025
pages: 22
extension: .pdf
mime: application/pdf
words: 12642
sentence: 397
flesch: 42
cache: cache/giw-156.pdf
txt: txt/giw-156.txt
title:
  Stratigraphic and anatomical evidence for multiple titanosaurid dinosaur taxa in the Late Cretaceous (Campanian-Maastrichtian) of southwestern North America

summary:
  Stratigraphic chart for North American Late Cretaceous titanosaurids. It therefore is not known how many taxa are represented by these nonoverlapping fossils, contrary to Jasinski et al. (2011) who insist on a presumption of one taxon while not noting that multiple titanosaurid and Formation Location Age Specimen Lower Black Peaks West Texas latest Maastrichtian BIBE 45854, 45958; TMM 43621-1 Lower North Horn Central Utah late Maastrichtian USNM 15560 (Utetitan holotype), BYU 9087, 11392, 11393 Upper Javelina West Texas middle to late Maastrichtian AMNH 21531; TMM 41541-1 Middle Javelina West Texas middle to late Maastrichtian TMM 46052-1 Lower Javelina West Texas, northeastern Chihuahua Province middle to late Maastrichtian TMM 40699, 41060, 41061, 41398-1- 2, 41450-1-2; TTU 542, 546; UTEP P-25, uncataloged Chihuahua fossil remains Javelina (stratigraphic position was not avail- able) West Texas middle to late Maastrichtian TMM 40597-5, 41063, 41396-1, 41541, 42495-7, 43090-2, 43598-1-6, 43599-1-3, 45601-1, 45602-1, 45854- 1-8, 45855-1-4, 45856-1, 45857-1, 45859-1, 45861-1, 45862-1, 45863-1, 45864-1, 45865-1, 45888-1, 45890- 1&2, 45891-1-17, 45864-1 Middle Hall Lake southern New Mexico middle Maastrichtian TKM 007, 009


id: giw-154
date: 2025
pages: 16
extension: .pdf
mime: application/pdf
words: 38812
sentence: 265
flesch: -36
cache: cache/giw-154.pdf
txt: txt/giw-154.txt
author:
  Malone, David; Stevens, Grace; Lesmann, Sarah; Rivera, Tiffany; Biek, Robert; Braunagel, Michael; Griffith, W. Ashley; Hacker, David; Rowley, Peter

title:
  Claron basin provenance shift from Sevier-Laramide compression to Basin and Range extension: Detrital zircon geochronology from the Eocene-Oligocene Brian Head Formation, Utah

summary:
  Spot 69 584.6577465478 178.9135880761 7506.6768908311 100 3.2678219292 21.5674593534 2.1502985728 0.0018604912 11.7016823351 0.0335884014 2.568385395 0.0052562508 1.4045709613 0.546869237 33.7952290718 0.4734359001 33.5448367232 0.8474847868 15.6655369804 NA 37.5507602453 4.3899895093 33.7952290718 0.4734359001 Spot 42 90.5265711707 95.7663783977 19919.926761126 429.7553258234 0.9452855238 17.7441393399 6.0551966075 0.0019206849 10.7436814334 0.0408341961 6.2655582444 0.0052573477 1.6099112272 0.2569461753 33.8022635496 0.5427621862 40.6381715635 2.4959335265 465.4593081699 134.2457213443 38.7645002777 4.1607412972 33.8022635496 0.5427621862 Spot 115 166.3037664177 196.6947319772 1883.1461515991 100 0.8454917157 26.1119233046 3.4611857085 0.001620195 10.7580975368 0.0278062207 3.9283699553 0.0052682767 1.8580322917 0.4729779305 33.87234764 0.6277085838 27.8485535604 1.0791285393 NA NA 32.7047259144 3.515559939 33.87234764 0.6277085838 Spot 6 455.2303726456 216.5734330565 14309.113024745 125.2634623945 2.1019677539 21.1136675396 2.4967338862 0.0017144342 13.8923297098 0.0344929715 2.8123389637 0.005284234 1.2944382365 0.4602710602 33.9746749178 0.4386243227 34.4330853241 0.952139905 66.5083729961 59.4407230615 34.6053788491 4.8033782307 33.9746749178 0.4386243227 Spot 113 178.5542832638 157.5174196806 8740.7146540225 137.2608934188 1.1335526168 21.0824396954 4.081838785 0.0016605858 10.4083896361 0.034572477 4.2446173212 0.0052885805 1.164202876 0.2742774644 34.0025466543 0.3948164529 34.5111191539 1.4402514463 70.0371490072 NA 33.5193651329 3.4859334162 34.0025466543 0.3948164529 Spot 117 91.9330051201 48.4378494411 1974.365995594 100 1.8979580262 22.1141871667 5.4585865352 0.0016164307 16.439856088 0.0330403474 5.5724446673 0.0053015558 1.1207018372 0.2011149332 34.0857506168 0.38099149 33.0062931539 1.8096869553 NA NA 32.6288017798 5.3597986423 34.0857506168 0.38099149 Spot 100 338.6125886308 248.9106933565 6348.2201775021 100 1.3603778289 23.2941452803 3.3491423744 0.0017152464 18.428651862 0.0313690759 3.5259137069 0.0053019577 1.1024122752 0.3126600271 34.0883275861 0.3748020671 31.36225776 1.0889034557 NA NA 34.6217588854 6.374859521 34.0883275861 0.3748020671 Spot 85 135.2975702231 100.9400435279 11978.2825488891 172.2058458391 1.3403755883 24.7009353704 3.8351736364 0.0017346727 11.6244765378 0.029587935 4.1376770013 0.005302929 1.5530016569 0.3753317759 34.094555643 0.5280912685 29.6072082617 1.2073631361 NA NA 35.0135323525 4.0666148233 34.094555643 0.5280912685 Spot 78 207.4521924437 211.7640363267 7567.6854558893 156.3795952599 0.9796384506 21.4666598375 4.0663214078 0.0018127973 12.7693606432 0.0340959604 4.319905972 0.0053107414 1.4582927741 0.3375751194 34.1446522369 0.4966126349 34.0433333504 1.4462607009 26.8795345473 NA 36.5890129799 4.667954633 34.1446522369 0.4966126349 Spot 111 339.0264533538 151.2057275008 8541.3615930627 100 2.2421535147 22.4558559416 2.1684443708 0.0018134948 19.9248019912 0.0326429055 2.4285829095 0.0053187083 1.0935556497 0.4502854918 34.1957386829 0.3729593555 32.6155694072 0.7795097874 NA NA 36.6030798556 7.2864884858 34.1957386829 0.3729593555 Spot 110 186.5471687196 103.6519640239 3870.6304278275 100 1.7997456245 23.121117771 3.4960784523 0.0016824139 14.439070061 0.031704008 3.6747699304 0.0053187644 1.1319759258 0.3080399446 34.1960978949 0.3860667127 31.691944975 1.1466194414 NA NA 33.9596011516 4.8993316563 34.1960978949 0.3860667127 Spot 18 165.8138501382 101.2393569272 1297.4406764074 100 1.6378398201 27.3303070477 4.2791903852 0.0018777864 9.8881644132 0.0268353793 4.553566544 0.0053215727 1.5567587859 0.341876806 34.214106142 0.5312201419 26.8889935656 1.2083387913 NA NA 37.8995068375 3.7440525235 34.214106142 0.5312201419 Spot 103 678.5108096486 180.3865581274 19536.3931253428 100 3.7614266644 20.8021197514 1.8122317039 0.0016682356 18.8878896772 0.0352755964 2.0926038036 0.0053243882 1.0463302205 0.5000135327 34.2321595892 0.3572320935 35.2009626046 0.7239946939 101.7628525876 42.8337127298 33.6736488597 6.35494403 34.2321595892 0.3572320935 Spot 112 674.8417223094 648.6024277878 8346.3245070884 146.7679192034 1.0404551284 19.5506752045 2.4629960136 0.0016757131 12.6810908727 0.0375349372 2.816549884 0.0053245782 1.3662371266 0.485074713 34.2333778681 0.4664694407 37.4144762808 1.0346190541 246.5763855554 56.704244508 33.8244586738 4.28572159 34.2333778681 0.4664694407 Spot 33 322.2152106075 108.4516134726 4007.1639578948 100 2.9710504094 23.8875844627 3.2269375186 0.0017394423 13.7228122682 0.0307776745 3.4917096003 0.0053345255 1.333757918 0.3819784778 34.2971621165 0.4562263985 30.7798559128 1.0586172906 NA NA 35.1097213119 4.813856947 34.2971621165 0.4562263985 Spot 36 669.0389031595 1355.809031363 12661.0559800963 456.1034416873 0.4934610168 21.3068367983 2.2767916996 0.0016568445 3.8585354036 0.0345398794 2.552417789 0.0053398315 1.1537140574 0.4520083124 34.3311853561 0.3950308852 34.4791256987 0.8652773978 44.7967546525 NA 33.4439080084 1.289377473 34.3311853561 0.3950308852 Spot 94 168.24572283 31.091121464 8796.644743678 100 5.4113751743 19.1276948117 3.5398351793 0.001801667 26.4571584478 0.0384992574 3.8801339764 0.0053432161 1.5890269282 0.4095288817 34.3528882337 0.5444247401 38.3577694518 1.4605724143 296.7144584142 80.7931068177 36.364565147 9.6123773898 34.3528882337 0.5444247401 Spot 22 137.1674753533 84.3866131511 2399.3522689116 100 1.6254648721 23.9310530552 3.7652121079 0.0015115885 13.1294388916 0.0308547916 4.0405215318 0.0053576234 1.4659440752 0.3628106084 34.4452691332 0.5036017317 30.8558184625 1.2279838955 NA NA 30.5140843552 4.0033039605 34.4452691332 0.5036017317 Spot 12 198.37008889 137.7084379026 9520.8089719715 114.6160842311 1.4405078724 23.0501326374 3.886676019 0.0016157808 17.0543160515 0.0320395382 4.0943043948 0.0053585518 1.2872754176 0.3144063786 34.451222057 0.4422991828 32.0221135861 1.2906253307 NA NA 32.6156938852 5.5578959035 34.451222057 0.4422991828 Spot 32 155.9918736214 110.8536941977 1846.0989947775 100 1.4071869661 22.6372668019 9.8482826969 0.0017539926 19.1690199017 0.0326605342 9.9420534228 0.0053645714 1.3622606887 0.1370200532 34.4898199597 0.4685866181 32.6329033545 3.1928104722 NA NA 35.4031535774 6.7804948149 34.4898199597 0.4685866181 Spot 108 267.008797389 777.3214915366 6386.2935912558 325.4168809699 0.3434985399 19.5237232512 4.9820100869 0.0016734436 5.8949206268 0.0378874962 5.1419260331 0.0053671818 1.2723909869 0.2474541599 34.5065577681 0.4378853233 37.759449372 1.9059077315 249.7067405664 114.7153191556 33.7786864801 1.9895629803 34.5065577681 0.4378853233 Spot 106 473.0126208425 54.9504666885 44781.4580741145 100 8.6079818671 20.9954118097 2.0403787363 0.0015975935 26.4570879487 0.0352334962 2.3076471523 0.0053674486 1.0780027791 0.4671436784 34.508268535 0.3710061926 35.1596704648 0.7974745436 79.8471423481 48.4593099916 32.2488619847 8.5253039229 34.508268535 0.3710061926 Spot 34 124.1676635102 83.4287374884 1810.5942021287 100 1.4883080728 27.3931557795 5.0430755181 0.0014566545 20.8838665303 0.027020251 5.2667239315 0.0053705554 1.5184763049 0.2883151509 34.5281894123 0.5229007491 27.0717868768 1.4069579381 NA NA 29.4059509738 6.1366324343 34.5281894123 0.5229007491 Spot 13 480.1923542212 498.1453149196 4629.1864191852 100 0.9639603944 22.4205887108 3.1069431087 0.0016467989 18.2090746577 0.0330154106 3.2426390594 0.0053709544 0.928230892 0.286257852 34.5307481532 0.3196681431 32.9817822976 1.0522975954 NA NA 33.2413013651 6.047956411 34.5307481532 0.3196681431 Spot 92 598.8718775646 296.9122746161 173435.330629171 2103.2903647447 2.0169993926 21.0366182249 2.1638595661 0.0018114219 6.7609015666 0.0352060658 2.5236133434 0.005373796 1.2985900374 0.5145756741 34.5489681824 0.4474493565 35.1327657294 0.8714521007 75.1889408604 51.4354670996 36.5612775756 2.4696365732 34.5489681824 0.4474493565 Spot 95 120.9749652569 139.4089898638 9250.5601321857 210.5959806456 0.8677701874 22.1568964005 4.6617000535 0.0018194249 13.4948050471 0.0334265925 4.8873951937 0.0053738902 1.4680546278 0.3003756745 34.5495720992 0.5058498306 33.3858654147 1.6051669313 NA NA 36.7226610906 4.9511502277 34.5495720992 0.5058498306 Spot 81 93.6765901165 60.4743681032 2069.1744016529 100 1.5490296642 24.7486291429 5.3205324208 0.0014567533 18.2080997079 0.0299392412 5.5337682689 0.0053762529 1.5213566359 0.2749223607 34.5647217702 0.5244454335 29.9536085606 1.6333544427 NA NA 29.4079445692 5.3507325369 34.5647217702 0.5244454335 Spot 126 319.2714437276 291.1737042194 6791.7300011289 109.5738438645 1.096498204 21.19672217 2.4035960155 0.0016219222 16.948618515 0.0349663186 2.6459771984 0.0053778214 1.1063098701 0.4181101299 34.5747785089 0.3814802552 34.8975821145 0.9076947369 57.1400366807 57.2989763066 32.739561071 5.5444095772 34.5747785089 0.3814802552 Spot 74 927.8564251564 937.3692659033 47290.1052637419 861.4627416281 0.9898515547 21.721001228 2.0697752431 0.0017240284 5.2416478845 0.0341253585 2.3465539192 0.0053782974 1.1055974579 0.4711579175 34.5778311024 0.3812681685 34.0721989939 0.7862570812 NA NA 34.7988689205 1.8224640936 34.5778311024 0.3812681685 Spot 82 397.8405006107 120.9573189315 5335.874465596 100 3.2890982053 22.2931441442 3.448416439 0.0015464976 15.2916294061 0.0332624269 3.6270302748 0.0053803808 1.124176444 0.3099440476 34.5911892606 0.3878245461 33.2245533537 1.1855628582 NA NA 31.2182433308 4.7700915982 34.5911892606 0.3878245461 Spot 80 270.9417691027 78.3573140385 13330.7090150907 100 3.457772544 22.5449895261 2.9942830816 0.0016523014 16.1314180626 0.0329211502 3.1658468006 0.0053853359 1.0280344313 0.3247265253 34.6229607305 0.3549818209 32.8891266425 1.0245373219 NA NA 33.352279347 5.3757570006 34.6229607305 0.3549818209 Spot 50 112.2805658701 74.7363309865 33715.7570967946 400.2939242587 1.5023558742 18.8354310475 5.6612312817 0.0017325628 15.3332428903 0.0394224156 5.942998983 0.005387739 1.8082304297 0.3042622815 34.6383694888 0.624661796 39.2599779168 2.2886925492 331.7321093395 128.4925442523 34.9709822941 5.3575473165 34.6383694888 0.624661796 Spot 118 435.9174342993 243.8385808995 8969.1455760148 100 1.787729541 21.4887573351 3.392326219 0.0017361012 18.9033549609 0.0345755074 3.5819065783 0.0053909787 1.1498598001 0.3210189252 34.6591421326 0.3974621081 34.5140933637 1.215488188 24.4478419395 NA 35.0423408265 6.6184364942 34.6591421326 0.3974621081 Spot 124 232.7746682574 315.0103419086 5190.4774041387 125.3119519583 0.7389429402 20.3748659839 3.156477203 0.0016911932 14.2923297487 0.0364728757 3.3505218917 0.0053920328 1.1236763831 0.3353735386 34.6659003731 0.3884870459 36.3745579935 1.1971667257 150.6606191944 74.0075396207 34.1366621974 4.8748046246 34.6659003731 0.3884870459 Spot 35 490.3235780618 340.9990607109 61379.7302079373 831.5098957876 1.4379030166 22.6550446606 2.2739557658 0.0018434097 5.6126533501 0.0328561897 2.4631595305 0.0054009465 0.9467206809 0.384352158 34.7230535053 0.3278465776 32.8252670414 0.7956093541 NA NA 37.2063163154 2.0863397576 34.7230535053 0.3278465776 Spot 48 78.5825137225 109.5501069812 3210.214109313 100 0.7173202828 19.1513854394 7.4119091777 0.0016027394 20.9535667245 0.0388796675 7.5698915907 0.0054026955 1.5384606061 0.2032341663 34.7342680031 0.5329359715 38.7296438128 2.8765904088 293.8685556366 169.4236918735 32.3526538751 6.7736099029 34.7342680031 0.5329359715 Spot 107 153.94388615 96.8960877502 3037.0932592781 100 1.58875234 23.8715633694 3.6883068128 0.0016214352 11.7129408173 0.0312005418 4.0137802199 0.0054041918 1.5832954583 0.3944649113 34.7438616508 0.548618229 31.1963223774 1.233112546 NA NA 32.7297389278 3.8305112105 34.7438616508 0.548618229 Spot 109 74.0578657216 103.6415822427 7949.5725399697 205.4244149623 0.7145574597 22.0485374039 5.6277943475 0.0017218168 14.0712375186 0.0337834183 5.9450258021 0.0054046943 1.9160539058 0.3222953053 34.7470833395 0.6639817645 33.7364005377 1.9726872129 NA NA 34.7542666391 4.8861513854 34.7470833395 0.6639817645 Spot 31 282.2257037275 147.3835608811 9907.3311549334 111.0955343157 1.9149062625 21.7955600134 3.8443397388 0.0019632666 16.967652958 0.0341899721 4.007865292 0.0054069771 1.1331531986 0.2827323565 34.7617206017 0.3928434107 34.1356395553 1.3453698927 NA NA 39.6230693685 6.7165163038 34.7617206017 0.3928434107 Spot 15 133.2503052552 83.0612087884 3022.281309492 100 1.6042423076 18.9081862858 5.572303393 0.0019163159 18.659266422 0.0394122346 5.6673921475 0.0054071533 1.0338126762 0.1824141773 34.7628504548 0.358415493 39.250032365 2.1820117173 322.9708103159 126.6391811256 38.6764066268 7.2098303136 34.7628504548 0.358415493 Spot 125 1542.9674871529 1031.466402982 305710.568252102 4931.035666681 1.4958969897 20.6873506205 1.4484725806 0.0017725151 2.981508512 0.0360447456 1.7325410533 0.005410465 0.950592281 0.548669412 34.784084116 0.3297643342 35.955052721 0.6120359746 114.8296041999 34.1888893865 35.7766876839 1.0657410261 34.784084116 0.3297643342 Spot 1 220.2350394674 143.2080481424 4380.2234433279 100 1.5378677548 22.3474021112 4.6111579836 0.0016420412 22.0536757202 0.0333713912 4.8461078224 0.0054111442 1.4906317708 0.3075936041 34.7884389046 0.5171707981 33.3316264372 1.5890633656 NA NA 33.1453436041 7.3037736442 34.7884389046 0.5171707981 Spot 104 1113.0326965222 884.9364846222 25257.5139382463 365.4486620949 1.2577543314 21.1026702466 1.5236080116 0.0016399242 6.2861314256 0.0353488922 1.656171528 0.0054125382 0.6492478396 0.3920172691 34.7973766925 0.2253125572 35.2728474441 0.5741486603 67.7808464578 36.2376135902 33.102646514 2.0791719615 34.7973766925 0.2253125572 Spot 86 136.5201934117 153.445288699 2306.4231120839 100 0.889699479 23.5119612926 3.816110114 0.0015054493 15.3245357678 0.031750627 3.9909990934 0.0054166268 1.168493629 0.2927822336 34.8235918439 0.4058143592 31.7378253749 1.2470656655 NA NA 30.390248001 4.6536633365 34.8235918439 0.4058143592 Spot 77 221.2729401819 61.3795414079 16057.5890032709 100 3.604995005 19.8290493869 3.4809724112 0.0018023237 22.7224848688 0.0376500692 3.7158692675 0.0054169575 1.3001982487 0.3499041961 34.8257118271 0.4515823972 37.5271439009 1.36900634 213.9234067698 80.6686810814 36.3778064243 8.2585042391 34.8257118271 0.4515823972 Spot 40 912.536131335 2537.434252401 115270.115744122 5607.8752478936 0.3596294684 22.2698812167 2.0174205226 0.0016735691 3.2645330035 0.0335238845 2.2416989065 0.0054170144 0.9773578782 0.4359898091 34.8260767904 0.3394576377 33.4814542399 0.7383139697 NA NA 33.7812161171 1.1018774302 34.8260767904 0.3394576377 Spot 19 97.0246855788 67.0907352745 3405.8376662078 100 1.4461711469 19.781961053 6.0690058956 0.0016275539 22.530332047 0.0377774856 6.2814008916 0.0054223824 1.6196186586 0.2578435426 34.8604948243 0.5630832057 37.6518184138 2.3217528306 219.4288071458 140.5521254557 32.8531486533 7.3959084529 34.8604948243 0.5630832057 Spot 130 121.5200129687 96.9071771428 3083.0949037361 100 1.2539836218 23.250468407 4.9030048498 0.0017746408 20.7753919937 0.0321771817 5.0997280356 0.0054283453 1.40277207 0.2750680154 34.898726305 0.4882268456 32.1575265505 1.6142509173 NA NA 35.8195553175 7.4350599823 34.898726305 0.4882268456 Spot 26 55.1471319845 70.3295076701 560.049523772 100 0.7841250964 62.3672268229 30.9354983398 0.0017619036 19.8497643604 0.0120005836 30.9993815097 0.0054305843 1.9891195159 0.0641664259 34.9130816841 0.6925857464 12.1126542893 3.7325574497 NA NA 35.5626924599 7.05290132 34.9130816841 0.6925857464 Spot 97 226.061955597 217.2177797733 10178.2658589147 182.1713626047 1.0407157086 21.1752995169 3.3496330504 0.0017930221 11.1357855327 0.0353631261 3.5469828958 0.0054333536 1.1666388004 0.328910185 34.9308373609 0.4064145996 35.2868068188 1.230119134 59.5968135463 NA 36.1902341176 4.0264592987 34.9308373609 0.4064145996 Spot 121 259.7931566979 384.6115488839 2526.7294841352 100 0.6754689438 21.2628176674 3.7605215721 0.0017526279 18.1098346672 0.0352256987 4.1124112202 0.0054346075 1.6644529281 0.4047389327 34.9388772502 0.5799680648 35.1520224903 1.4208600437 49.7581367406 NA 35.3756328483 6.4008629443 34.9388772502 0.5799680648 Spot 39 437.2162911792 240.9746506023 4020.9477902098 100 1.8143663248 21.5868125823 4.5254077256 0.0016196199 19.1241596817 0.0347423938 4.7179132329 0.0054417178 1.3339378512 0.2827389537 34.9844649089 0.4654070042 34.6778705695 1.6084505708 13.4759829608 NA 32.6931252117 6.2472293304 34.9844649089 0.4654070042 Spot 96 417.2787917473 165.9556445484 13446.171124776 100 2.5143995125 20.1171212867 2.8160115412 0.0017034487 16.0565128725 0.0373007883 3.0039916536 0.0054446705 1.0459659911 0.348192043 35.0033961276 0.3651314087 37.1853007372 1.0968370291 180.3671580327 65.640591986 34.3838285045 5.5161484145 35.0033961276 0.3651314087 Spot 73 349.4463552656 178.4400811946 7234.9341557894 100 1.9583400373 22.322695123 2.6328443819 0.0015812107 16.2617396704 0.0336425671 2.8654701259 0.0054490841 1.1309507078 0.3946824284 35.0316940703 0.3951166307 33.5980469733 0.946988409 NA NA 31.9184220589 5.1863925859 35.0316940703 0.3951166307 Spot 17 238.2433755924 116.3483981581 16138.2263473051 146.2842676135 2.0476721585 20.9509009644 3.2040802774 0.0017832959 9.8353824125 0.0358538159 3.3941100412 0.0054503682 1.119755575 0.329911394 35.039927177 0.3912971139 35.767913449 1.1928695244 84.9300872284 76.0206355468 35.9940948576 3.5370050211 35.039927177 0.3912971139 Spot 47 458.4040017767 734.723015532 17689.0167432253 501.4400875686 0.6239140357 20.7509174296 2.3876439212 0.0016984783 4.6939878891 0.0362035942 2.6510799296 0.0054510071 1.152120349 0.4345852934 35.0440232313 0.4026538773 36.1107215014 0.9405014106 107.6329993975 56.3838478886 34.2835853138 1.6079026246 35.0440232313 0.4026538773 Spot 41 680.0499877921 824.5933441933 8974.1730790229 206.9486454976 0.8247095281 21.2846647556 1.7955256669 0.0017863252 7.2166046665 0.0353026008 2.0266422814 0.0054520681 0.9398757984 0.4637600858 35.0508258602 0.328540241 35.2274477544 0.7016919202 47.2972756321 42.8926738252 36.0551846344 2.5996396316 35.0508258602 0.328540241 Spot 129 634.3527973003 1029.6529453566 14500.5802937136 420.9577306511 0.6160840895 21.3480839738 2.0652006063 0.0017257354 5.1021467801 0.0352187389 2.3391543636 0.0054553228 1.0984487207 0.4695922329 35.0716935929 0.3841985071 35.1451959943 0.8080357214 40.1932819962 NA 34.8332933379 1.775714433 35.0716935929 0.3841985071 Spot 25 461.007265856 306.7508881288 5293.6986262632 100 1.5028718211 23.8986759392 2.2876132328 0.0016157011 14.0380276716 0.031512723 2.5666730935 0.0054644635 1.163888511 0.4534619208 35.1302978168 0.4077654149 31.5036684642 0.7961811664 NA NA 32.6140856395 4.5746807756 35.1302978168 0.4077654149 Spot 11 182.9723988768 94.6466891876 4400.2960311794 100 1.9332149962 22.4713400253 4.8876117757 0.0020815829 19.5096586707 0.0335145777 5.0257403687 0.0054645006 1.1701783558 0.2328370091 35.1305358808 0.4099718169 33.4723107395 1.654807533 NA NA 42.0084738801 8.187195059 35.1305358808 0.4099718169 Spot 61 165.5169698375 117.7693352753 1769.9486725369 100 1.4054335065 25.5202365407 4.6467303878 0.0017532353 12.9354058024 0.029534241 4.9684107487 0.0054688784 1.7586932851 0.3539750182 35.158603443 0.6166488764 29.5542537596 1.4472138741 NA NA 35.3878833432 4.5735594715 35.158603443 0.6166488764 Spot 105 484.997923183 837.2353071381 23262.1073412787 717.2786653204 0.5792850816 21.270722106 2.3005238139 0.0017594312 6.6276592715 0.0354485376 2.7119790388 0.0054710201 1.436112979 0.5295442769 35.1723349253 0.503738991 35.3705666288 0.9427274848 48.8231278198 NA 35.5128332877 2.3516020697 35.1723349253 0.503738991 Spot 87 371.8180226292 192.2445746461 4001.207772541 100 1.9340885084 21.4791484551 2.556644619 0.002109197 21.34397655 0.0351095153 2.8768418503 0.0054717929 1.3190099787 0.4584923494 35.177289167 0.4627282813 35.0380596003 0.9907967411 25.5197914453 NA 42.5651676538 9.0755356892 35.177289167 0.4627282813 Spot 66 96.7668993176 85.3843484175 1566.399199326 100 1.1333095715 27.3078413157 4.7795665471 0.0017904298 13.5117647397 0.0276271802 5.0056882675 0.0054740869 1.487500808 0.2971620941 35.1919968707 0.522054952 27.6716617545 1.3664537942 NA NA 36.1379573774 4.8785111657 35.1919968707 0.522054952 Spot 2 99.5815955923 83.2656079405 1314.7149707865 100 1.1959511022 30.5656010861 4.7330912065 0.0017271973 11.2093061651 0.0247107241 4.9826399636 0.0054803231 1.55709622 0.3125042611 35.2319793962 0.5470994111 24.7858580843 1.2200392891 NA NA 34.862776391 3.904505406 35.2319793962 0.5470994111 Spot 102 207.2479967658 92.8139418485 2487.8357318425 100 2.2329403604 23.0001739721 4.1503499842 0.0017907197 11.0190720061 0.0328506674 4.3798127681 0.0054823035 1.3990549995 0.3194326045 35.2446758929 0.4917469048 32.8198381599 1.4144656312 NA NA 36.1438036675 3.9791511559 35.2446758929 0.4917469048 Spot 30 144.6158512887 97.3200357262 2773.8724598036 100 1.4859823079 18.6941550673 4.9444613543 0.0018707643 17.8447558512 0.0404343769 5.1596637794 0.0054845923 1.4745956162 0.2857929662 35.2593502204 0.5185135086 40.2480540941 2.0360477421 348.788685103 111.8717761226 37.7579107599 6.7315146232 35.2593502204 0.5185135086 Spot 83 356.068280164 173.7606838974 8180.9352044673 100 2.049187838 17.8699402283 4.7663700727 0.0017482259 19.5628506018 0.0423229458 4.8645815322 0.0054876543 0.9725583852 0.199926423 35.2789811953 0.3421715433 42.0894797285 2.005624158 449.7896343502 105.9461570143 35.286860026 6.897090651 35.2789811953 0.3421715433 Spot 59 621.1419919033 773.9543127421 52824.9749095027 1281.6032526658 0.8025564063 16.7303149389 4.6922545847 0.001875857 4.4068219612 0.0452342323 4.9234970678 0.0054910967 1.4911640721 0.3028668549 35.301051595 0.5249579331 44.9215677891 2.1635047388 594.3581811511 101.7454647282 37.8606023281 1.6668868977 35.301051595 0.5249579331 Spot 23 237.2014151505 375.9919915408 49741.1746405229 1446.4553264129 0.6308682645 22.1552228945 3.2718575817 0.0018650871 6.0792565778 0.0341604668 3.6799534125 0.0054914581 1.6843411422 0.4577071918 35.3033684397 0.5930039051 34.1066704654 1.2342647062 NA NA 37.6434334972 2.2863101573 35.3033684397 0.5930039051 Spot 101 199.7893214708 41.6559677975 2934.711020287 100 4.7961752429 25.2429669615 4.9317245869 0.0017373391 17.390146158 0.0300085836 5.121119578 0.0054963408 1.3798399657 0.2694410753 35.3346720177 0.4862281308 30.0219685753 1.5149552427 NA NA 35.0673056857 6.0929661857 35.3346720177 0.4862281308 Spot 20 490.3157282412 159.5279471906 69364.2895389022 439.7408519009 3.0735412627 20.4909568194 2.3318581355 0.0018973707 8.5156952658 0.0369963079 2.5158950354 0.0055005786 0.9445451102 0.3754310482 35.3618417352 0.3330941172 36.8872100914 0.9113888695 137.302827118 54.8088343797 38.294403777 3.2579459451 35.3618417352 0.3330941172 Spot 88 567.3168055887 159.5307293304 16305.8576206779 100 3.556160045 22.3585496035 2.0551524277 0.0017436259 14.0063926697 0.0339770808 2.3161784805 0.0055121045 1.0681906442 0.4611866716 35.435735573 0.3774827566 33.9265982485 0.7728178914 NA NA 35.1940919564 4.9251315136 35.435735573 0.3774827566 Spot 8 346.2064537015 566.5761613579 3387.3163602536 100 0.6110501594 23.4966720974 3.109629478 0.0015545784 5.5078227267 0.03234635 3.3357392293 0.0055146683 1.2072119597 0.3619023781 35.4521717455 0.4268081626 32.3239286979 1.0612605378 NA NA 31.3812378726 1.7270812092 35.4521717455 0.4268081626 Spot 57 1837.969317052 1906.5693131985 100124.160394818 1726.647254781 0.9640191439 21.2036626322 1.306321339 0.0016374891 2.7219061898 0.0358672007 1.5729281715 0.0055181833 0.876143591 0.5570143677 35.4747069005 0.3099557436 35.7810336038 0.5530090584 56.3965803026 31.1651131041 33.0535320937 0.8989505272 35.4747069005 0.3099557436 Spot 46 206.7726411414 155.0723665799 14771.5882036313 203.5070152927 1.3333945028 21.0363759521 3.4886850751 0.0018018226 10.6060156174 0.0361644444 3.8491105426 0.0055200178 1.6262620995 0.4225033502 35.4864676758 0.5755174572 36.0723575444 1.3640920167 75.2163144644 NA 36.3677031501 3.8536945688 35.4864676758 0.5755174572 Spot 21 119.323027604 89.943302299 2070.8472080237 100 1.3266471717 24.0163448336 6.7900645644 0.0018439554 23.6359793008 0.03168412 7.052312028 0.0055212361 1.9052895191 0.2701652326 35.4942781618 0.6744103917 31.6723714006 2.1991609404 NA NA 37.2173207501 8.7885808841 35.4942781618 0.6744103917 Spot 62 1055.836687305 761.7810509825 19831.0186037732 255.5980816787 1.3860106995 21.0261387004 1.9414677721 0.0016659075 7.5215803059 0.0362045928 2.0980884236 0.0055234566 0.7954105375 0.3791120186 35.508514155 0.2816620178 36.1116999721 0.7443409805 76.3731940919 46.1131330585 33.6266948856 2.5271550379 35.508514155 0.2816620178 Spot 65 259.1581034394 294.0001311151 3238.8515689194 100 0.8814897546 20.9737377445 3.9994069995 0.0017522933 11.9962576845 0.0363345462 4.1840520141 0.0055294677 1.229241599 0.2937921409 35.5470514401 0.4357566076 36.2390341564 1.4895224813 82.2986783048 NA 35.3688862366 4.239230775 35.5470514401 0.4357566076 Spot 89 140.5130936612 68.053846543 7822.9336538089 100 2.0647340422 24.4427190459 3.4720068501 0.0016482913 18.1812221304 0.0312143979 3.9268933908 0.0055359509 1.8345735568 0.4671819105 35.5886149095 0.6511004071 31.2099658523 1.2069387224 NA NA 33.2714003996 6.0441688523 35.5886149095 0.6511004071 Spot 64 313.1266403855 196.9993769409 7377.6034447426 100 1.589480359 22.3323294608 2.6306882773 0.0015821517 17.93890854 0.0341789499 2.8398995861 0.0055383513 1.0698172023 0.3767095173 35.6040031282 0.3798478218 34.1248178078 0.9530068998 NA NA 31.9374022157 5.7246952452 35.6040031282 0.3798478218 Spot 75 313.5811098667 210.9115226231 15748.8962024604 187.0311174062 1.4867898442 23.0190190692 3.2423693191 0.001699211 12.024442542 0.0332267074 3.4228229737 0.0055496025 1.096703382 0.320409028 35.6761331115 0.3901806823 33.1894512684 1.1176509909 NA NA 34.2983636345 4.1206881072 35.6761331115 0.3901806823 Spot 63 230.6299082588 140.3378616209 5110.2638403896 100 1.6433904977 23.2513987396 3.5564779382 0.0017093739 15.625908199 0.0329980889 3.7280254246 0.0055670565 1.1178721937 0.2998563761 35.7880270138 0.398955953 32.9647561845 1.2092003168 NA NA 34.5033250499 5.3868565708 35.7880270138 0.398955953 Spot 52 2262.784395911 629.1750426856 82660.9356977386 411.0139809485 3.5964306312 21.0619579171 1.0957062517 0.0017839872 6.3538150132 0.0365239154 1.5038446108 0.0055816657 1.030037098 0.6849358575 35.8816821413 0.3685679348 36.424557889 0.5380602589 72.3428154281 26.0441061905 36.0080356483 2.285846236 35.8816821413 0.3685679348 Spot 58 104.4190580719 53.805552831 888.9324605063 100 1.9406743836 31.1795867624 5.0662800174 0.0015186233 19.813637047 0.024684312 5.3862056143 0.0055844337 1.8286655532 0.3395090504 35.8994263931 0.6546558985 24.7596860792 1.317479973 NA NA 30.6559879482 6.0694600872 35.8994263931 0.6546558985 Spot 53 720.220433632 202.144411228 21490.1801128983 114.1409592805 3.5629005485 19.4444619936 2.3683048131 0.001728771 16.6177942719 0.0396921809 2.6177593445 0.005600008 1.115256158 0.4260346393 35.9992667526 0.4003651027 39.523470029 1.0147520989 259.0620210806 54.4211583906 34.8945139288 5.7936935944 35.9992667526 0.4003651027 Spot 98 114.6344819204 93.1607288541 3343.1911455544 100 1.2305022012 21.8547744465 4.5230323359 0.0020133352 16.0160169738 0.0353672339 4.7279024603 0.0056083509 1.376677218 0.2911813917 36.0527487276 0.4949446549 35.2908353109 1.6398550984 NA NA 40.6325480329 6.5011758791 36.0527487276 0.4949446549 Spot 4 199.9892558533 139.0810315868 5822.4876960545 100 1.4379333657 13.5662330222 5.4446293481 0.0019757849 19.6419308993 0.0572802924 5.5638309752 0.0056383529 1.145524501 0.2058877249 36.2450724575 0.4140311467 56.5566827324 3.0606963314 1032.7064583884 110.1204925926 39.8754670404 7.8245873085 36.2450724575 0.4140311467 Spot 38 209.2641060853 100.9579923117 7243.8307714189 100 2.07278395 23.0803921773 4.2747543543 0.001696167 19.5486224464 0.0337125377 4.4254611474 0.0056457596 1.1450683723 0.2587455486 36.2925515571 0.4144069044 33.6667792032 1.4654817224 NA NA 34.236972748 6.6871886934 36.2925515571 0.4144069044 Spot 91 234.8200283982 198.1351257953 5984.6472399547 100 1.185150929 23.1201876652 3.313889919 0.001505381 18.7201601982 0.0337688997 3.4712264875 0.0056649492 1.0332216279 0.2976531873 36.4155597681 0.3751927171 33.7221402385 1.151347693 NA NA 30.388870542 5.6845688224 36.4155597681 0.3751927171 Spot 70 441.0600220381 333.3768543608 6526.5407247885 100 1.3230073302 18.7022829807 4.0239572543 0.0018928281 18.1232411676 0.0420102432 4.7003498523 0.0057008232 2.4292090789 0.5168145256 36.6455118774 0.8876706748 41.7848135781 1.9241716992 347.7624910661 91.015641937 38.2028082293 6.9170450764 36.6455118774 0.8876706748 Spot 5 98.2165360208 67.8661953896 10900.0755091113 140.7068526753 1.4472085175 21.1886700255 4.6908839915 0.0017823504 20.115694658 0.0372012147 4.8870292906 0.005719375 1.3706431577 0.2804655091 36.7644253334 0.5024748918 37.0878264258 1.7797926218 58.0458124331 NA 35.9750283452 7.2301876248 36.7644253334 0.5024748918 Spot 49 286.949439119 179.592025449 19529.7543122833 251.0908962465 1.5977849707 19.8288331022 2.5125286577 0.0020286779 11.5534070711 0.0399162044 2.7229489992 0.0057429383 1.0495956346 0.3854628327 36.9154584351 0.3863557498 39.7422320574 1.0612567573 213.9491216854 58.1988486212 40.9418777563 4.7253919748 36.9154584351 0.3863557498 Spot 90 140.2777713575 57.2530614357 90034.8145342666 1236.2016954462 2.4501357279 10.3862659455 9.2004488364 0.0034713709 12.2775243091 0.0764066324 9.3207551634 0.0057580874 1.4927216841 0.1601502945 37.0125574088 0.5509114092 74.7609295737 6.7180315865 1552.4271291091 173.1162369375 70.0072643446 8.5802839437 37.0125574088 0.5509114092 Spot 127 104.3897598221 83.8820000924 1349.9405147654 100 1.2444834375 23.534339003 5.6300700956 0.0016820206 13.4354348533 0.0342781993 5.8507922119 0.005853394 1.5918794633 0.2720793024 37.6233969815 0.5971747822 34.2222586499 1.9689095179 NA NA 33.9516688625 4.5577234839 37.6233969815 0.5971747822 Spot 29 219.2952121004 165.7141414949 10513.0313496994 223.3898222585 1.3233343282 9.4950419872 9.9403305966 0.0030191403 10.6447253715 0.0858241705 10.0052270966 0.0059128146 1.1377156435 0.1137121259 38.0042061211 0.4311077733 83.6059326902 8.0300088702 1719.0587194041 183.1404387575 60.9008451733 6.4729663616 38.0042061211 0.4311077733 Spot 14 812.2342308576 166.783561577 29894.486667005 101.6891792894 4.8699897231 21.6543850686 1.2986082633 0.0023416089 16.1226473496 0.0554256609 1.7143357824 0.0087085227 1.1191799469 0.652835902 55.8957117091 0.6228693016 54.7739814575 0.9141325001 5.9564872791 NA 47.2499305807 7.6090382904 55.8957117091 0.6228693016 Spot 116 75.3244362848 52.2784714004 523.0295344973 100 1.4408308863 2.3249409631 7.2578169741 0.0156867871 6.7557124023 0.6428296721 7.4463133343 0.0108441521 1.6648348394 0.2235784024 69.5295786716 1.1513324931 504.0566227026 29.5935823123 4017.2161105498 108.5559294645 314.4448723911 21.078529516 69.5295786716 1.1513324931 Spot 24 601.411955034 97.092878122 35435.8419344391 184.234625028 6.194192269 13.1863867511 2.3198251931 0.0084094045 8.5379957729 0.1752136169 3.4481913504 0.0167641454 2.5511633939 0.7398555169 107.1727836285 2.7115505252 163.933525622 5.2200676928 1089.8469290549 46.4650223889 169.1766144374 14.3839830898 107.1727836285 2.7115505252 Spot 122 188.6955472999 250.1365164358 10758.0530574895 255.9290033034 0.7543702534 20.4925173094 1.560386059 0.0076319259 4.2915891735 0.1646570791 1.7290871469 0.0244829346 0.744941413 0.4308293045 155.9260676536 1.1476225469 154.7714789138 2.4821612689 137.1522320922 36.6503852367 153.5949517667 6.5666698893 155.9260676536 1.1476225469 Spot 99 490.0267919632 286.7446616455 250891.458789318 4464.0309044869 1.7089308277 11.4902108005 0.7721116688 0.0276007298 2.3643259502 0.7881990626 1.5653262876 0.065713056 1.3616497191 0.8698823561 410.2763017163 5.412464824 590.1497721781 7.0058644817 1360.3146983668 14.8790364487 550.0342708947 12.829164364 410.2763017163 5.412464824 Spot 10 211.1908659085 83.0109292159 38885.891380595 451.6771438701 2.5441332594 11.9460517546 0.7843633565 0.039516088 4.0695924158 0.8678943661 1.2467909891 0.0752279133 0.9691552484 0.7773197407 467.5755133545 4.37109363 634.4233020515 5.8822432618 1284.949165503 15.2752943247 782.9354517313 31.2527898425 467.5755133545 4.37109363 Spot 27 142.9627045485 51.903467413 31175.9338861941 100 2.7543960293 13.3776906207 0.9493358623 0.0131479579 17.6623502051 0.9001734093 1.2107705318 0.0873765881 0.7514830013 0.6206650902 540.0031932577 3.8927142393 651.8202265048 5.8241085325 1060.964640301 19.1182760349 263.8843185293 46.3051702998 540.0031932577 3.8927142393 Spot 71 163.2688909206 91.0276021292 56790.9084658117 564.091574891 1.7936195956 14.6857635295 0.6205096918 0.0443681328 3.3983130577 1.3184686878 1.0524535177 0.1404928122 0.8500741905 0.8077071112 847.4485760206 6.7505125318 853.8426353273 6.0772430538 870.484320916 12.863716037 877.0110080468 29.1659433095 847.4485760206 6.7505125318 Spot 72 50.112761527 30.3337305702 28494.1369689901 290.3380821394 1.6520474266 13.2481692722 1.3994976048 0.0547625054 4.5412933866 1.9487084394 1.6051779062 0.1873227345 0.7861313914 0.489747204 1106.8555652723 7.9953093538 1098.0019874309 10.7717039539 1080.5073388138 28.0606797685 1077.0833978882 47.6325455646 1080.5073388138 28.0606797685 Spot 3 184.8664046559 99.5264814966 117359.608853592 1060.8976880367 1.8574594608 13.022934856 0.7795903491 0.0561010207 3.3712450133 1.9517860745 1.1805528352 0.1844288413 0.886534762 0.750948823 1091.1243699437 8.8988546728 1099.0612135172 7.9263180773 1114.8293226232 15.5601230519 1102.7039234291 36.1785271588 1114.8293226232 15.5601230519 Spot 60 397.6546922354 147.9991866716 619633.295812813 4833.328766449 2.6868707942 12.9659812694 0.698526899 0.0509697838 2.2843014186 1.8689533696 1.2512714032 0.175829447 1.0381427146 0.8296702953 1044.1502716428 10.0074376466 1070.1602108846 8.2768679279 1123.5528014877 13.9306848223 1004.3099299944 22.3805600342 1123.5528014877 13.9306848223 Spot 76 322.8953814956 106.8768453037 428982.079643642 2760.0198253255 3.0211911717 12.7396661547 0.6443609238 0.0464482211 4.3485338943 1.9115308084 1.5312232816 0.1766961569 1.3890441814 0.9071467226 1048.9002061426 13.4461410798 1085.1185397249 10.2080544446 1158.5481319353 12.7910321386 917.2077486042 38.9932596838 1158.5481319353 12.7910321386 Spot 128 139.8773570288 62.1387470245 129410.535061929 922.2001182078 2.2510488822 12.6176241802 0.7137020266 0.0569288342 3.2109809178 2.1043111338 1.0689504187 0.1926527866 0.7957916905 0.7444608063 1135.7296275801 8.2866522235 1150.2176308017 7.3576611692 1177.6488089443 14.1334928502 1118.5328590928 34.9397266518 1177.6488089443 14.1334928502 Spot 79 115.9253374446 42.3976424082 153400.546195356 940.4345237053 2.7342401808 11.7716327539 0.6126451601 0.0666176055 3.5286121688 2.6225658184 0.9635732636 0.2240014634 0.7437333811 0.7718493333 1302.9839141687 8.7741421612 1306.9833623162 7.0832375685 1313.5340276298 11.8834515049 1302.8792974875 44.5225163593 1313.5340276298 11.8834515049 Spot 51 128.6276990649 99.6049623841 165172.356763038 2080.7433862163 1.2913784212 11.4595299085 0.6850473128 0.0664930866 2.6809094474 2.7543718033 0.9437544144 0.2290219566 0.6491398723 0.687827111 1329.3711255318 7.7978375256 1343.2715389892 7.0304177403 1365.4676613871 13.192113848 1300.5207399703 33.7672582832 1365.4676613871 13.192113848 Spot 43 200.8408440602 73.8798053094 31217.8233971393 192.7582220512 2.71848096 11.1832458281 1.4038132279 0.059452271 8.2467297338 2.4805913077 1.6181196512 0.2012847366 0.804748176 0.4973353951 1182.2181975548 8.6924730778 1266.387973143 11.7101371853 1412.3092703293 26.8595474315 1166.7080627132 93.4903349543 1412.3092703293 26.8595474315 Spot 7 181.8477633677 111.8808181823 76961.8157385693 787.1372330767 1.6253703389 9.8568649821 0.6701605919 0.0832515822 2.5707825562 3.9212627145 1.1710731799 0.2804481 0.9603630426 0.8200709052 1593.618660812 13.5595353251 1618.0790443799 9.4749284857 1650.0308961752 12.4252825552 1615.4998436825 39.9138733241 1650.0308961752 12.4252825552 Spot 67 174.2329167529 46.9256970433 95368.7626944078 408.3902406338 3.7129531948 9.4630463994 0.6443853801 0.0872627405 2.5687281033 4.4773846984 1.0600797708 0.3074277982 0.8417461626 0.7940403976 1728.0367070297 12.759255611 1726.7885893614 8.7989428108 1725.2599391098 11.8340080464 1690.1674848649 41.6493181578 1725.2599391098 11.8340080464 Spot 9 162.5092523291 102.8051804056 306001.636026249 4015.8903174929 1.580749644 7.8709114923 0.5165831609 0.1083965187 2.4734829168 6.7646376027 0.9672698457 0.3863290077 0.8177730689 0.8454446012 2105.7808343286 14.6907094537 2081.1085798813 8.5567961325 2056.7678483342 9.1179421246 2079.0786506293 48.8680202247 2056.7678483342 9.1179421246 Spot 16 70.3221545621 56.3032841369 130794.281290025 1588.4810287277 1.2489885029 5.5022741756 0.592577149 0.1425051142 2.7120239021 12.6992468722 0.8994059793 0.5069999863 0.6765969539 0.7522709093 2643.8092542633 14.6738370849 2657.6035523084 8.4659757189 2668.1074040007 9.8148348441 2691.3802042578 68.3380005824 2668.1074040007 9.8148348441 Spot 56 119.2087688534 163.9056879418 584243.778495725 16491.29886178 0.7273009885 4.887019209 0.5940469034 0.1581711776 1.9171170787 15.9852730922 0.8882444785 0.5668287379 0.6603684806 0.743453516 2894.7859109992 15.4005311673 2875.9168197365 8.4882872916 2862.7170192413 9.6652611523 2966.5088882093 52.8931004196 2862.7170192413 9.6652611523 Spot 28 636.7812377381 563.3062423686 593775.649910125 10860.6473150346 1.1304352586 4.8693506138 0.4721959092 0.1505128698 2.1832867446 15.4732899353 1.0337992942 0.5466904212 0.9196586345 0.8895910838 2811.3936242527 20.9548451764 2844.8395973471 9.860118037 2868.6084008418 7.6786073889 2832.481146087 57.701740797 2868.6084008418 7.6786073889 Spot 114 146.225139124 174.8450490054 212742.12104864 5169.7079740618 0.8363127235 4.8635279785 0.4407019345 0.1543897598 2.2354609878 15.8288338643 0.9071292357 0.5585834884 0.7928841373 0.8740586304 2860.7728508042 18.3183826467 2866.5215176849 8.6637220671 2870.5538851421 7.1652062937 2900.4415735598 60.3989260109 2870.5538851421 7.1652062937 Spot 120 116.6896501908 164.2962384899 271302.196182043 7745.9535045944 0.7102393291 4.8498744993 0.4529013124 0.1509066041 2.3018892562 15.6491023607 0.9139206172 0.5506906289 0.7938080975 0.8685744501 2828.0444720623 18.1726141063 2855.6189294824 8.7226345288 2875.1236540474 7.360526334 2839.3935995855 60.9745648711 2875.1236540474 7.360526334 Spot 37 320.0480757539 342.3125048751 2147081.15830581 46255.4566004289 0.9349587619 4.8498601965 0.4638508746 0.1553846845 1.6837135148 15.9909912902 0.9728636038 0.5627200128 0.8551642869 0.8790176584 2877.8591516332 19.8509054519 2876.2585972413 9.2971678751 2875.1284468671 7.5384769087 2917.8454289068 45.7451804728 2875.1284468671 7.5384769087 Spot 45 234.8887131817 166.2540424266 503022.562148405 7206.4611819759 1.4128300867 4.8338071211 0.4762689074 0.1533788253 2.4139130695 15.9258879624 1.0210708503 0.5585740142 0.9031907933 0.8845525196 2860.7336650319 20.8666398786 2872.3605442096 9.755540718 2880.5154381372 7.7329666667 2882.7422927689 64.850204822 2880.5154381372 7.7329666667 1.            Analyses with >10% uncertainty (1-sigma) in 206Pb/238U age are not included. 238U* (Ma) 235U (Ma) 207Pb* (Ma) (Ma) (Ma) (%) Base of Markagunt landslide-Spot 115 68.6017221178 732.6316127872 0.7081656692 38.7781759448 5.5222976291 0.0182315753 5.7343441027 0.0051297869 1.5449696385 0.2694239499 32.9842023545 0.5082944155 18.3453042417 1.0425369304 NA NA 32.9842023545 0.5082944155 NA Base of Markagunt landslide-Spot 44 158.7513200224 1292.4220318755 1.5549908648 26.54083024 8.177146828 0.0267708886 8.2531166602 0.0051554318 1.1172306658 0.1353707589 33.1486740186 0.3693965845 26.8252201408 2.1849313968 NA NA 33.1486740186 0.3693965845 NA Base of Markagunt landslide-Spot 55 261.1685231606 9398.7413523873 2.2221800844 22.0182323921 2.266809702 0.0322884752 2.5862914467 0.0051584324 1.245181602 0.4814544794 33.1679177497 0.4119401497 32.2670033046 0.8213985392 NA NA 33.1679177497 0.4119401497 NA Base of Markagunt landslide-Spot 127 134.5722158521 4467.1066787243 0.6532926385 23.9407715537 3.1963127108 0.0297250212 3.4237856542 0.0051635462 1.2271484266 0.35841859 33.2007145313 0.4063746805 29.7423941554 1.0035465615 NA NA 33.2007145313 0.4063746805 NA Base of Markagunt landslide-Spot 83 86.2284784031 7992.7327767651 0.7919335565 20.3230331974 3.4712621316 0.0351301378 3.8787397259 0.0051803146 1.7305955839 0.446174713 33.3082541125 0.5749445443 35.0582888911 1.3366130587 156.6164932432 81.2767451798 33.3082541125 0.5749445443 NA Base of Markagunt landslide-Spot 56 904.4690290409 45513.126872985 1.1939947496 21.1678179778 1.7742065758 0.0337326389 1.9515428917 0.0051810068 0.8128411187 0.416512044 33.3126935108 0.2700808306 33.6865237371 0.6466215265 60.4396898261 42.2757016336 33.3126935108 0.2700808306 NA Base of Markagunt landslide-Spot 38 314.264990861 5191.9232290652 3.5480964084 22.4992990467 1.6246023022 0.031776683 1.9537559147 0.0051875859 1.0852785512 0.5554831814 33.3548865222 0.3610585337 31.7634677784 0.6109745525 NA NA 33.3548865222 0.3610585337 NA Base of Markagunt landslide-Spot 110 128.7004919882 1849.1651324876 1.3018078603 23.1401927817 4.242472452 0.03091324 4.4123686119 0.0051903812 1.212610515 0.2748207645 33.3728126725 0.4036365301 30.9133879733 1.3434588187 NA NA 33.3728126725 0.4036365301 NA Base of Markagunt landslide-Spot 68 423.2142327032 24793.8314355648 1.5156594295 21.6732964442 1.4349374558 0.0330560014 1.7386569302 0.0051983204 0.9817751367 0.5646744448 33.4237278314 0.3272966238 33.0216795329 0.5648983486 3.8549719951 34.540642909 33.4237278314 0.3272966238 NA Base of Markagunt landslide-Spot 65 671.9688849524 10672.5230195806 0.4605623397 19.8525087604 1.4122311908 0.0360926907 1.7494716888 0.005199031 1.0325958811 0.5902329759 33.4282851725 0.3442856672 36.0020405049 0.6188102986 211.1406157225 32.7482396029 33.4282851725 0.3442856672 NA Base of Markagunt landslide-Spot 126 90.5995787905 5563.1301795239 1.4386383309 22.3191228678 3.4950133546 0.0321529415 3.7399304023 0.0052069761 1.3311502791 0.355929158 33.4792374931 0.4445037073 32.1336804604 1.1829606085 NA NA 33.4792374931 0.4445037073 NA Base of Markagunt landslide-Spot 106 199.4981054009 6624.2547722868 1.2616229751 22.1778528546 2.7432150021 0.0323684042 2.9703424008 0.0052086904 1.1391687455 0.3835142862 33.490230812 0.3805209509 32.3456203209 0.9456341232 NA NA 33.490230812 0.3805209509 NA Base of Markagunt landslide-Spot 75 208.120149894 1726.9943551539 1.9543605932 24.3649694553 4.1417935237 0.0294740491 4.3074312719 0.0052106683 1.1830091164 0.2746437591 33.5029153327 0.3953144013 29.4948873793 1.252197655 NA NA 33.5029153327 0.3953144013 NA Base of Markagunt landslide-Spot 103 226.1154937511 6948.5879005492 0.6361446134 19.8189841719 2.1430397773 0.0362457094 2.447310544 0.0052122561 1.1818246112 0.4829074978 33.513098124 0.3950383057 36.1519895812 0.8691864689 215.0550454026 49.6490540104 33.513098124 0.3950383057 NA Base of Markagunt landslide-Spot 8 262.0099629445 14478.5672414809 1.360161154 18.7816220732 2.594754513 0.0383454552 2.8553221955 0.005225583 1.1916853014 0.4173558078 33.5985625267 0.3993475325 38.2073796628 1.0706739208 338.1812094174 58.7616947521 33.5985625267 0.3993475325 NA Base of Markagunt landslide-Spot 122 214.8772582346 3052.141037693 1.7483684789 23.451676013 6.2614310409 0.0307745081 6.4556483015 0.0052366405 1.5715840139 0.2434432516 33.6694728961 0.5277646038 30.7767368851 1.9570312555 NA NA 33.6694728961 0.5277646038 NA Base of Markagunt landslide-Spot 37 195.9248592169 2428.3274565225 1.0869240737 23.6536426962 6.4032139158 0.0305438463 6.4860516689 0.0052421508 1.0333043117 0.1593117608 33.7048095939 0.3473643697 30.5494938653 1.9519473595 NA NA 33.7048095939 0.3473643697 NA Base of Markagunt landslide-Spot 92 246.4787285165 87946.4501312177 0.8077410176 19.9975302831 1.633256149 0.0361973992 1.9911396937 0.0052522028 1.1389080873 0.5719880383 33.7692703592 0.3835953503 36.1046509111 0.7062632042 194.290649303 37.9608067929 33.7692703592 0.3835953503 NA Base of Markagunt landslide-Spot 50 97.1243149375 1953.8895049727 2.3843595406 25.4459664299 4.0127272484 0.0284664766 4.3541013634 0.0052558192 1.6900351218 0.3881478589 33.7924617434 0.5696102049 28.5006195011 1.2236923138 NA NA 33.7924617434 0.5696102049 NA Base of Markagunt landslide-Spot 25 109.828534103 12327.7198874827 0.770615622 19.9828596423 2.4428808129 0.0363015245 2.6819481689 0.005263447 1.1068781842 0.412714234 33.841376307 0.3736013171 36.2066794853 0.9539357955 195.996336121 56.7564962868 33.841376307 0.3736013171 NA Base of Markagunt landslide-Spot 10 207.0563797574 9727.4775503979 1.7442186431 21.6564934139 2.0631987086 0.0335287868 2.3516505316 0.0052685818 1.1284818614 0.4798680103 33.8743041183 0.3812627802 33.486270435 0.7746366491 5.7337529418 49.6672865618 33.8743041183 0.3812627802 NA Base of Markagunt landslide-Spot 76 106.1658556809 66025.5995617255 2.1540285853 20.1815222136 3.6302684168 0.0359816391 3.8299428665 0.0052689323 1.2204972685 0.3186724479 33.8765513898 0.4123778924 35.8932028115 1.3506765099 172.9133496243 84.7363217991 33.8765513898 0.4123778924 NA Base of Markagunt landslide-Spot 86 170.2246621747 14511.6553938045 1.8278412401 19.9295351803 2.4408427694 0.036454892 2.7035680652 0.0052715792 1.1625690768 0.4300128751 33.8935252965 0.3930015905 36.3569400071 0.9655455336 202.158455261 56.6442148626 33.8935252965 0.3930015905 NA Base of Markagunt landslide-Spot 19 458.8678754574 2887.9715639255 0.6633744726 23.0380565745 1.074159063 0.0315512494 1.5653863279 0.0052741218 1.1386907671 0.7274183675 33.9098298353 0.3851143128 31.5415918009 0.4861577721 NA NA 33.9098298353 0.3851143128 NA Base of Markagunt landslide-Spot 80 403.4873477669 13480.1802840855 1.6628824871 20.7646656228 2.5447337941 0.0350342112 3.6227531497 0.0052784333 2.5785015612 0.7117519341 33.9374776958 0.8727789869 34.9641879315 1.2451065283 106.0232167861 60.1135228846 33.9374776958 0.8727789869 NA Base of Markagunt landslide-Spot 27 256.3930757374 4056.2686185619 1.8715448991 22.714739349 1.9402887797 0.0320433631 2.3587542122 0.005281212 1.3412683867 0.5686342306 33.9552961832 0.4542343062 32.02587668 0.7436230145 NA NA 33.9552961832 0.4542343062 NA Base of Markagunt landslide-Spot 45 127.5423950473 1085.2541323841 1.0878251736 30.4733359051 3.1798925802 0.0238879735 3.4154190873 0.0052818621 1.2463429383 0.3649165466 33.95946517 0.4221385156 23.9702693392 0.8090975213 NA NA 33.95946517 0.4221385156 NA Base of Markagunt landslide-Spot 119 172.5433565413 2841.3945768267 4.6716075007 23.1566573709 3.1216660716 0.0314521603 3.5369976628 0.0052846242 1.6629953108 0.4701714475 33.9771766303 0.5635523904 31.4440510894 1.0951314294 NA NA 33.9771766303 0.5635523904 NA Base of Markagunt landslide-Spot 33 319.4279070465 10504.9849928658 1.2466187191 21.3868992062 2.0851827687 0.0340564617 2.3245481549 0.0052848797 1.0273932769 0.4419754759 33.9788150403 0.3481776397 34.004548628 0.7773629091 35.7984091689 49.9267199596 33.9788150403 0.3481776397 NA Base of Markagunt landslide-Spot 36 261.0208401472 2850.9954894253 0.58949555 22.4764885723 6.1888970654 0.0324133008 6.334294524 0.0052861499 1.3493851308 0.2130284794 33.9869607949 0.4574081567 32.389777275 2.0192886513 NA NA 33.9869607949 0.4574081567 NA Base of Markagunt landslide-Spot 109 79.4781798938 17626.1600877405 0.9364211308 19.2150854117 4.51341808 0.037948553 4.7640203218 0.0052908481 1.5247776433 0.3200611123 34.0170878128 0.5173188305 37.8191804835 1.7685744548 286.2820836326 103.2337321712 34.0170878128 0.5173188305 NA Base of Markagunt landslide-Spot 13 407.1701364722 10334.6715138605 4.1568562291 22.6459558928 2.0002359907 0.0322064008 2.3255899352 0.0052920094 1.1863492439 0.5101283016 34.0245344072 0.4025864357 32.1862698298 0.7367816004 NA NA 34.0245344072 0.4025864357 NA Base of Markagunt landslide-Spot 39 186.1702014487 16120.0800888651 1.5737234929 21.8205143957 2.5069737085 0.0334401032 2.8435707027 0.0052944439 1.3420049056 0.4719435688 34.0401454864 0.4556164282 33.3991401283 0.9342785171 NA NA 34.0401454864 0.4556164282 NA Base of Markagunt landslide-Spot 52 145.3285040459 1745.375894573 0.8176454929 24.3044737418 3.1417060361 0.0300595299 3.5021080803 0.0053009799 1.5473991692 0.4418479195 34.082057654 0.5259937938 30.0721902311 1.0377182777 NA NA 34.082057654 0.5259937938 NA Base of Markagunt landslide-Spot 105 79.6497025205 2346.5833579364 1.4299659715 24.0585969704 4.44649148 0.0303944272 4.7697109936 0.0053058139 1.7259364072 0.361853456 34.1130551035 0.5872145616 30.4022622067 1.4286068362 NA NA 34.1130551035 0.5872145616 NA Base of Markagunt landslide-Spot 4 345.8415569891 212176.151068825 1.4648000626 20.6307030677 1.4567828975 0.035460954 1.8095028318 0.0053082601 1.0733518007 0.593174977 34.1287412527 0.3653534748 35.3827422971 0.629224931 121.3199052303 34.304293544 34.1287412527 0.3653534748 NA Base of Markagunt landslide-Spot 34 288.7681577271 7617.850132522 2.0714185058 20.0225420088 2.7831736808 0.0365448153 2.9651863231 0.0053092447 1.0228754532 0.3449616118 34.1350543715 0.3482362883 36.4450313085 1.0614993794 191.3839707849 64.736958565 34.1350543715 0.3482362883 NA Base of Markagunt landslide-Spot 9 161.8875665614 5127.216382508 1.05562636 18.4298698152 5.6465387672 0.0397081001 5.7342284762 0.0053099341 0.9989875711 0.1742148181 34.1394752143 0.340147628 39.539016892 2.223685063 380.8462465821 127.0164712467 34.1394752143 0.340147628 NA Base of Markagunt landslide-Spot 51 142.1944520814 25381.6754348654 2.6941508584 20.0624823597 2.8539426512 0.0364830604 3.0448725477 0.0053108457 1.0612540581 0.3485380887 34.1453208349 0.3614105999 36.3845353466 1.0882489296 186.702231641 66.4401574339 34.1453208349 0.3614105999 NA Base of Markagunt landslide-Spot 63 44.5519914424 1140.4102465087 1.00995908 23.262420876 8.3700883078 0.0314735099 8.4895951732 0.0053123642 1.4194533891 0.1671991844 34.1550579686 0.4835330453 31.4650678376 2.6302980465 NA NA 34.1550579686 0.4835330453 NA Base of Markagunt landslide-Spot 114 150.3147902313 2001.0152916561 1.9675392146 24.8064329687 2.7348093898 0.0295159464 2.9308786744 0.0053126204 1.0539769474 0.3596112513 34.1567008751 0.3590516854 29.5362103667 0.8532012603 NA NA 34.1567008751 0.3590516854 NA Base of Markagunt landslide-Spot 47 219.8847187393 5217.7770885877 1.8770640032 22.037576655 2.7404071202 0.033237359 3.2436017184 0.005314692 1.7352581719 0.5349788052 34.1699844369 0.5913687541 33.1999189189 1.0594586175 NA NA 34.1699844369 0.5913687541 NA Base of Markagunt landslide-Spot 40 347.0691188255 3535.7873261443 1.4414437292 22.1827534349 2.1913711501 0.0330253609 2.5122404537 0.0053155815 1.2285131581 0.4890109767 34.175688222 0.4187418657 32.9915627655 0.8155071963 NA NA 34.175688222 0.4187418657 NA Base of Markagunt landslide-Spot 66 253.3724899274 4595.0752748865 1.2894325542 23.6313605697 2.1979006261 0.0310047222 2.4429594419 0.0053162369 1.0664350297 0.4365340707 34.1798909909 0.363541702 31.0034880372 0.7459563841 NA NA 34.1798909909 0.363541702 NA Base of Markagunt landslide-Spot 43 179.46996584 2016.9086381296 2.8552348327 24.4047067345 2.9914886932 0.0300340307 3.1539192958 0.0053183262 0.9991007571 0.3167806984 34.1932880394 0.3407209693 30.0470540864 0.9337758903 NA NA 34.1932880394 0.3407209693 NA Base of Markagunt landslide-Spot 62 285.1363629541 3806.7870287697 1.3146410847 23.1180960611 2.6841248447 0.0317076973 2.8745857882 0.0053186881 1.0289398775 0.3579437016 34.195608788 0.3509206868 31.6955758348 0.8970431419 NA NA 34.195608788 0.3509206868 NA Base of Markagunt landslide-Spot 79 390.8279777249 26053.6165289206 0.7007061824 21.780753539 1.7326025277 0.033672471 2.1778168771 0.0053215193 1.3194600529 0.6058636366 34.2137634605 0.4502410783 33.6274221246 0.7203496998 NA NA 34.2137634605 0.4502410783 NA Base of Markagunt landslide-Spot 42 188.5901920564 2636.0210868583 1.506376597 23.4911286975 2.6806432186 0.0312225186 2.9725305569 0.0053218125 1.28455823 0.4321429857 34.2156436505 0.4383555079 31.2179617779 0.9138436541 NA NA 34.2156436505 0.4383555079 NA Base of Markagunt landslide-Spot 24 167.5386093288 2361.6783499929 3.958365821 23.9274172842 2.7268222003 0.0306748811 3.0210425915 0.0053255745 1.3004380138 0.4304600066 34.2397666247 0.4440865274 30.678592743 0.912952269 NA NA 34.2397666247 0.4440865274 NA Base of Markagunt landslide-Spot 100 207.4703430199 25295.3368667569 2.9680462358 20.2052217382 2.6414827076 0.0363513994 2.9067868783 0.0053293287 1.213251442 0.4173857571 34.2638395705 0.4146037059 36.2555464909 1.0352788666 170.1738696797 61.6671706469 34.2638395705 0.4146037059 NA Base of Markagunt landslide-Spot 48 161.1746623439 3501.91528091 3.1955439739 19.8083583138 3.9865359221 0.0370973127 4.1482450817 0.0053318594 1.1469387949 0.2764877128 34.2800667905 0.3921278532 36.9861049247 1.5066680479 216.3274862027 92.3442501402 34.2800667905 0.3921278532 NA Base of Markagunt landslide-Spot 15 113.8193080706 2082.8098960329 3.9684379817 25.0697388201 6.7997244206 0.0293500966 6.9383980954 0.0053388424 1.3802593724 0.1989305533 34.3248430437 0.4725127672 29.3726241679 2.0087973037 NA NA 34.3248430437 0.4725127672 NA Base of Markagunt landslide-Spot 20 350.1424808283 16542.0676895136 1.6157795032 20.7395915708 1.3047435497 0.0355238025 1.9244784954 0.0053457347 1.4146595876 0.735087241 34.3690377071 0.4849110884 35.4443703211 0.6703512102 108.8968054056 30.8200210616 34.3690377071 0.4849110884 NA Base of Markagunt landslide-Spot 2 44.6769624877 899.1052143677 1.1050620552 28.5365830001 24.8378904424 0.0258358793 24.8863886953 0.0053494973 1.5529136047 0.0624001185 34.3931637979 0.532673886 25.9001596645 6.3641856469 NA NA 34.3931637979 0.532673886 NA Base of Markagunt landslide-Spot 112 173.6298970514 8196.0274726728 2.3785795326 21.8890255728 2.3288122682 0.0336960993 2.5992303818 0.0053517253 1.154396811 0.4441302391 34.4074500991 0.3961403759 33.6506321368 0.8603230156 NA NA 34.4074500991 0.3961403759 NA Base of Markagunt landslide-Spot 97 162.5440768633 1822.1991383265 1.6421949347 17.7877657677 8.1918315616 0.0414816609 8.2545891438 0.0053538388 1.0159417307 0.12307599 34.4210022842 0.3487653716 41.2696077239 3.3383467708 460.0190479475 181.908525201 34.4210022842 0.3487653716 NA Base of Markagunt landslide-Spot 73 213.422880429 6747.6749966196 1.2773143408 21.7813109879 3.0034940583 0.0339207497 3.2140165763 0.0053608939 1.1440830366 0.3559667504 34.4662399151 0.3932701436 33.8712786422 1.0706718273 NA NA 34.4662399151 0.3932701436 NA Base of Markagunt landslide-Spot 90 198.1424701497 1475.4698855915 1.6925605832 25.0277547574 4.3318597058 0.0295381767 4.4706646393 0.0053640563 1.105365915 0.2472486765 34.4865173872 0.380184362 29.5581352854 1.3023972495 NA NA 34.4865173872 0.380184362 NA Base of Markagunt landslide-Spot 32 161.389970058 1285.0535504885 1.332051253 29.0766208005 2.9172985506 0.0254309381 3.1064589524 0.0053653007 1.0674532259 0.3436237988 34.4944964818 0.3672292254 25.4992655562 0.7822608239 NA NA 34.4944964818 0.3672292254 NA Base of Markagunt landslide-Spot 125 165.7873122368 3266.2019075915 1.2911785905 21.9833085038 2.4453569139 0.0336976549 2.6730924573 0.005375025 1.0796540412 0.4038970064 34.5568483236 0.3720961836 33.6521601823 0.8848102573 NA NA 34.5568483236 0.3720961836 NA Base of Markagunt landslide-Spot 78 273.3065263962 4762.1770753857 1.3533700114 22.9949329442 2.3388738381 0.0322218254 2.7764128435 0.0053761335 1.4960405901 0.5388393853 34.563955792 0.5157070319 32.2014428771 0.8800172114 NA NA 34.563955792 0.5157070319 NA Base of Markagunt landslide-Spot 72 279.1131616812 1936.5672937435 1.1856474542 24.8701758818 1.8915954131 0.0298007295 2.2617181156 0.0053776621 1.2398530669 0.5481908016 34.5737570148 0.4275163232 29.8170452437 0.6645721683 NA NA 34.5737570148 0.4275163232 NA Base of Markagunt landslide-Spot 6 204.6701190955 4634.6672057572 1.5597949032 22.2553745371 2.6012258162 0.0333095186 2.8584220584 0.0053788696 1.1849898385 0.4145608361 34.5814999348 0.4086900809 33.2708291207 0.935608836 NA NA 34.5814999348 0.4086900809 NA Base of Markagunt landslide-Spot 64 62.8085640228 751.7866504392 1.0514178228 34.2575063416 10.42477866 0.0216412177 10.5459380541 0.0053792929 1.5939884978 0.1511471516 34.58421417 0.5497922948 21.7397280402 2.2682929205 NA NA 34.58421417 0.5497922948 NA Base of Markagunt landslide-Spot 82 86.8247642591 1346.3666709223 1.7450429548 27.5144189617 7.9561546389 0.0269929414 8.022993093 0.0053888775 1.0334512718 0.128811188 34.6456693821 0.3570856894 27.0447863938 2.141162979 NA NA 34.6456693821 0.3570856894 NA Base of Markagunt landslide-Spot 118 67.3882287951 3911.5766892137 2.1257642488 23.400503575 4.6089487165 0.0317429042 4.853439955 0.0053896382 1.521009903 0.3133880128 34.6505470833 0.5256243291 31.7302250554 1.5161950057 NA NA 34.6505470833 0.5256243291 NA Base of Markagunt landslide-Spot 3 62.5757529141 2314.2622832335 0.6045607354 29.5325066041 9.6619228995 0.0251588205 9.766220303 0.0053911118 1.4234833651 0.1457558115 34.6599954712 0.4920552854 25.2297785188 2.4336402648 NA NA 34.6599954712 0.4920552854 NA Base of Markagunt landslide-Spot 11 457.5163367453 5265.2434775774 1.1647477095 22.9414321842 1.8708644873 0.0324124828 2.1050809149 0.0053953619 0.9650034862 0.458416339 34.6872461691 0.3338341723 32.3889727301 0.6710545411 NA NA 34.6872461691 0.3338341723 NA Base of Markagunt landslide-Spot 123 2702.1669638052 68044.7952184843 1.1235067988 21.6093042757 0.7707157944 0.0344278605 1.2487485566 0.0053980708 0.9825325042 0.7868137257 34.7046150046 0.340067915 34.3691750818 0.4220022442 10.9718235802 18.5394393958 34.7046150046 0.340067915 NA Base of Markagunt landslide-Spot 117 202.6253076328 4701.6620214711 1.2899748721 21.7993776587 2.9387329373 0.0341649919 3.4631183101 0.005403973 1.832221917 0.5290670872 34.7424589625 0.6348466841 34.1111133622 1.1616864368 NA NA 34.7424589625 0.6348466841 NA Base of Markagunt landslide-Spot 101 146.9828674451 2170.4395592407 1.9777571517 23.0900258017 3.3499095934 0.0322717236 3.6322141183 0.0054067257 1.4039533887 0.386528256 34.7601082896 0.486702351 32.2505259739 1.1530009636 NA NA 34.7601082896 0.486702351 NA Base of Markagunt landslide-Spot 77 157.8732241932 6796.5370799978 1.1629886486 21.7026974231 2.3635846403 0.0343964643 2.690480183 0.0054164567 1.2853603632 0.4777438508 34.8225006314 0.4463878778 34.3383564216 0.9084198156 NA NA 34.8225006314 0.4463878778 NA Base of Markagunt landslide-Spot 53 222.2744907205 2261.5449788515 1.2301494962 24.9255432599 8.5870875901 0.0299540968 8.7402096296 0.0054173715 1.6288618999 0.1863641685 34.8283660713 0.5657762367 29.9682540552 2.5810181248 NA NA 34.8283660713 0.5657762367 NA Base of Markagunt landslide-Spot 1 132.1315829432 1292.3298687695 1.990846059 31.0110264346 3.3858008732 0.0241414614 3.592111755 0.0054320962 1.1998413676 0.334021169 34.9227756911 0.417884964 24.2216205497 0.859772327 NA NA 34.9227756911 0.417884964 NA Base of Markagunt landslide-Spot 28 246.752482644 4126.0780601726 2.0258121989 22.4420997722 4.5250019922 0.0333706129 4.7594781036 0.0054339473 1.475462229 0.3100050461 34.9346444611 0.5140533385 33.3308616913 1.5606217732 NA NA 34.9346444611 0.5140533385 NA Base of Markagunt landslide-Spot 74 93.1100789729 8726.2646055321 1.4383751156 18.329656175 4.4412614721 0.0409156786 4.7003905166 0.0054416654 1.5391125836 0.3274435556 34.9841289313 0.5369867239 40.7176584954 1.8760247116 393.0903505565 99.6531044201 34.9841289313 0.5369867239 NA Base of Markagunt landslide-Spot 59 164.2002491239 3447.7862563554 1.3594436808 22.8405790532 2.2141030776 0.0328851731 2.4616966858 0.0054499811 1.0759638165 0.4370822054 35.0374452217 0.3759675813 32.8537597122 0.7958159315 NA NA 35.0374452217 0.3759675813 NA Base of Markagunt landslide-Spot 5 2702.1669638052 74795.0795846688 1.7496626443 20.9026780993 0.7462398014 0.0359365291 1.1865292532 0.0054503679 0.9224845947 0.7774646872 35.0399250356 0.3223610094 35.8489888304 0.4179375256 90.3650324051 17.6792267269 35.0399250356 0.3223610094 NA Base of Markagunt landslide-Spot 93 84.9932388417 4758.8493823196 2.1051835974 21.1783219765 3.7241808266 0.0354750058 3.9057859593 0.0054513213 1.1771325885 0.3013817451 35.0460376053 0.4114189738 35.3965215657 1.3586933972 59.2574860984 88.7750847447 35.0460376053 0.4114189738 NA Base of Markagunt landslide-Spot 60 251.5641604979 11150.3712595259 0.8372731299 20.6005941857 2.2213691977 0.036557053 2.5739153416 0.0054643522 1.3002150103 0.505150651 35.1295841722 0.455517833 36.4570191208 0.9217268865 124.734535741 52.3017284676 35.1295841722 0.455517833 NA Base of Markagunt landslide-Spot 70 83.0955968784 5320.2504867202 1.4506994861 23.5621016565 3.2411211383 0.0320054465 3.4862963278 0.0054717427 1.2842880722 0.3683817873 35.1769678236 0.4505432164 31.9885714985 1.0978329948 NA NA 35.1769678236 0.4505432164 NA Base of Markagunt landslide-Spot 30 418.9561420666 4625.5665981499 1.1050769159 19.5478668223 3.8996431595 0.0386069496 3.9737567017 0.0054758635 0.7638884424 0.1922333197 35.20338746 0.2681816817 38.4630590721 1.4998428754 246.8851252853 89.820818811 35.20338746 0.2681816817 NA Base of Markagunt landslide-Spot 22 162.5365754084 9666.9141437789 0.8464795862 23.5044455343 2.9644966537 0.0321405216 3.2457067661 0.0054813898 1.3215036896 0.4071543688 35.2388180041 0.4644117891 32.1214623305 1.0262506187 NA NA 35.2388180041 0.4644117891 NA Base of Markagunt landslide-Spot 85 544.8010781014 48229.9915258287 1.5616740292 20.6940583643 1.3262778863 0.0365433693 1.7993578912 0.0054870891 1.2160081369 0.6758011526 35.2753576407 0.4277797278 36.4436148702 0.6441227392 114.0779735679 31.3150816887 35.2753576407 0.4277797278 NA Base of Markagunt landslide-Spot 120 301.7122581513 13339.2354643494 0.901665288 22.4147910506 1.770741365 0.0337671892 2.0767058196 0.0054918335 1.0849802207 0.5224525354 35.3057750089 0.3820136135 33.7204601942 0.6887746021 NA NA 35.3057750089 0.3820136135 NA Base of Markagunt landslide-Spot 46 66.4406514057 10620.6800504383 1.5657125039 17.316526935 4.4251358635 0.0437278311 4.7160357098 0.0054942255 1.6306947616 0.3457765933 35.3211110231 0.5744044369 43.457132851 2.0062185123 519.249437759 97.1682508008 35.3211110231 0.5744044369 NA Base of Markagunt landslide-Spot 18 151.139737455 3716.7776299882 4.1210257963 22.3857516558 2.6239813262 0.0338592968 2.956938966 0.0054996794 1.3631617837 0.4610043695 35.3560764036 0.4806412526 33.810925803 0.9833064872 NA NA 35.3560764036 0.4806412526 NA Base of Markagunt landslide-Spot 98 210.0901064139 7876.3333436549 1.2260946953 17.0161241309 4.4266638335 0.0447258169 4.5514321641 0.0055221307 1.058386531 0.23253923 35.5000137166 0.3746947066 44.4275522232 1.9784928681 557.5343198757 96.5565192545 35.5000137166 0.3746947066 NA Base of Markagunt landslide-Spot 96 159.4138421284 152216.157112189 1.2378640731 20.2077554459 2.5052090185 0.0377561786 2.8944158491 0.0055359717 1.4496795787 0.5008539389 35.5887481177 0.5145013033 37.6309709473 1.0692609403 169.8803421445 58.4877793441 35.5887481177 0.5145013033 NA Base of Markagunt landslide-Spot 71 166.0167648923 13540.327048056 0.6668499145 21.1205911326 2.8197712343 0.0361372116 3.2706873995 0.0055379428 1.6571922796 0.5066801186 35.6013843033 0.5883572484 36.0456706536 1.1582611912 65.7298291456 67.1289035277 35.6013843033 0.5883572484 NA Base of Markagunt landslide-Spot 81 127.6474686167 2200.246642814 1.4867186044 25.1635639851 4.9713792553 0.0303568337 5.1395917716 0.0055426362 1.3041441173 0.2537446893 35.6314736661 0.463403895 30.3652157119 1.5375444607 NA NA 35.6314736661 0.463403895 NA Base of Markagunt landslide-Spot 12 231.5336176832 12236.1854541709 1.3943131711 21.9369558185 1.9600353421 0.0348340481 2.2702899046 0.0055445724 1.145634195 0.5046202217 35.6438864554 0.4072216978 34.7678061393 0.775969321 NA NA 35.6438864554 0.4072216978 NA Base of Markagunt landslide-Spot 17 121.6495500659 1185.8120685669 0.8615154888 20.198648834 11.6448274097 0.0378927379 11.7692670046 0.0055534908 1.7069389045 0.145033578 35.7010608141 0.6077109547 37.7645774184 4.3630030055 170.9330841569 272.6367282287 35.7010608141 0.6077109547 NA Base of Markagunt landslide-Spot 111 119.5972371483 3443.910059868 2.9646993452 16.8072548762 4.5454801302 0.045552322 4.727574607 0.0055551407 1.2994506727 0.2748662434 35.7116375847 0.4627721071 45.2305261066 2.0913834431 584.4476732915 98.7380399067 35.7116375847 0.4627721071 NA Base of Markagunt landslide-Spot 54 51.5313769339 5149.1257635553 1.2563233858 19.8378278787 5.0767778136 0.0386142799 5.2542122784 0.0055581442 1.3539105206 0.2576809708 35.7308928136 0.482426098 38.4702254247 1.9834978268 212.8548123523 117.7059695661 35.7308928136 0.482426098 NA Base of Markagunt landslide-Spot 26 59.8129298603 518.7483052731 1.6674761957 41.8128054992 24.7470962618 0.0183309706 24.7809747315 0.0055613794 1.2953514029 0.0522720118 35.7516326149 0.4618274506 18.4444166238 4.529473091 NA NA 35.7516326149 0.4618274506 NA Base of Markagunt landslide-Spot 94 69.4005339536 1010.4895026574 2.0688108592 30.0369412656 7.6444669631 0.0257694042 7.858056114 0.0056162682 1.8196622604 0.231566463 36.1035019438 0.6551255558 25.834359759 2.0044731189 NA NA 36.1035019438 0.6551255558 NA Base of Markagunt landslide-Spot 57 81.226125272 699.0025371483 2.583235296 13.3722188896 14.9998947528 0.0579156723 15.1051417924 0.0056193662 1.7800185317 0.1178418949 36.1233614151 0.6412043138 57.1667009212 8.3967199277 1061.7889582006 303.4316154892 36.1233614151 0.6412043138 NA Base of Markagunt landslide-Spot 95 397.980708005 10637.6247703346 2.3974269483 21.0338462405 2.1371496387 0.0368900128 2.4717014064 0.0056300889 1.2417323642 0.5023796001 36.1920981225 0.4481497957 36.7831250907 0.8928985996 75.5019539281 50.8000161519 36.1920981225 0.4481497957 NA Base of Markagunt landslide-Spot 113 170.2679684458 479857.775388242 2.5307054163 19.7517855233 2.3336765304 0.0393867417 2.6585180423 0.005644743 1.2734488731 0.4790070456 36.2860344416 0.4607860283 39.2251284525 1.0229220766 222.9513439958 53.9962787741 36.2860344416 0.4607860283 NA Base of Markagunt landslide-Spot 23 182.2996635655 6204.5778649427 1.7758143409 20.2348292432 2.3816943428 0.038466038 2.9065725502 0.0056476107 1.6660420305 0.5731981575 36.3044175053 0.6031468842 38.3252889857 1.0931918987 166.7537683864 55.6584324088 36.3044175053 0.6031468842 NA Base of Markagunt landslide-Spot 61 157.7126611389 3240.3732105199 1.0019951645 21.8930469734 3.0020324042 0.0356191503 3.4594866349 0.0056581899 1.7192583346 0.4969692085 36.3722317988 0.6235718027 35.5378592562 1.2081622313 NA NA 36.3722317988 0.6235718027 NA Base of Markagunt landslide-Spot 104 72.7695916014 790.8839682891 2.0458788438 10.6147535581 15.8001099123 0.0739515266 15.8901125126 0.0056956699 1.6888464767 0.106282852 36.6124798154 0.6165759948 72.4423633322 11.1105786896 1511.4599690679 300.1491877964 36.6124798154 0.6165759948 NA Base of Markagunt landslide-Spot 129 130.6946021286 4059.4057456002 1.3149134648 20.6852542636 2.1937884151 0.0381037642 2.6030535976 0.0057189526 1.4011354045 0.5382660602 36.7617180007 0.5136155675 37.9710060388 0.9701530848 115.1151573831 51.7369685829 36.7617180007 0.5136155675 NA Base of Markagunt landslide-Spot 108 73.7621777198 1092.6837006842 1.0623962433 30.2553282595 12.1612331785 0.0261538272 12.4450289346 0.0057414934 2.6425655642 0.2123390454 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281.4680983423 14679.1346794486 4.9018598002 14.2489330899 3.0750193308 0.0943112969 3.8291780645 0.0097506556 2.2818546767 0.5959123964 62.5522950334 1.4204497338 91.5116137851 3.3508877849 932.7341003541 63.1004193097 62.5522950334 1.4204497338 NA Base of Markagunt landslide-Spot 107 217.2389396615 13244.4684551251 1.4293983382 12.7015481609 7.2366725089 0.1121266794 9.2623385618 0.0103336411 5.7811319508 0.6241546789 66.2730961544 3.8117086584 107.9089299451 9.4823916428 1164.487762229 143.5817951763 66.2730961544 3.8117086584 NA Base of Markagunt landslide-Spot 31 613.9680918089 27000.7003331448 1.5326233512 20.3010802219 0.6317709134 0.1641489454 1.1442936153 0.024179371 0.9540824865 0.8337741937 154.0156535137 1.452021715 154.3283759734 1.6383146326 159.1336170253 14.7816476333 154.0156535137 1.452021715 NA Base of Markagunt landslide-Spot 21 552.6253109993 74763.5510674642 1.4680524002 20.4257732667 0.8027865645 0.1650420754 1.357971708 0.0244602526 1.0952720627 0.8065499865 155.7833428189 1.6858000015 155.107074768 1.9533237676 144.7646883268 18.8101333916 155.7833428189 1.6858000015 NA Base of Markagunt landslide-Spot 87 108.7386418791 62775.7375617826 1.7681334465 13.5014222965 0.5585032328 1.7657884194 1.3719947635 0.1729840019 1.2531734796 0.9133952351 1028.5313839141 11.9136200807 1032.9753129743 8.8943288502 1042.3754462093 11.2883849101 1042.3754462093 11.2883849101 98.6718737145 Base of Markagunt landslide-Spot 116 122.7574245007 303964.396090226 2.2655028253 13.1792574722 0.7426623879 1.9083360735 1.4813342609 0.1824876829 1.2817190683 0.865246354 1080.5506860143 12.7511263288 1084.003778836 9.8697675762 1090.9320695453 14.8772032334 1090.9320695453 14.8772032334 99.0483932207 Base of Markagunt landslide-Spot 91 189.6286913344 170504.819091906 3.0125295191 13.1245408541 0.6346604112 1.9320652958 1.2435799972 0.1839897686 1.0694378766 0.8599670942 1088.7342145793 10.7132167247 1092.2547127443 8.3207317644 1099.2980435935 12.6861243421 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29804.5885079568 3.8110722048 12.4614210012 0.8620658807 2.2718015405 1.2778431481 0.2054119535 0.9432526324 0.7381599485 1204.3279846593 10.3618386251 1203.5749231143 9.0095332776 1202.2057261708 16.971363561 1202.2057261708 16.971363561 100.1765303926 Base of Markagunt landslide-Spot 88 67.3195452619 135126.853855951 2.2324463271 12.0475424561 0.7103949492 2.4643907854 1.1208272661 0.2154248485 0.8669445061 0.7734862742 1257.6546990757 9.9055257502 1261.6508074151 8.0958136385 1268.4901917732 13.8488783853 1268.4901917732 13.8488783853 99.1457960993 Base of Markagunt landslide-Spot 130 101.7883045744 79603.1755839954 0.9562764998 11.7335083158 0.6970542068 2.6844868457 1.1725670115 0.2285477342 0.9428832533 0.804118864 1326.8832741631 11.3073662123 1324.192781693 8.6748588818 1319.8242865223 13.5090866646 1319.8242865223 13.5090866646 100.5348429873 Base of Markagunt landslide-Spot 89 104.6658839265 53787.9368168727 1.3620735184 11.224409671 0.6847099864 2.8792797455 1.2298987061 0.2344958309 1.0216765935 0.8306997873 1358.018711853 12.5105871583 1376.5035323076 9.2692390463 1405.2765030769 13.1128035518 1405.2765030769 13.1128035518 96.6371179536 Base of Markagunt landslide-Spot 49 114.5606220532 14549548.249423 2.9261277104 9.3807210663 0.571645702 4.4679520163 1.1521791984 0.3041112437 1.0003689802 0.8682407924 1711.6633001043 15.0382412539 1725.0384763797 9.5597509509 1741.2902714807 10.4753251526 1741.2902714807 10.4753251526 98.2985621719 Base of Markagunt landslide-Spot 35 61.6339213198 64998.4150515421 4.8595297398 9.2620556763 0.6213516638 4.5085976639 1.0915359426 0.3029958104 0.8974256647 0.8221677636 1706.1471894742 13.4527454753 1732.5583422059 9.0715173252 1764.5853796925 11.3551423485 1764.5853796925 11.3551423485 96.6882764138 Base of Markagunt landslide-Spot 84 74.2997819823 59662.4808356922 2.1824917552 8.8859389266 0.7006168131 5.1533444987 1.1626979021 0.3322616782 0.9279021999 0.7980595805 1849.3344586446 14.9180446804 1844.9466974012 9.8875449813 1839.9863872038 12.6857899294 1839.9863872038 12.6857899294 100.5080511196 PlotDat15 Source sheet Haycock 30 0.0000000231 32 0 30 0 Plot name ProbDens10 30.02 0.0000000279 33 0 69.98 0 Plot Type 16 30.04 0.0000000335 33 6 1st free col 9 30.06 0.0000000403 32 6 Sigma Level 1 30.08 0.0000000484 32 0 Absolute Errs TRUE 30.1 0.000000058 ErrBox ErrBox Symbol Type 1 30.12 0.0000000695 33 0 Inverse Plot FALSE 30.14 0.0000000831 34 0 Color Plot TRUE 30.16 0.0000000992 34 32 3D plot FALSE 30.18 0.0000001182 33 32 Linear FALSE 30.2 0.0000001408 33 0 Data Range R8:S113 30.22 0.0000001674 ErrBox ErrBox Filled Symbols TRUE 30.24 0.0000001987 34 0 ConcAge FALSE 30.26 0.0000002356 35 0 ConcSwap FALSE 30.28 0.0000002789 35 43 1st Symbol-row 1 30.3 0.0000003298 34 43 30.32 0.0000003893 34 0 30.34 0.000000459 ErrBox ErrBox 30.36 0.0000005404 35 0 30.38 0.0000006354 36 0 30.4 0.000000746 36 15 30.42 0.0000008747 35 15 30.44 0.0000010241 35 0 30.46 0.0000011973 ErrBox ErrBox 30.48 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66.36 0.0000001954 66.38 0.0000001724 66.4 0.000000152 66.42 0.000000134 66.44 0.0000001179 66.46 0.0000001037 66.48 0.0000000912 66.5 0.0000000801 66.52 0.0000000703 66.54 0.0000000617 66.56 0.000000054 66.58 0.0000000473 66.6 0.0000000414 66.62 0.0000000362 66.64 0.0000000316 66.66 0.0000000276 66.68 0.0000000241 66.7 0.000000021 66.72 0.0000000183 66.74 0.0000000159 66.76 0.0000000138 66.78 0.000000012 66.8 0.0000000104 66.82 0 66.84 0 66.86 0 66.88 0 66.9 0 66.92 0 66.94 0 66.96 0 66.98 0 67 0 67.02 0 67.04 0 67.06 0 67.08 0 67.1 0 67.12 0 67.14 0 67.16 0 67.18 0 67.2 0 67.22 0 67.24 0 67.26 0 67.28 0 67.3 0 67.32 0 67.34 0 67.36 0 67.38 0 67.4 0 67.42 0 67.44 0 67.46 0 67.48 0 67.5 0 67.52 0 67.54 0 67.56 0 67.58 0 67.6 0 67.62 0 67.64 0 67.66 0 67.68 0 67.7 0 67.72 0 67.74 0 67.76 0 67.78 0 67.8 0 67.82 0 67.84 0 67.86 0 67.88 0 67.9 0 67.92 0 67.94 0 67.96 0 67.98 0 68 0 68.02 0 68.04 0 68.06 0 68.08 0 68.1 0 68.12 0 68.14 0 68.16 0 68.18 0 68.2 0 68.22 0 68.24 0 68.26 0 68.28 0 68.3 0 68.32 0 68.34 0 68.36 0 68.38 0 68.4 0 68.42 0 68.44 0 68.46 0 68.48 0 68.5 0 68.52 0 68.54 0 68.56 0 68.58 0 68.6 0 68.62 0 68.64 0 68.66 0 68.68 0 68.7 0 68.72 0 68.74 0 68.76 0 68.78 0 68.8 0 68.82 0 68.84 0 68.86 0 68.88 0 68.9 0 68.92 0 68.94 0 68.96 0 68.98 0 69 0 69.02 0 69.04 0 69.06 0 69.08 0 69.1 0 69.12 0 69.14 0 69.16 0 69.18 0 69.2 0 69.22 0 69.24 0 69.26 0 69.28 0 69.3 0 69.32 0 69.34 0 69.36 0 69.38 0 69.4 0 69.42 0 69.44 0 69.46 0 69.48 0 69.5 0 69.52 0 69.54 0 69.56 0 69.58 0 69.6 0 69.62 0 69.64 0 69.66 0 69.68 0 69.7 0 69.72 0 69.74 0 69.76 0 69.78 0 69.8 0 69.82 0 69.84 0 69.86 0 69.88 0 69.9 0 69.92 0 69.94 0 69.96 0 69.98 0 IsoLine IsoLine PlotDat19 Source sheet Haycock 0.2 33.0502620997 1 32.6034162685 0.3770061812 0.85 32.2264100874 Plot name Average14 12.8 33.0502620997 2 32.6907730712 0.5354746576 1.15 32.2264100874 Plot Type 15 3 32.8341038655 0.411767643 1.15 32.9804224497 1st free col 8 4 32.8489777283 0.3256411561 0.85 32.9804224497 Sigma Level 1 5 32.9020240883 0.4166964214 0.85 32.2264100874 Absolute Errs TRUE 6 32.9989734715 0.382961434 ErrBox ErrBox Symbol Type 1 7 33.0584304133 0.3247164703 1.85 32.1552984136 Inverse Plot FALSE 8 33.1802124617 0.305920206 2.15 32.1552984136 Color Plot TRUE 9 33.2426131375 0.46354794 2.15 33.2262477288 3D plot FALSE 10 33.2614958985 0.2980553337 1.85 33.2262477288 Linear FALSE 11 33.2816199632 0.3134843775 1.85 32.1552984136 Data Range R8:S19 12 33.3576597197 0.4276475245 ErrBox ErrBox Filled Symbols TRUE IsoLine IsoLine IsoLine 2.85 32.4223362225 ConcAge FALSE 3.15 32.4223362225 ConcSwap FALSE 3.15 33.2458715085 1st Symbol-row 1 2.85 33.2458715085 2.85 32.4223362225 ErrBox ErrBox 3.85 32.5233365722 4.15 32.5233365722 4.15 33.1746188844 3.85 33.1746188844 3.85 32.5233365722 ErrBox ErrBox 4.85 32.4853276668 5.15 32.4853276668 5.15 33.3187205097 4.85 33.3187205097 4.85 32.4853276668 ErrBox ErrBox 5.85 32.6160120376 6.15 32.6160120376 6.15 33.3819349055 5.85 33.3819349055 5.85 32.6160120376 ErrBox ErrBox 6.85 32.733713943 7.15 32.733713943 7.15 33.3831468836 6.85 33.3831468836 6.85 32.733713943 ErrBox ErrBox 7.85 32.8742922557 8.15 32.8742922557 8.15 33.4861326677 7.85 33.4861326677 7.85 32.8742922557 ErrBox ErrBox 8.85 32.7790651976 9.15 32.7790651976 9.15 33.7061610775 8.85 33.7061610775 8.85 32.7790651976 ErrBox ErrBox 9.85 32.9634405648 10.15 32.9634405648 10.15 33.5595512323 9.85 33.5595512323 9.85 32.9634405648 ErrBox ErrBox 10.85 32.9681355857 11.15 32.9681355857 11.15 33.5951043408 10.85 33.5951043408 10.85 32.9681355857 ErrBox ErrBox 11.85 32.9300121952 12.15 32.9300121952 12.15 33.7853072443 11.85 33.7853072443 11.85 32.9300121952 ErrBox ErrBox Haycock Analysis U 206Pb U/Th 206Pb* ± 207Pb* ± 206Pb* ± error 206Pb* ± 207Pb* ± 206Pb* ± Best age ± Conc (ppm) 204Pb 207Pb* (%) 235U* (%) 238U (%) corr.


id: giw-157
title: A visual paleontological inventory of Utah’s National Park Service areas
date: 2025
pages: 136
extension: .pdf
mime: application/pdf
words: 61208
sentence: 2607
flesch: 59
cache: cache/giw-157.pdf
txt: txt/giw-157.txt
author:
  Tran, Tut; Milner, Andrew; Tweet, Justin; DeBlieux, Donald; Hunt-Foster, ReBecca; Shaffer, Austin; Kirkland, James; Warner-Cowgill, Ethan; Santucci, Vincent

summary:
  224 A Visual Paleontological Inventory of Utah’s National Park Service Areas Tut Tran, Andrew R.C. Milner, Justin S. Tweet, Donald D. DeBlieux, ReBecca Hunt-Foster, Austin B. Shaffer, James I. Kirkland Ethan Warner-Cowgill, and Vincent L. Santucci Geology of the Intermountain West 2025 Volume 12 paleontologists, collaboration with outside researchers, and recruitment of paleontology interns to help them protect, monitor, and study their fossils (ARCH, Swan- son et al., 2005, Madsen et al., 2012; BRCA, Tran et al., 2024; CANY, DeBlieux et al., 2021, 2023, 2024; CARE, Kirkland et al., 2014a, 2020; GLCA, Kirkland et al., 2010; METHODS This work began after the Tut Tran created a bio- stratigraphic diagram for BRCA, first for the Society of Vertebrate Paleontology 83rd Annual Meeting (Tran, 2023b), and subsequently for the full BRCA Paleonto- logical Resource Inventory (Tran et al., 2024).


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author: Kirkland, James; Hunt-Foster, ReBecca; Morgan, Kirsty; McHugh, Julia; Foster, John
date: 2025
pages: 81
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summary: Dorsal osteoderm MWC 6762 in (U) dorsal view. Dorsal osteoderm MWC 6755 in (V) dorsal view.
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title:
  Differentiating ankylosaur species in the Upper Jurassic Morrison Formation in light of newly recovered skeletal elements of Mymoorapelta maysi from its type locality


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