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 xv
... Grangemouth . - Channels not excavated by Sea nor by Ice . - Section of buried Channel at Grange- mouth . Mr. Milne Home's Theory . - German Ocean dry Land.- Buried River Channel from Kilsyth to the Clyde . — Journal of Borings ...
... Grangemouth . - Channels not excavated by Sea nor by Ice . - Section of buried Channel at Grange- mouth . Mr. Milne Home's Theory . - German Ocean dry Land.- Buried River Channel from Kilsyth to the Clyde . — Journal of Borings ...
Página 466
... Grangemouth . - Channels not excavated by Sea nor by Ice . - Section of buried Channel at Grangemouth . - Mr . Milne Home's Theory . - German Ocean dry Land . - Buried River Channel from Kilsyth to the Clyde .-- Journal of Borings ...
... Grangemouth . - Channels not excavated by Sea nor by Ice . - Section of buried Channel at Grangemouth . - Mr . Milne Home's Theory . - German Ocean dry Land . - Buried River Channel from Kilsyth to the Clyde .-- Journal of Borings ...
Página 468
... Grangemouth , Firth of Forth . --These borings reveal the existence of a deep pre - glacial , or perhaps inter - glacial , trough or hollow , extending from the Clyde above Bowling across the country by Kilsyth , along the valley of the ...
... Grangemouth , Firth of Forth . --These borings reveal the existence of a deep pre - glacial , or perhaps inter - glacial , trough or hollow , extending from the Clyde above Bowling across the country by Kilsyth , along the valley of the ...
Página 472
... from Kilsyth to the river Forth at Grangemouth , and I found unmistakable evidence that the eastern portion of it , stretching from the watershed to the Forth , had been cut out , not by the sea , but by a 472 CLIMATE AND TIME .
... from Kilsyth to the river Forth at Grangemouth , and I found unmistakable evidence that the eastern portion of it , stretching from the watershed to the Forth , had been cut out , not by the sea , but by a 472 CLIMATE AND TIME .
Página 476
... Grangemouth is 260 feet below the present sea - level ; add to this 150 feet , and we have 410 feet as its depth here at the time in question . If this hollow was scooped out by the sea , how then does it thus happen that at the place ...
... Grangemouth is 260 feet below the present sea - level ; add to this 150 feet , and we have 410 feet as its depth here at the time in question . If this hollow was scooped out by the sea , how then does it thus happen that at the place ...
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Términos y frases comunes
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