Travels in North America: With Geological Observations on the United States, Canada, and Nova Scotia, Volume 2J. Murray, 1845 - 5 pagina's |
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Pagina iii
... Drift . - Structure and Origin of Appalachians.— Theory of Subsidence and Contraction of Subterranean Fluid . Kentucky Farmers . Emigrants . - Cumberland Coal Field . - Clay with Stigmaria . — Marine Shells in Coal Measures near ...
... Drift . - Structure and Origin of Appalachians.— Theory of Subsidence and Contraction of Subterranean Fluid . Kentucky Farmers . Emigrants . - Cumberland Coal Field . - Clay with Stigmaria . — Marine Shells in Coal Measures near ...
Pagina iv
... Drift , and Deposits with Bones of Mastodon on the Ohio -- - - 58 CHAPTER XVIII . - Cincinnati . -Journey across Ohio to Cleveland . - New Clearings . Rapid Progress of the State since the Year 1800 . -Increase of Population in the ...
... Drift , and Deposits with Bones of Mastodon on the Ohio -- - - 58 CHAPTER XVIII . - Cincinnati . -Journey across Ohio to Cleveland . - New Clearings . Rapid Progress of the State since the Year 1800 . -Increase of Population in the ...
Pagina v
... Drift more than 500 Feet above the Sea.- -Lake St. Peter . - Falls of Maskinongé.- Deposit of Shells at Beauport , near Quebec.- Agreement with Swedish Fossils . Shells in Boulder Formation of Lake Champlain.- Burlington , Vermont ...
... Drift more than 500 Feet above the Sea.- -Lake St. Peter . - Falls of Maskinongé.- Deposit of Shells at Beauport , near Quebec.- Agreement with Swedish Fossils . Shells in Boulder Formation of Lake Champlain.- Burlington , Vermont ...
Pagina 9
... drift with transported blocks , which forms so marked a feature in the hills and valleys of New England . I have before spoken briefly of the structure of the Alleghanies ( p . 92. ) and their geological conformation , as explained by ...
... drift with transported blocks , which forms so marked a feature in the hills and valleys of New England . I have before spoken briefly of the structure of the Alleghanies ( p . 92. ) and their geological conformation , as explained by ...
Pagina 31
... drift and boulders , so common in the north . The carboniferous strata were exposed on the banks of every small streamlet , and not con- cealed by any superficial covering . On reaching one of those innumerable towns to which , as if ...
... drift and boulders , so common in the north . The carboniferous strata were exposed on the banks of every small streamlet , and not con- cealed by any superficial covering . On reaching one of those innumerable towns to which , as if ...
Overige edities - Alles bekijken
Travels in North America: With Geological Observations on the ..., Volume 2 Sir Charles Lyell Volledige weergave - 1845 |
Travels in North America: With Geological Observations on the ..., Volume 2 Sir Charles Lyell Volledige weergave - 1845 |
Travels in North America: With Geological Observations on the United States ... Charles Lyell Geen voorbeeld beschikbaar - 2007 |
Veelvoorkomende woorden en zinsdelen
abundant Alleghany America ancient appears bank Bay of Fundy beds bituminous bones boulder formation brachiopoda British Brongn Canada Cape Breton Cincinnati clay cliffs coal measures coal-measures coloured corals Debert River denudation deposits Devonian district drift Europe feet high feet thick ferns forest formed fossiliferous fossils Frostburg furrows genus Geological Society geologists gneiss grænlandica granite gravel grit gypsiferous gypsum height hills horizontal hypogene inches Island Joggins Lake Erie Lake Ontario land Lawrence layers Lepidodendron limestone loam Lower Silurian marine shells mastodon miles millstone grit Minudie Monongahela Montreal mountain nearly Niagara northern Nova Scotia observed occur Ohio organic remains origin Pecopteris Pictou quartzose Red sandstone ridges sand seams of coal shale shore Shubenacadie Sigillaria Silurian rocks slate South Joggins species Stigmaria strata stratified surface terrace trilobites Upper Silurian valley Verneuil Windsor York
Populaire passages
Pagina 33 - The same conformity of organization is not less obvious in the osteological structure of these people, as seen in the squared or rounded, head, the flattened or vertical occiput, the high cheek bones, the ponderous maxillae, the large quadrangular orbits, and the low, receding forehead.
Pagina 127 - He also stated that fragments of the " black stone" which fell from the summit of the cliff, » a pile of which, d, fig. 16, lay at its base, were often frozen into the ice, and moved along with it. I then examined these fallen blocks of amygdaloid scattered round me, and observed in them numerous geodes coated with quartz crystals. I have no doubt that the hardness of these gravers, firmly fixed in masses of ice, which, although only fifteen feet thick, are often of considerable horizontal extent,...
Pagina 186 - This lake-like scenery continues for about fifteen miles, during which the fall of the river scarcely exceeds as many feet, but on reaching the rapids, it descends over a limestone bed about 50 feet in less than a mile, and is then thrown down about 165 feet perpendicularly at the Falls.
Pagina 125 - ... being N. 35° E., or corresponding to that of the shore at this point. After walking about a quarter of a mile, I found another set of similar furrows, having the same general direction within five degrees ; and I made up my mind that if these grooves could not be referred to the modern instrumentality of ice, it would throw no small doubt on the glacial hypothesis.
Pagina 22 - I was truly astonished, now that I had entered the hydrographical basin of the Ohio, at beholding the richness of the seams of coal, which appear everywhere on the flanks of the hills and at the bottom of the valleys, and which are accessible in a degree I never witnessed elsewhere. The time has not yet arrived, the soil being still densely covered with the primeval forest, and manufacturing industry...
Pagina 35 - European nation, appears to me a baseless hypothesis, however true it may be that the aboriginal Americans had derived some hints from foreign sources If, then, a large continent can be inhabited by hundreds of tribes, all belonging to the same race, and nearly all remaining for centuries in a state of apparently hopeless barbarism, while two or three of them make a start in their social condition, and in the arts and sciences; if these same nations, when brought into contact with Europeans, relapse...
Pagina 25 - Horizontal galleries may be driven everywhere at very slight expense, and so worked as to drain themselves, while the cars, laden with coal and attached to each other, glide down on a railway, so as to deliver their burden into barges moored to the river's bank.
Pagina 49 - Secondly, a gradual submergence then took place, bringing down each part of the land successively to the level of the waters, and then to a moderate depth below them. Large islands and bergs of floating ice came from the north, which, as they grounded on the coast and on shoals, pushed along all loose materials of sand and pebbles, broke off...
Pagina 126 - I found another set of similar furrows, having the same general direction within five degrees ; and I made up my mind that, if these grooves could not be referred to the modern instrumentality of ice, it would throw no small doubt on the glacial hypothesis. When I asked my guide — a peasant of the neighborhood — whether he had ever seen much ice on the spot where we stood, the heat was so excessive (for we were in the latitude of the south of France, 45° north), that I seemed to be putting a...
Pagina 125 - ... passage of sand and gravel, washed over it from the talus of fallen fragments, which lies at the foot of the cliff on the beach above. The slow but constant undermining of the perpendicular cliff forming this promontory, round which the powerful currents caused by the tide sweep backwards and forwards with prodigious velocity, must satisfy every geologist that the denudation by which the ledge in question has been exposed to view is of modern date. Whether the rocks forming the cliff extended...