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ePub Study of Global Sand Seas, A download

by Edwin D. McKee

ePub Study of Global Sand Seas, A download
Author:
Edwin D. McKee
ISBN13:
978-1410214577
ISBN:
1410214575
Language:
Publisher:
University Press of the Pacific (June 19, 2004)
Category:
Subcategory:
Earth Sciences
ePub file:
1139 kb
Fb2 file:
1330 kb
Other formats:
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Rating:
4.9
Votes:
677

Digitized by. Google. Although the book is concerned primarily with desert sand seas

Digitized by. Prepared in cooperation with the National Aeronautics and Space Administration. United states government printing office, washington : 1979. Although the book is concerned primarily with desert sand seas. the subject matter is not restricted to deserts; it includes many references to deposits of coastal sand and to sand bodies in humid climates. Nor does the book deal exclusively with dunes. according to most definitions. involve mounds or hills.

Early descriptions and considerations of the characteristics of modern eolian sand deposits, mostly in the great sand seas of the world, date back to the 1880's and 1890's, when pioneer geologists and explorers wrote their classic papers on desert dunes.

Results from Google Books. No current Talk conversations about this book.

Although the book is concerned primarily with desert sand seas, the subject matter is not restricted to deserts; it includes many references to deposits of coastal. Professional Paper 1052. Document: Document (pdf). Preceding Publications: Techniques for the evaluation of surface wind data in terms of eolian sand drift (1978).

Published by U. S. Geological Survey, Washington . This book has 429 pages with no tears or markings and previous owners name stamp on front inside cover board. Coverboards show minimal shelf wear and glue binding is tight and intact. 4to - over 9¾" - 12" tall.

Introduction to a study of global sand seas A Study of Global Sand Seas. E., A Study of Global Sand Seas. United States Geological Survey, Washington, DC, pp. 1–19. Introduction to a study of global sand seas.

Book Publishing WeChat. ABSTRACT: A sedimentological, petrographic, and geochemical study of beach, dune, and river sands was carried out along the northwestern Gulf of Mexico

Book Publishing WeChat. ABSTRACT: A sedimentological, petrographic, and geochemical study of beach, dune, and river sands was carried out along the northwestern Gulf of Mexico.

US Geological Survey Professional Paper 1952:305–397Google Scholar. Walker T (1979) Red colour in dune sands. In McKee E (ed) A Study of Global Sand Seas. Bubenzer O, Besler H, Hilgers A (2007) Filling the gap: OSL data expanding 14C chronology of Late Quaternary Environmental change in the Libyan Desert. US Geological Survey Professional Paper 1052:61–82Google Scholar.

An erg (also sand sea or dune sea, or sand sheet if it lacks dunes) is a broad, flat area of desert covered with . Geological Survey Professional Paper 1052, pp. 305–397. Pye, Kenneth; Tsoar, Haim (2009).

An erg (also sand sea or dune sea, or sand sheet if it lacks dunes) is a broad, flat area of desert covered with wind-swept sand with little or no vegetative cover. The term takes its name from the Arabic word ʿarq (عرق), meaning "dune field". Strictly speaking, an erg is defined as a desert area that contains more than.

Early descriptions and considerations of the characteristics of modern eolian sand deposits, mostly in the great sand seas of the world, date back to the 1880's and 1890's, when pioneer geologists and explorers wrote their classic papers on desert dunes. One or two decades later, interest in eolian processes greatly increased when wind-formed deposits were recognized in ancient sandstones in many parts of the world and in rocks of many ages. Throughout the 20th century, as the science of geology has expanded and the programs of the U.S. Geological Survey have proliferated to keep pace, dune studies have had a similar growth. Work was initially concentrated mostly on the description of dune forms or morphology and on analysis of textural features; by midcentury, however, major contributions had been made to the physics of eolian sand by detailed studies and interpretations of minor eolian structures, by statistical analyses of cross-strata dip directions, and by the development of systems for dune classification. Most recently, interest has been renewed in detailed grain studies, in the study of cross-strata, and in interpretation of dune patterns by means of aerial photographs and Landsat imagery. A major feature of this report on global sand seas is the compilation and comparison of available data based on many different methods of investigation. The application of these studies to economic problems, which is described in one chapter, clearly illustrates the importance of eolian deposits to our present culture and to human welfare. H. William Menard Director, U.S. Geological Survey