Characteristics of fluvial systems in the plains and deserts of Wyoming
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Characteristics of fluvial systems in the plains and deserts of Wyoming

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Published by U.S. Dept. of the Interior, U.S. Geological Survey, Books and Open-File Reports [distributor] in Cheyenne, Wyo, Denver, Colo .
Written in English

Subjects:

  • Ephemeral streams -- Physiological effect -- Wyoming,
  • Streamflow -- Physiological effect -- Wyoming,
  • Landscape changes -- Wyoming

Book details:

Edition Notes

Statementby H.W. Lowham and Mark E. Smith ; prepared in cooperation with the U.S. Bureau of Land Management
SeriesWater-resources investigations report -- 91-4153
ContributionsSmith, Mark E, United States. Bureau of Land Management, Geological Survey (U.S.)
The Physical Object
Paginationv, 57 p. :
Number of Pages57
ID Numbers
Open LibraryOL13615883M
OCLC/WorldCa28760811

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2 days ago  Fluvial process, the physical interaction of flowing water and the natural channels of rivers and streams. Such processes play an essential and conspicuous role in the denudation of land surfaces and the transport of rock detritus from higher to lower levels. Over much of the world the erosion of   1. Introduction. Fluvial sandstone reservoirs are one of the most important hydrocarbon exploration targets in continental basins (e.g., Bohacs, ).However, the prediction of high-quality and large-volume reservoir facies distribution can be problematic as fluvial deposits are generally influenced by many complex allogenic controls, such as accommodation, topography, and climate (Shanley The book summarizes methods of mapping and interpretation of fluvial depositional systems, with a detailed treatment of the tectonic, climatic and eustatic controls on fluvial depositional :// Recent work suggests that soils developed on much of the modern landscape have limited preservation potential, as a significant part of the terrestrial environment is undergoing long-term degradation (Hartley et al. ; Weissmann et al. , ).Only in areas of active sediment accumulation, commonly restricted to subsiding sedimentary basins, will soils and their associated sediments

The notion that the desert areas of the world possess a distinct geomorphology has a long history and, in many ways, is informed by the popular concept of deserts as places that are ://   Fluvial. Fluvial geomorphological processes are related to rivers and streams. The flowing water found here is important in shaping the landscape in two ways. First, the power of the water moving across a landscape cuts and erodes its ://   Great Plains, vast high plateau of semiarid grassland that is a major region of North America. It lies between the Rio Grande in the south and the delta of the Mackenzie River at the Arctic Ocean in the north and between the Interior Lowland and the Canadian Shield on the east and the Rocky Mountains on the :// Billy G. Adhiperdana, Hendarmawan, Kenichiro Shibata and Makoto Ito, Relationships between discharge parameters and cross-sectional channel dimensions of rivers in an active margin influenced by tropical climate: The case of modern fluvial systems in the Indonesian islands, CATENA, /, , (), ().

  Rivers Physical, Fluvial and Environmental Processes nyxup No Comments. Rivers – Physical, Fluvial and Environmental Processes They showed that distributive fluvial systems (DFSs), commonly called megafans, fluvial fans, and alluvial fans in the literature, dominate the fluvial depositional patterns in active continental sedimentary basins, with a much smaller proportion of the fluvial area in these basins covered by rivers that are generally confined, for example: (1   Plains Indian, member of any of the Native American peoples inhabiting the Great Plains of the United States and Canada. This culture area comprises a vast grassland between the Mississippi River and the Rocky Mountains and from present-day provinces of Alberta and Saskatchewan in Canada through the present-day state of Texas in the United States. The area is drained principally by the Ephemeral fluvial systems drained off the London-Brabant and Rhenish Massifs and flowed northwards towards the Silverpit Formation desert lake, whilst marginal dune fields expanded and contracted