Climate and Time in Their Geological Relations: A Theory of Secular Changes of the Earth's ClimateAppleton, 1890 - 577 páginas |
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Página x
... Periods in North and South . - Mr . Darwin's Views quoted . - How Glaciers at the Equator may be accounted for . — Migration across the Equator . 220 T CHAPTER XV . WARM INTER - GLACIAL PERIODS . Alternate CONTENTS .
... Periods in North and South . - Mr . Darwin's Views quoted . - How Glaciers at the Equator may be accounted for . — Migration across the Equator . 220 T CHAPTER XV . WARM INTER - GLACIAL PERIODS . Alternate CONTENTS .
Página xii
... Glaciers . - Permian Conglomerate in Arran . - Professor Hull on Boulder Clay of Perinian Age . - Permian Boulder Clay of Natal . - Oolitic Boulder Conglomerate in Sutherland- shire . - Warm Climate in North Greenland during Oolitic ...
... Glaciers . - Permian Conglomerate in Arran . - Professor Hull on Boulder Clay of Perinian Age . - Permian Boulder Clay of Natal . - Oolitic Boulder Conglomerate in Sutherland- shire . - Warm Climate in North Greenland during Oolitic ...
Página xiii
... Glacier . - Probable Thickness of the Antarctic Ice - cap.— Probable Thickness of Greenland Ice - sheet . - The Icebergs of the Southern Ocean . - Inadequate Conceptions regarding the Magnitude of Continental Ice 368 CHAPTER XXIV . THE ...
... Glacier . - Probable Thickness of the Antarctic Ice - cap.— Probable Thickness of Greenland Ice - sheet . - The Icebergs of the Southern Ocean . - Inadequate Conceptions regarding the Magnitude of Continental Ice 368 CHAPTER XXIV . THE ...
Página xiv
... Glacier . - Jutland and Denmark crossed by Ice . - Sir R. Murchison's Observations . - Orkney , Shetland , and Faroe Islands striated across . - Loess accounted for . - Professor Geikie's Suggestion . - Professor Geikie and B. N. ...
... Glacier . - Jutland and Denmark crossed by Ice . - Sir R. Murchison's Observations . - Orkney , Shetland , and Faroe Islands striated across . - Loess accounted for . - Professor Geikie's Suggestion . - Professor Geikie and B. N. ...
Página xv
... GLACIERS . - THEORIES OF GLACIER - MOTION . Why the Question of Glacier - motion has been found to be so difficult.— The Regelation Theory . - It accounts for the Continuity of a Glacier , but not for its Motion . - Gravitation proved ...
... GLACIERS . - THEORIES OF GLACIER - MOTION . Why the Question of Glacier - motion has been found to be so difficult.— The Regelation Theory . - It accounts for the Continuity of a Glacier , but not for its Motion . - Gravitation proved ...
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amount of heat antarctic aphelion arctic regions Atlantic beds bottom boulder clay Caithness Carboniferous cause consequently considerable density denudation deposits depth descend difference of specific difference of temperature earth's orbit eccentricity ecliptic effect Eocene equal equator equatorial column equatorial regions evidence extent fact feet flow foot-pounds force Geol geological geologists glacial epoch glacier globe Grangemouth greater Greenland Gulf-stream heat received ice-cap icebergs inter-tropical John Herschel land land-ice latitude lower mass mean temperature melting miles Miocene molecules motion North North Sea northern obliquity ocean-currents oceanic circulation perihelion polar column polar regions poles present probably produce Professor quantity of heat radiation regard result river rocks sand Scotland sea-bottom sea-level shear slope snow and ice southern hemisphere specific gravity Straits of Florida stratified stream striated submergence summer sun's supposed surface theory thickness tion tropical warm periods warm water winds winter