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Tuesday, July 28, 2020 | History

3 edition of Water-table decline in the south-central Great Basin during the Quaternary period found in the catalog.

Water-table decline in the south-central Great Basin during the Quaternary period

Water-table decline in the south-central Great Basin during the Quaternary period

implications for toxic-waste disposal

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  • 16 Currently reading

Published by U.S. Dept. of the Interior, Geological Survey, Open-file Services Section, Western Distribution Branch in Reston, Va, Denver, Colo .
Written in English

    Subjects:
  • Water table -- Great Basin.,
  • Water table -- Death Valley (Calif. and Nev.)

  • Edition Notes

    Statementby Isaac J. Winograd and Barney J. Szabo.
    SeriesOpen-file report -- 85-697., Open-file report (Geological Survey (U.S.)) -- 85-697.
    ContributionsSzabo, B. J., Geological Survey (U.S.)
    The Physical Object
    FormatMicroform
    Pagination1 v.
    ID Numbers
    Open LibraryOL18044839M

    Babylonia and Assyria according to Compton's Encyclopedia BC: Oregon; Diamond Pond, climate of the great basin, eastern Oregon. "By BP the water table was within 10 m of its present level. Rising water table at Diamond Pond suggests that midHolocene drought had given way to effectively moister conditions. Historical Climate Change in the Santa Cruz River Basin During the past two decades, more and greater flood flows have occurred in the fall the water table in the inner valley has been lowered created for the Santa Cruz River at Tucson from data gathered during the period There is a great amount of scatter in the data points.

    INTRODUCTION TO GROUNDWATER INVESTIGATIONS () 3 Days This introductory course is designed to provide participants with information concerning hydrogeological processes and the necessary elements of a sound groundwater site investigation. The Powder River Basin is a geologic structural basin in southeast Montana and northeast Wyoming, about miles east to west and miles north to south, known for its coal deposits. The region supplies about 40 percent of coal in the United States. It is both a topographic.

    The direction of movement is inferred from the water-table-contour map (fig., 5). Water moves downgradient at approximately right angles to the contours, Well data are insufficient to define accurately water-table contours in much of the study area, so topography, springs, and other hydrographic features were used to aid construction of the map. Professor Baker has been President of the Geological Society of America (), Chair of the American Association for the Advancement of Science Section on Geology and Geography ( and ), and President of the International Union for Quaternary Research Commission on Global Continental Paleohydrology ().


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Water-table decline in the south-central Great Basin during the Quaternary period Download PDF EPUB FB2

WATER-TABLE DECLINE IN THE SOUTH-CENTRAL GREAT BASIN DURING THE QUATERNARY PERIOD: IMPLICATIONS FOR TOXIC WASTE DISPOSAL by Isaac J. Winograd and Barney J. Szabo ABSTRACT The distribution of vein calcite, tufa, and other features in­ dicative of paleo-ground water discharge, indicates that during theCited by: 5.

Get this from a library. Water-table decline in the south-central Great Basin during the Quaternary period: implications for toxic-waste disposal.

[Isaac J Winograd; B J Szabo; Geological Survey (U.S.)]. Devils Hole, Nevada - A Primer. south-central Great Basin during the Nevada and Transverse Ranges during the Quaternary, and 4) decline in water-table altitude in response to erosion.

The Climatic and Hydrologic History of Southern Nevada during the Late Quaternary Water-table decline in the south-central Great Basin during the Quaternary: implications for toxic waste.

Winograd, I. J., and Szabo, B. J.,Water-table decline in the south-central Great Basin during the Quaternary period--implications for toxic waste disposal, in: Geologic and Hydro-logic Investigations of a Potential Nuclear Waste Disposal Site at Yucca Mountain, U.S. Cited by: Winograd, I.

J., and Szabo, B. J.,Water-table decline in the south-central Great Basin during the Quaternary period-implications for toxic waste disposal, in: Geologic and Hydro-logic Investigations of a Potential Nuclear Waste Disposal Site at Yucca Mountain, U.S.

Cited by: Yucca Mountain is situated in the southwestern part of the Great Basin physiographic province. The Great Basin is coincident with the northern part of the Basin and Range physiographic province (Figure ), which is characterized by numerous north-trending mountain ranges and intervening broad, flat valleys, or basins, spaced about km apart.

The Chad Basin is the largest endorheic basin in Africa, centered on Lake rafaelrvalcarcel.com has no outlet to the sea and contains large areas of desert or semi-arid savanna. The drainage basin is roughly coterminous with the sedimentary basin of the same name, but extends further to the northeast and east.

Read chapter Might Increased Rainfall Cause Flooding of the Proposed Repository?: Figure Regional ground-water systems and heat flow in the south-central Great Basin. (From Dudley, a.) it is the rapid decline of the water table level north of Yucca Mountain that allows for the “unsaturated” condition m below the surface.

climate of the great basin, eastern Oregon. "By BP the water table was within 10 m of its present level. Rising water table at Diamond Pond suggests that midHolocene drought had given way to effectively moister conditions. Geohydrology of the Great Bend Prairie, South-Central Kansas The six observation wells in the Great Bend Prairie that have recorded water levels from this period show an average decline of feet.

However, the hydrographs in figure 2 show that much of this decline in stored water was recovered by Water table--That surface in an.

The estimation of recharge is important for proper management of the water resources of the Great Lakes Basin. Previous estimates of shallow ground-water recharge in parts of the Great Lakes Basin are useful, but usually do not extend basinwide and may be inaccurate for some areas.

To be of major concern, groundwater withdrawal must occur in densely populated and highly developed areas, possibly located close to the sea or a lagoon or a delta, and take place from unconsolidated geological basins of alluvial, lacustrine, or shallow marine origin, formed typically, although not exclusively, in the Quaternary rafaelrvalcarcel.com by: The Cenozoic fill of the Gulf of Mexico basin contains a continuous record of sediment supply from the North American continental interior for the past 65 million years.

This value estimates the average rate that solid mineral matter was deposited in the basin during each of 14 This great period of GOM depositional quiescence ended Cited by: High-water-table farming adjacent to playas was probably an important factor in the initial process of maize cultivation in the Chuska Valley.

Certainly, these eastern slopes would have provided excellent opportunities for a variety of cultivation tech - niques, including runoff and high-water-table farming.

The Snake River Aquifer is a large reservoir of groundwater underlying the Snake River Plain in the southern part of the U.S.

state of Idaho. Most of the water in the aquifer comes from rain and melting snow that flows onto the plain from the Snake River, Big Lost River, Bruneau River, and other watercourses of southern Idaho. The Rio Grande alluvial floodplain in the El Paso/Juárez Valley is underlain by a complex mosaic of braided and meandering river deposits.

Formed during alternating periods of scour and fill in the late Quaternary Period, the river deposits consist of irregularly.

The River Thames (/ ˈ t ɛ m z / TEMZ), known alternatively in parts as the Isis, is a river that flows through southern England including London.

At miles ( km), it is the longest river entirely in England and the second-longest in the United Kingdom, after the River Severn.⁃ coordinates: 51°41′39″N 2°01′47″W /.

While shallow flow systems are undoubtedly controlled by water-table topography, the driving forces on these deeper fault-hosted flow systems have not received much attention apart from the study of López and Smith (). In the Great Basin, density changes with depth are due primarily to Cited by: This banner text can have markup.

web; books; video; audio; software; images; Toggle navigation. Sea-surface singularities (e.g., vortexes, whirlpools, strong currents and water-table roughness) are observable today during the transit of the strait between Messina and Villa S.

Giovanni (Fig. 2A), and inspired the Greek mythology of Scylla and Charybdis described by Homer in his ‘Odyssey’.

Sited on the Calabrian side of the strait Cited by: 1.Following the main Lake Algonquin phase at about 10, B.P., water level in the Lake Michigan basin dropped intermittently as lower eastern outlets were successively deglaciated. The lowest lake phase, known as the Chippewa phase, occurred around 9, B.P.

in response to opening of the outlet at.Martin Grosjean, Vivien G. Standen, in Climate Change and Cultural Dynamics, Vegetation records.

The vegetation history as recorded in pollen profiles shows a picture of mid-Holocene aridity in the western South Central Andes and the Chilean coast between 18°S and 35°S. The database has substantially increased in recent years.