id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
amq-114	Giraudi, Carlo	The morphology of the base of the alluvial sediments of the Vercelli plain (Piedmont, NW Italy): an integration of the knowledge on the quaternary geological evolution	2017	12	.pdf	application/pdf	8130	334	58	However the lack of Middle Pleistocene river sediments and terraces in the southern part of the plain prevents any knowledge of the geological evolution for a period that lasted about 600-700 ka and limits the data useful to establish the seismo-tectonic characteris- tics of the Monferrato thrust front and to establish the seismic hazard. The data indicate that in the southern Vercelli Plain there are small valleys and ridges covered by alluvial sediments, originated by erosion connected with the Alpine rivers and local streams, that do not show any evidence.	cache/amq-114.pdf	txt/amq-114.txt