Skip to Main Content
Skip Nav Destination

Upper Pliocene and Quaternary deposits were mapped in an area of 1,800 km2 in the west-central San Joaquin Valley and adjacent Diablo Range. The upper Pliocene and Pleistocene Tulare Formation, which consists of alluvial sand, gravel, silt, and clay and locally dips 20°, is overlain by a sequence of six units, each 0 to 20 m thick, each the result of an episode of deposition of alluvium from the Diablo Range. Erosional unconformities and soils between the units record the intervening periods. The units consist of unconsolidated gravel, sand, silt, and clay, with textures and sedimentary structures indicating deposition...

You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

Figures & Tables




Citing Books via

Related Book Content
Close Modal

or Create an Account

Close Modal
Close Modal