TAILIEUCHUNG - Ice-Marginal and Periglacial Processes and Sediments

The Society makes every effort to ensure that the scientific and production quality of its books matches that of its journals. Since 1997, all book proposals have been refereed by specialist reviewers as well as by the Society’s Books Editorial Committee. If the referees identify weaknesses in the proposal, these must be addressed before the proposal is accepted. Once the book is accepted, the Society Book Editors ensure that the volume editors follow strict guidelines on refereeing and quality control. We insist that individual papers can only be accepted after satisfactory review by two independent referees. The questions on the review forms are similar to those. | Ice-Marginal and Periglacial Processes and Sediments Edited by I. p. Martini H. M. French and A. Pérez Alberti Geological Society Special Publication 3S4 Understanding the sediments deposited by glaciers or other cold-climate processes assumes enhanced significance in the context of current global warming and the predicted melt and retreat of glaciers and ice sheets. This volume analyses glacial proglacial and periglacial settings focusing among others on sedimentation at termini of tidewater glaciers on hitherto not-well-understood high-mountain features and on sediments such as slope and aeolian deposits whose clasts were sourced in glacial and periglacial regions but have been transported and deposited by azonal processes. Difficulties are thus often encountered in inferring Pleistocene and pre-Pleistocene cold-climate conditions when the sedimentary record lacks many of the specific diagnostic indicators. The main objective of this volume is to establish the validity and limitations of the evidence that can be obtained from widely distributed clastic deposits in order to achieve reliable palaeogeographic and palaeoclimatic reconstructions. At a more general level and on the much longer geological timescale an understanding of ice-marginal and periglacial environments may better prepare us for the unavoidable reversal towards cooler and perhaps even glacial times in the future. Ice-Marginal and Periglacial Processes and .

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