Response of alluvial fan systems to the late Pleistocene to Holocene climatic transition: contrasts between the margins of pluvial Lakes Lahontan and Mojave, Nevada and California, USA

Author:

Harvey Adrian M,Wigand Peter E,Wells Stephen G

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference67 articles.

1. Adams, K.D., Fontaine, S.A. (Eds.), 1996, Quaternary History, Isostatic Rebound and Active Faulting in the Lake Lahontan Basin, Nevada and California, Friends of the Pleistocene Pacific Cell, Field Trip Guidebook, University of Nevada, Reno, pp. 1–56.

2. Shoreline processes and the age of the Lake Lahontan highstand in the Jessup embayment, Nevada;Adams;Geological Society of America, Bulletin,1998

3. Adams, K.D., Wesnousky, S.G., in press. The Lake Lahontan highstand: age, surficial characteristics, soil development, and regional correlation. Geomorphology.

4. Stages and rate of gravel shattering processes by salts in desert Reg soil;Amit;Geoderma,1993

5. Chronology of expansion and contraction of four Great Basin lake systems during the past 35,000 years;Benson;Palaeogeography, Palaeoclimatology, Palaeoecology,1990

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