Glacigenic sediments /
This book aims primarily at providing those involved in fundamental or applied research in the fields of geology, geomorphology and hydrology with a systematic overview of glacigenic sediments. A generally applicable terminology is proposed which should facilitate communication between scientists fr...
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Main Authors: | |
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Published: |
Elsevier,
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Publisher Address: | Amsterdam ; New York : |
Publication Dates: | 1991. |
Literature type: | eBook |
Language: | English |
Series: |
Developments in sedimentology ;
49 |
Subjects: | |
Online Access: |
http://www.sciencedirect.com/science/bookseries/00704571/49 |
Summary: |
This book aims primarily at providing those involved in fundamental or applied research in the fields of geology, geomorphology and hydrology with a systematic overview of glacigenic sediments. A generally applicable terminology is proposed which should facilitate communication between scientists from several fields. Also it should form a bridge between western and eastern "schools" dealing with Quaternary geology. Because the book is mainly devoted to depositional processes and the resulting deposits, the approach and the terminology followed in this book are obviously founded strongly on s |
Carrier Form: | 1 online resource (xiv, 674 pages) : illustrations. |
Bibliography: | Includes bibliographical references and indexes. |
ISBN: |
9780444883070 044488307X 9780080869636 0080869637 |
Index Number: | QE471 |
CLC: | P512.4 |
Contents: | Preface. Introduction. General Characteristics of Glacigenic Sedimentation. The System of Glacigenic Depositional Environments. Glacigenic Facies and Their Characteristics. Tables of the Continental and Marine Glacigenic Environments, Subenvironments, Facies and Deposits. The Continental Supraglacial Subenvironment and its Deposits. The Continental Englacial Subenvironment and its Deposits. The Continental Subglacial Subenvironment and its Deposits. The Marine Glacial Environment and its Deposits. The Continental Terminoglacial Subenvironment and its Deposits. The Continental Proglacial Sube |