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Titlebook: Glaciation and Speleogenesis; Interpretations from Max P. Cooper,John E. Mylroie Book 2015 Springer International Publishing Switzerland 20

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發(fā)表于 2025-3-21 19:38:47 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書(shū)目名稱(chēng)Glaciation and Speleogenesis
副標(biāo)題Interpretations from
編輯Max P. Cooper,John E. Mylroie
視頻videohttp://file.papertrans.cn/386/385813/385813.mp4
概述Contributes to the understanding of cave and karst systems of the world.Provides a thorough review and synthesis of literature on continentally glaciated karst.Presents the evolution of thought on gla
叢書(shū)名稱(chēng)Cave and Karst Systems of the World
圖書(shū)封面Titlebook: Glaciation and Speleogenesis; Interpretations from Max P. Cooper,John E. Mylroie Book 2015 Springer International Publishing Switzerland 20
描述.Focusing on glaciation and speleogenesis in the region of New York and New England, this book serves as an example of a karst region that has experienced large-scale continental glaciation. It reviews the literature on the controls of glaciation on karst development, exploring examples from the marbles of the Adirondacks, New England and eastern New York, the Ordovician strata of northern New York and the Siluro-Devonian strata of central New York. Each of these areas is examined in detail, demonstrating the evolution of thought on glaciated karst through case studies of individual caves as well as larger cave systems. Additionally, this book describes the geology and glaciation, the evolution of karst landscapes from pre-glacial times to the present and human interaction with the caves in the region..
出版日期Book 2015
關(guān)鍵詞Cambro-Ordovician Strata of Northern New York; Caves and Karst of the Adirondacks; Devonian Strata of
版次1
doihttps://doi.org/10.1007/978-3-319-16534-9
isbn_softcover978-3-319-36540-4
isbn_ebook978-3-319-16534-9Series ISSN 2364-4591 Series E-ISSN 2364-4605
issn_series 2364-4591
copyrightSpringer International Publishing Switzerland 2015
The information of publication is updating

書(shū)目名稱(chēng)Glaciation and Speleogenesis影響因子(影響力)




書(shū)目名稱(chēng)Glaciation and Speleogenesis影響因子(影響力)學(xué)科排名




書(shū)目名稱(chēng)Glaciation and Speleogenesis網(wǎng)絡(luò)公開(kāi)度




書(shū)目名稱(chēng)Glaciation and Speleogenesis網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




書(shū)目名稱(chēng)Glaciation and Speleogenesis被引頻次




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書(shū)目名稱(chēng)Glaciation and Speleogenesis讀者反饋




書(shū)目名稱(chēng)Glaciation and Speleogenesis讀者反饋學(xué)科排名




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Hauptwerke der Organisationstheorie,ences of caves, creating sediment occlusion and backflooding conditions within caves, and opening joints via isostatic rebound to influence ground water flow. The influence of proximal or overlying glacial lakes affects speleogenesis, water budgets, and cave sediment deposition. Glaciation acts duri
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Hauptwerke der Ungleichheitsforschungng clastics and eventually greatly deforming the Devonian carbonates along the Hudson River Valley. Other than Holocene calcareous tufa, no further carbonates were deposited on the region; clastic units of the Catskills migrated westward as the Alleghenian Orogeny ended the Paleozoic with the comple
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Die Aufbewahrung der Arzneimittel,by each ice advance, to be formed again upon ice retreat. Only the lava tube of King Phillips Cave in Connecticut is a definite pre-glacial pseudokarst cave. Crevice caves of over 300?m (1000?ft) in length, e.g. Eagle Cave, Adirondack Mountains, NY or Xanadu Cave, Shawangunks, NY, and talus caves of
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