An Introduction to Geology: Intended to Convey a Practical Knowledge of the Science, and Comprising the Most Important Recent Discoveries, with Explanations of the Facts and Phenomena which Serve to Confirm Or Invalidate Various Geological TheoriesHezekiah Howe, 1833 - 479 strán (strany) |
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Alps ancient animals appear basalt bed of coal beds of limestone bones calcareous called caverns chalk Charnwood Forest clay coal coal strata coal-field colour composed conchology considerable contain covered crater crystals deposited Derbyshire diluvial discovered distance districts dyke earth earthquakes elevation England epoch eruptions extend feet felspar fissures formation formed fossil fragments frequently geologists globe gneiss granite green sand greywacke gypsum hills hornblende igneous imbedded intermixed ironstone island lakes land lava lias lime London clay lower magnesian limestone marine marl mass mastodon metallic mica mica-slate miles mineral mountain limestone nearly numerous observed occur ocean oolite organic remains plants Plate porphyry present probably quadrupeds quartz range red marl red sandstone rivers rock-salt sand secondary strata shale shells side slate sometimes species stone stratum subterranean supposed surface tain temperature tertiary strata thickness tion toadstone trachyte transition limestone transition rocks upper valleys vegetable veins volcanic Wealden
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Strana 454 - generations of the heavens and the earth when they were created, in the day that the Lord God made the heavens and the earth." Which of the three senses shall we adopt? If the
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Strana 445 - from a verb, which, from Joel ii. 22, we learn the meaning is to spring, to shoot, to vegetate, " Be not afraid, ye beasts of the field, for the pastures of the wilderness do spring, (dasheu.") In the
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Strana 264 - well about the fort, as on the declivities of the mountain, alarmed by this appearance, betook themselves to flight; but before they could all save themselves, the mountain began to give way, and the greatest part of it actually fell in, and disappeared in the earth. At
Strana 126 - beds of workable coal, the total average thickness of which is 95 feet, and the quantity contained in each acre is 100,000 tons, or 65,000,000 tons per square mile. If from this we deduct one half for waste, and for the minor extent of the upper beds, we shall have a clear supply of coal, equal to