Australian Landforms: Understanding a Low, Flat, Arid and Old LandscapeAustralian Landforms is concerned with general theories as applied to the problems posed by the Australian landscape. The book is devoted to the major factors of structure, process, and time, as well as the most recent geological period, called the Quaternary. Chapters deal with structural impacts on landform development, the work of water and rivers, of wind, ice and waves, the time factor, and the events and resultant forms associated with the climatic aberrations of the last two million years. Australian Landforms will interest those concerned with the physical landscape in the context of geology, geography, botany, zoology, ecology, environmental studies, and agricultural science, as well as travelers and others curious about the origins of the Australian landscape. |
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Results 1-3 of 55
Page 141
... bedrock walls give way to rock platforms and even , in Little Uluru , blocks and boulders resting on a small bedrock dome . Four kilometres northwest of the base of the inselberg , the sand cover over Cambrian bedrock is only 4 m thick ...
... bedrock walls give way to rock platforms and even , in Little Uluru , blocks and boulders resting on a small bedrock dome . Four kilometres northwest of the base of the inselberg , the sand cover over Cambrian bedrock is only 4 m thick ...
Page 156
... bedrock , and wind - driven waves are limited in the extent of planation they can achieve . The answer to the puzzle may be found in the character of the bedrock and in its weathering . Limestone swallows water , but is susceptible to ...
... bedrock , and wind - driven waves are limited in the extent of planation they can achieve . The answer to the puzzle may be found in the character of the bedrock and in its weathering . Limestone swallows water , but is susceptible to ...
Page 212
... bedrock Fig . 18.4 b : Section of the Greenland ice cap . ( After Hamblin et al . 1956 ) reason , it can be argued that sea - level. 3000 000 € 2000 2500 2000 exposed land contours in metres O miles T 0 km Fig . 18.4a : Plan of the ...
... bedrock Fig . 18.4 b : Section of the Greenland ice cap . ( After Hamblin et al . 1956 ) reason , it can be argued that sea - level. 3000 000 € 2000 2500 2000 exposed land contours in metres O miles T 0 km Fig . 18.4a : Plan of the ...
Contents
68 | 8 |
Plate tectonics | 29 |
Folded and faulted surfaces | 53 |
Copyright | |
15 other sections not shown
Common terms and phrases
adjacent areas arid basaltic base-level basins beach bedrock beneath blocks bornhardts boulders calcrete caused channel Chapter clay cliff climatic coast coastal continents Cretaceous crust debris deposited depressions desert developed dissected dome drainage dunes duricrust Earth earthquake eastern Eocene eroded erosional example exposed Eyre Peninsula fault flared slopes Flinders Ranges flood flow fold Gawler Ranges geological glacial glaciers granite hill incised inselbergs Island karst Lake Eyre land surface landforms landscape laterite lava layers limestone lunettes margins meanders million moraine mountain northern ocean pattern peneplain piedmont plains planation plate Plateau platform quartzite reefs regions regolith relief remnants result ridges river rock sand sandstone scarp sea-level sedimentary sediments sheet fractures silcrete soil South Australia southern strata stream structure summit surface tectonic Uluru uplands uplift velocity volcanic waves weathering and erosion weathering front western Western Australia wind zone