Class-book of GeologyMacmillan and Company, 1890 - 516 σελίδες |
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Σελίδα xviii
... Sheet 100. Examples of normal Faults IOI . Sections to show the relations of Plications to reversed Faults 102. Throw ... Sheets 195 196 197 198 . 198 202 203 204 205 109. Section to illustrate evidence of contemporaneous volcanic action ...
... Sheet 100. Examples of normal Faults IOI . Sections to show the relations of Plications to reversed Faults 102. Throw ... Sheets 195 196 197 198 . 198 202 203 204 205 109. Section to illustrate evidence of contemporaneous volcanic action ...
Σελίδα 23
... sheets or heaps of loose earth or sand , but that much of it is washed off the land by rain or blown into the rivers or into the sea by wind . We have now to consider the part taken by Running Water in this transport . From the single ...
... sheets or heaps of loose earth or sand , but that much of it is washed off the land by rain or blown into the rivers or into the sea by wind . We have now to consider the part taken by Running Water in this transport . From the single ...
Σελίδα 26
... sheets of sand begin to make their appearance , and at last when the stream reaches the plains , no sediment of coarser grain than mere silt may be seen in its channel . It is thus obvious that in the constant transport maintained by ...
... sheets of sand begin to make their appearance , and at last when the stream reaches the plains , no sediment of coarser grain than mere silt may be seen in its channel . It is thus obvious that in the constant transport maintained by ...
Σελίδα 45
... sheets of water and the successive stages of their diminution and disappearance are shown by the series of alluvial shelves known as " parallel roads . " The highest of these is 1140 feet , the middle 1059 feet , and the lowest 847 feet ...
... sheets of water and the successive stages of their diminution and disappearance are shown by the series of alluvial shelves known as " parallel roads . " The highest of these is 1140 feet , the middle 1059 feet , and the lowest 847 feet ...
Σελίδα 47
... sheets of water have no outlet ; yet there is reason to believe that most of them were at first fresh , and discharged their outflow like ordinary lakes . Owing to geological changes of level and of climate , they have long ceased to ...
... sheets of water have no outlet ; yet there is reason to believe that most of them were at first fresh , and discharged their outflow like ordinary lakes . Owing to geological changes of level and of climate , they have long ceased to ...
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Άλλες εκδόσεις - Προβολή όλων
Συχνά εμφανιζόμενοι όροι και φράσεις
abundant accumulated acid Ammonites ancient Assistant Master beds BOOK bottom Brachiopods calcareous calcite Cambrian Cambridge carbonate of lime Carboniferous Chapter chiefly clay College containing corals Cretaceous crinoids crystalline crystals decay deposits detritus Devonian earth earth's crust Edited ELEMENTARY Eocene eruptive Europe evidence example extinct fauna Fcap feet fissures fossils genera GEOGRAPHY geological history glacier globe gradually granite gravel GREEK ground Illustrated Jurassic kinds known lakes land lava layers limestone living lower marine marls mass materials Mesozoic mineral Miocene mountains natural occur Old Red Sandstone organic remains original Palæozoic Paleozoic period Permian plants and animals Pliocene present preserved Prof Professor quartz Red Sandstone regions revised rivers rocks sand schists sediment sedimentary sedimentary rocks shales sheets shells siliceous Silurian soil solid sometimes species stone strata structure substance surface terrestrial Tertiary thick trace Triassic upper various vegetation volcanic
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