Quaternary history of the Coorong Coastal Plain, southern Australia :
[Book]
an archive of environmental and global sea-level changes /
Colin V. Murray-Wallace.
Cham, Switzerland :
Springer,
2018.
1 online resource
Includes bibliographical references and index.
Intro; Preface; References; Contents; Abbreviations; About the Author; 1 The Coorong Coastal Plain, Southern Australia-An Introduction; Abstract; 1.1 Introduction; 1.2 The Coorong Coastal Plain as a Morphotectonic Province; 1.3 Historical Background; 1.4 Geological and Geomorphological Setting of the Coorong Coastal Plain; 1.5 Pre-Quaternary Geology-An Antecedent Framework for Quaternary Coastal Landscape Evolution; 1.6 Early Notions of Aeolianite Formation and Pleistocene Sea Levels-the Relevance of the Coorong Coastal Plain; 1.7 Arrangement of This Book; References.
2 The Pleistocene Barrier Sequence of the Coorong Coastal Plain, Southern AustraliaAbstract; 2.1 Introduction; 2.2 The Pleistocene Bridgewater Formation-A Record of Successive Coastal Barrier Formation; 2.3 Facies Associations Within the Coastal Barrier Complexes of the Bridgewater Formation; 2.4 Sediment Properties of the Pleistocene Bridgewater Formation; 2.5 Other Quaternary Stratigraphical Units Relevant to the Evolution of the Coastal Plain; 2.5.1 Coomandook Formation; 2.5.2 Padthaway Formation; 2.5.3 Glanville Formation; 2.5.4 St. Kilda Formation.
2.6 Early Pleistocene Coastal Sedimentation-Robe to Naracoorte Line of Section2.6.1 Marmon Jabuk Range; 2.6.2 Cannonball Hill Range; 2.6.3 Coonalpyn Range; 2.6.4 Mount Monster Range; 2.6.5 The Black Range; 2.6.6 Hynam-Koppamurra Range; 2.6.7 East Naracoorte Range; 2.7 Middle Pleistocene Coastal Sedimentation-Robe to Naracoorte Line of Section; 2.7.1 West Naracoorte Range; 2.7.2 Harper Range; 2.7.3 Stewarts/Cave Ranges; 2.7.4 Woolumbool and Peacock Ranges; 2.7.5 Baker Range; 2.7.6 Lucindale Range; 2.7.7 Ardune; 2.7.8 East Avenue Range; 2.7.9 West Avenue Range.
2.7.10 Reedy Creek Range and East and West Dairy Ranges2.7.11 Neville Range; 2.8 Late Pleistocene Coastal Sedimentation-Robe to Naracoorte Line of Section; 2.8.1 Woakwine Range; 2.8.2 Robe Range; 2.9 Coastal Plain Sedimentation-Mount Gambier Region; 2.9.1 Dismal Range; 2.9.2 Mingbool Range; 2.9.3 Compton Range; 2.9.4 Glenburnie Range; 2.9.5 Gambier Range; 2.9.6 Caveton Range; 2.9.7 Burleigh Range; 2.9.8 MacDonnell Range; 2.9.9 Robe Range (Canunda Range); 2.10 Coastal Plain Sedimentation-River Murray Mouth Region; 2.11 Summary and Conclusions; References.
3 Holocene Coastal Sedimentary Environments of the Coorong Coastal Plain, Southern AustraliaAbstract; 3.1 Introduction; 3.2 Physical Processes in the Modern Shelf and Coastal Environments; 3.3 The Terminal Lakes to the River Murray-Lakes Alexandrina and Albert; 3.4 Younghusband Peninsula-A Holocene Analogue for the Pleistocene Barrier Successions; 3.5 The Coorong Lagoon and Associated Saline Lake Environments; 3.5.1 North Stromatolite Lake; 3.5.2 Dolomite and Pellet Lake; 3.5.3 Halite Lake; 3.5.4 Milne Lake; 3.6 Soft Sediment Deformation Structures in Lagoonal Muds.
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This book provides an up-to-date overview of the Quaternary geological and geomorphological evolution of the Coorong Coastal Plain region and its significance in a global context for understanding long-term records of Quaternary sea-level changes. The Coorong Coastal Plain in southern Australia is a natural laboratory for examining the response of coastal barrier landscapes to relative sea-level changes. The region provides direct evidence of coastal sedimentation during successive interglacials over the past 1 million years, as well as more recent volcanism. The region has received international focus and attracted scientists from around the World, with interests in long-term coastal evolution, sea-level changes, Quaternary dating methods and geochronology, soil development, temperate carbonate sedimentation, karst geomorphology and geologically recent volcanism.
Springer Nature
com.springer.onix.9783319893426
Quaternary history of the Coorong Coastal Plain, Southern Australia.