Sand Transport Paths in the Mojave Desert, Southwestern United States

@inproceedings{Zimbelman1995SandTP,
  title={Sand Transport Paths in the Mojave Desert, Southwestern United States},
  author={J. Zimbelman and S. H. Williams and V. P. Tchakerian},
  year={1995}
}
Remote sensing and field evidence are used to describe sand deposits found in associated pathways of emplacement in the eastern Mojave Desert. Two separate pathways are identified here: one extending eastward from the Bristol Playa through the Cadiz and Danby Playas and Rice Valley to the Colorado River, and a second parallel path extending eastward from Dale Playa through the Palen and Ford Playas to the Mule Mountains near the Colorado River. The preferential location of sand ramps on the… Expand
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References

SHOWING 1-10 OF 47 REFERENCES
Development of the Gran Desierto sand sea, northwestern Mexico
Three major eolian sand populations can be recognized in the Gran Desierto sand sea of northwestern Mexico by using spectral data from the Landsat thematic mapper in conjunction with textural andExpand
Kelso Dunes, Mojave Desert, California
Kelso Dunes lie in a mountain-rimmed basin, 35 miles east of their principal sand source, where the predominant, sand transporting, westerly wind is locally counterbalanced by strong, orographicallyExpand
Eolian features in the western desert of Egypt and some applications to Mars
Relations of landform types to wind regimes, bedrock composition, sediment supply, and topography are shown by field studies and satellite photographs of the Western Desert of Egypt. This desert,Expand
PAST VERSUS PRESENT WIND ACTION IN THE MOJAVE DESERT REGION, CALIFORNIA
Abstract : The major products of wind action in the Mojave - dunes, sand sheets, deflation basins, and deeply abraded rock surfaces - are interpreted to have been formed during a past arid intervalExpand
Regional aeolian dynamics and sand mixing in the Gran Desierto: Evidence from Landsat thematic mapper images
Spatial variations in sand composition were mapped on a regional scale in a terrestrial sand sea, the Gran Desierto of Sonora, Mexico. Mesoscale mapping on a satellite image base allowed quantitativeExpand
DESERT SANDFLOW BASINS AND A MODEL FOR THE DEVELOPMENT OF ERGS
The movement and deposition of sand in deserts is not a random phenomenon. Sand flows in patterns analagous to drainage sysems that are closely related to the wind systems though not to topography.Expand
LATE QUATERNARY AEOLIAN GEOMORPHOLOGY OF THE DALE LAKE SAND SHEET, SOUTHERN MOJAVE DESERT, CALIFORNIA
Geomorphological and sedimentological analysis of aeolian deposits, combined with scanning electron microscopy (SEM) of quartz-grain surface characteristics, suggest six dune-building episodes duringExpand
Influences of eolian and pedogenic processes on the origin and evolution of desert pavements
Well-developed desert pavements are present above eolian deposits that mantle flows of the Cima volcanic field, located in the Mojave Desert, California. Soil-stratigraphic data and geochemical dataExpand
Soil-forming intervals caused by eolian sediment pulses in the Lahontan basin, northwestern Nevada
We have studied a series of Toyeh (post-Isotope Stage 2: Eolian dust fall was the source of fines and salts in these soils. Apparently, this influx was concentrated during two brief intervals, orExpand
Correlation between Fish Distribution and Pleistocene Hydrography in Eastern California and Southwestern Nevada, with a Map of the Pleistocene Waters
During late Pleistocene time an integrated river system occupied several of the desert basins in eastern California and southwestern Nevada, with Death Valley as the sump. A study of the Recent andExpand
...
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3
4
5
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