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all geography including DSDP/ODP Sites and Legs
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San Joaquin River
Disequilibrium river networks dissecting the western slope of the Sierra Nevada, California, USA, record significant late Cenozoic tilting and associated surface uplift
Arsenic and mercury contamination related to historical gold mining in the Sierra Nevada, California
Imaging P and S Attenuation in the Sacramento–San Joaquin Delta Region, Northern California
Dynamic Response of a Model Levee on Sherman Island Peat: A Curated Data Set
Paleochannels, stream incision, erosion, topographic evolution, and alternative explanations of paleoaltimetry, Sierra Nevada, California
Seismic Response of Levees in the Sacramento-San Joaquin Delta
Site Effects for the Sacramento-San Joaquin Delta
Pace of landscape evolution in the Sierra Nevada, California, revealed by cosmogenic dating of cave sediments
Geochemical tracers of sediment sources to San Francisco Bay
Salmon origin in California's Sacramento–San Joaquin river system as determined by otolith strontium isotopic composition
A 2000 yr record of Sacramento–San Joaquin river inflow to San Francisco Bay estuary, California
Subsidence of Peat in California and Florida
Late Cenozoic stratigraphy and structure of the west margin of the central San Joaquin Valley, California
Upper Pliocene and Quaternary deposits were mapped in an area of 1,800 km 2 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 primarily by flowing water and secondardily by mudflows. The lower three units are grouped into the informally designated alluvium of Los Banos, of middle and late Pleistocene age, the two middle units are grouped into the upper Pleistocene alluvium of San Luis Ranch, and the uppermost unit is the Holocene alluvium of Patterson. Holocene arkosic alluvium, derived from the Sierra Nevada and deposited in flood basins along the San Joaquin River, is informally named the alluvium of Dos Palos. The two older units of the alluvium of Los Banos are coeval with broad pediment remnants preserved across the foothills, which indicates that the present elevation of the foothills is due to late Quaternary deformation. These surfaces are deformed into a series of broad, gentle northeast-trending folds that have been displaced more than 100 m along three northwest-trending fault systems. The Ortigalita fault displaces Holocene alluvium and has predominantly strike-slip displacement. The O’Neill fault system is a group of small reverse faults whose fault planes coincide with bedding in the northeast-dipping Great Valley sequence; these faults are interpreted to be sympathetic displacements associated with continued uplift and northeastward tilting of the foothills. The San Joaquin fault, at the foothill-valley margin, vertically displaces the pediments as much as 140 m. The orientation of the fault plane and the magnitude of lateral displacement, however, are not known. Neither the San Joaquin fault nor the O’Neill fault appears to displace the alluvium of San Luis Ranch or younger alluvium.