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

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,Sonderbauarten von K?ltemaschinen, argued to be the prime initiator of cave development. The caves that result are commonly shallow, and vulnerable to removal by the next glaciation, indicating a cyclic nature to cave development and destruction, avoided only by the larger, deeper or fortuitously placed cave systems. A general lack

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2364-4591 the evolution of karst landscapes from pre-glacial times to the present and human interaction with the caves in the region..978-3-319-36540-4978-3-319-16534-9Series ISSN 2364-4591 Series E-ISSN 2364-4605

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Introductionences 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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Pseudokarst and Non-dissolutional Cavesby 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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