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Titlebook: Desert Aeolian Processes; Vatche P. Tchakerian Book 1995 Vatche P. Tachakerian 1995 Mineral.North America.desert.environment.geomorphology

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發(fā)表于 2025-3-21 18:56:09 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Desert Aeolian Processes
編輯Vatche P. Tchakerian
視頻videohttp://file.papertrans.cn/269/268316/268316.mp4
圖書封面Titlebook: Desert Aeolian Processes;  Vatche P. Tchakerian Book 1995 Vatche P. Tachakerian 1995 Mineral.North America.desert.environment.geomorphology
描述The idea for this volume came during the dryland sessions of the Association of American Geographers meeting in San Diego in April, 1992. The large number of papers devoted to aeolian processes and landforms indicated to me that aeolian geomorphology had come of age and the last 15 years or so had produced a plethora of papers, books, and edited volumes on all aspects of aeolian geomorphology. Chapter one is my tentative attempt to place develop- ments in aeolian geomorphology in a historical perspective and to contemplate some thoughts about the future. The fourteen papers selected address a wide range of issues ranging from micro-scale studies devoted to aeolian dust, sediment transport, and rock varnish in ventifacts to medium-scale studies of dunes and dune forms, reverse desertification, and macro-scale studies of ergs and sand transport pathways. The American Southwest, particularly the spectacular and unique Mojave Desert of California, is featured prominently in seven chapters. I hope this volume provides students and colleagues some new perspectives in aeolian geomorphology as well as pathways for future work.
出版日期Book 1995
關(guān)鍵詞Mineral; North America; desert; environment; geomorphology; global warming; land degradation; moisture; morp
版次1
doihttps://doi.org/10.1007/978-94-009-0067-7
isbn_softcover978-94-010-6519-1
isbn_ebook978-94-009-0067-7
copyrightVatche P. Tachakerian 1995
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978-94-010-6519-1Vatche P. Tachakerian 1995
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Johan F. M. Swinnen,Miet Maertensold in 1941 produced few significant works in aeolian geomorphology. More recently, however, the number of papers, edited volumes and conference proceedings has been phenomenal. This ‘renaissance’ in aeolian geomorphology is attributed to a number of interrelated factors including the increased desi
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Manuel A. Hernandez,Máximo Toreros to have formed as a result of a genetically distinct episode of sediment input and/or reworking of preexisting dunes. Formation of different dune generations was probably the result of fluctuations in sediment supply from source zones which were controlled by tectonic reorganizations of the Colora
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https://doi.org/10.1007/978-1-4471-0609-8arate 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. T
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Financialization: Limits and Ways Outnd dune morphology. The study focused on a barchan located west of the Salton Sea in southern California. This paper describes the research design, study area, field methods, and instrumentation used in the study. To describe and analyze the wind events that occurred during the course of the field s
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