Earth Sculpture; Or, The Origin of Land-forms |
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Page viii
... in determining Surface- features Texture and Mineralogical composition of Rocks in rela- tion to Weathering - Forms assumed by various Rocks . 128 150 173 · 195 CHAPTER X LAND - FORMS MODIFIED BY GLACIAL ACTION · viii CONTENTS.
... in determining Surface- features Texture and Mineralogical composition of Rocks in rela- tion to Weathering - Forms assumed by various Rocks . 128 150 173 · 195 CHAPTER X LAND - FORMS MODIFIED BY GLACIAL ACTION · viii CONTENTS.
Page ix
... MODIFIED BY GLACIAL ACTION ( continued ) . 232 Former Glacial conditions of Northern Europe - Extent of the old Inland Ice - Glacial character of Boulder - clay - Central Region of Glacial Erosion and Peripheral Area of Glacial ...
... MODIFIED BY GLACIAL ACTION ( continued ) . 232 Former Glacial conditions of Northern Europe - Extent of the old Inland Ice - Glacial character of Boulder - clay - Central Region of Glacial Erosion and Peripheral Area of Glacial ...
Page 2
... But with increased knowledge these views gradu- ally became modified . Eventually , it was recognised that no hard - and - fast line separates past and present . The belief in world - wide , or nearly world 2 EARTH SCULPTURE.
... But with increased knowledge these views gradu- ally became modified . Eventually , it was recognised that no hard - and - fast line separates past and present . The belief in world - wide , or nearly world 2 EARTH SCULPTURE.
Page 31
... leached out at the surface and carried away by streams and rivers , it is obvious that in course of time the land cannot fail to have been con- siderably modified by chemical action alone . In point of AGENTS OF DENUDATION 31.
... leached out at the surface and carried away by streams and rivers , it is obvious that in course of time the land cannot fail to have been con- siderably modified by chemical action alone . In point of AGENTS OF DENUDATION 31.
Page 32
James Geikie. siderably modified by chemical action alone . In point of fact , it can be shown that from the surface of cer- tain regions hundreds of feet of various calcareous rocks have thus been gradually removed ; while in other ...
James Geikie. siderably modified by chemical action alone . In point of fact , it can be shown that from the surface of cer- tain regions hundreds of feet of various calcareous rocks have thus been gradually removed ; while in other ...
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Common terms and phrases
accumulation Alpine Alps anticlines basalt base-level basins become beds boulder-clay Carboniferous character cirques cliffs coast-lines coasts configuration Cretaceous crust crustal movements crystalline débris denudation deposits depressions depth detritus direction dislocations drainage elevation epigene epigene action epigene agents eroded escarpments feet fiords flow fluvio-glacial fluvio-glacial deposits folds gently geological structure glacial action glacial erosion glaciers gradually ground-moraines hills hollows horizontal strata ice-flow ice-sheet igneous rocks inclined indented infrequently irregular islands joints kind laccoliths lakes land land-forms land-surface lava less limestone low grounds materials mer de glace modified moraines mountain-chain mountain-valleys mountains névé normal faults Old Red Sandstone outcrops owe their origin plain of erosion plateau regions relatively result ridges rock-basins rock-masses sand sandstone schistose schists SECTION sediment slopes Southern Uplands strata streams and rivers superficial surface surface-features synclinal tectonic tend thickness tion tracts traversed underground undulating usually valleys vertical volcanic wind