The Lithology of EdinburghWilliam P. Kennedy, 1859 - 102 pages |
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... Silt - Drift - peat , Sand , and Gravel - Organic Re- mains of Plants and Animals - Chalk Flints - Marine or Lacustrine Origin - Sand Hills - Erratics , 42 63 50 66 CHAPTER VII . Phaneritic series - Raised Beaches - Sea Margins . Ayres ...
... Silt - Drift - peat , Sand , and Gravel - Organic Re- mains of Plants and Animals - Chalk Flints - Marine or Lacustrine Origin - Sand Hills - Erratics , 42 63 50 66 CHAPTER VII . Phaneritic series - Raised Beaches - Sea Margins . Ayres ...
Page xxxix
... silt , and lacustrine diluvium . In another , the causes in operation prevent , in some measure , the tendency of the wearing and lowering of the elevated parts of the earth , and the products are soil and inland sand - drifts . — In a ...
... silt , and lacustrine diluvium . In another , the causes in operation prevent , in some measure , the tendency of the wearing and lowering of the elevated parts of the earth , and the products are soil and inland sand - drifts . — In a ...
Page 29
... silt , exactly as in the diluvial caves . " ( Wern . Mem . vol . viii . p . 65. ) Mr David Milne Home of Milnegraden , to whose important labours we have already referred , says , - " In the Tower Burn near Dunglass , there was lately a ...
... silt , exactly as in the diluvial caves . " ( Wern . Mem . vol . viii . p . 65. ) Mr David Milne Home of Milnegraden , to whose important labours we have already referred , says , - " In the Tower Burn near Dunglass , there was lately a ...
Page 58
... silt or clayey mud , may very frequently be detected . In one place , to the south of Inverleith Cemetery , a thin layer of silt or dark - coloured clay occupied a horizontal posi- tion in the sand , and indicated at one spot , by its ...
... silt or clayey mud , may very frequently be detected . In one place , to the south of Inverleith Cemetery , a thin layer of silt or dark - coloured clay occupied a horizontal posi- tion in the sand , and indicated at one spot , by its ...
Page 65
... of the rocks on which the deposit rests , the character of the materials , and the evidence of intermittency exhibited in its upper members . E 66 CHAPTER VI . Akumite series - Silt - Drift LITHOLOGY OF EDINBURGH . 65.
... of the rocks on which the deposit rests , the character of the materials , and the evidence of intermittency exhibited in its upper members . E 66 CHAPTER VI . Akumite series - Silt - Drift LITHOLOGY OF EDINBURGH . 65.
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Common terms and phrases
Aberdeen appearance Arthur's Seat bones boulder-clay Bressay British Animals Buckland Chair of Natural character Christian Clackmannan clay cloth College Contents Cupar Cuvier dear Sir deposit Dr Chalmers Dr Fleming Dr Fleming's dressed surfaces Edin Edinburgh Edition exhibited favour feel feet Fife fish Flisk foolscap 8vo fossils Free Church genus geologists geology GIDEON MANTELL give Granton gravel Holoptychius hope Hugh Miller illustrative inches indicated influence interesting John Journal kind labours lectures letter Lord Lord Dundas Lyell Memoirs mind Mineralogy minister Natural History Natural Science naturalist neighbourhood Neill notice observed occurred Old Red Sandstone paper parish phenomena Phil Philosophy of Zoology portion present Professor Jameson proof quadrupeds quarry referred regarded remarks rocks Royal Society sand says scientific Scotland Scottish shells shew silt species specimens St Andrews stone strata structure tion views Wernerian Society wrote Zoology
Popular passages
Page xxix - For, to say nothing of half the birds, and some quadrupeds which are almost entirely supported by them, worms seem to be the great promoters of vegetation, which would proceed but lamely without them, by boring, perforating, and loosening the soil, and rendering it pervious to rains and the fibres of plants, by drawing straws and stalks of leaves and twigs into it ; and, most of all, by throwing up such infinite numbers of lumps of earth called worm-casts, which, being their excrement, is a fine...
Page xxix - Earthworms, though in appearance a small and despicable link in the chain of Nature, yet, if lost, would make a lamentable chasm. For to say nothing of half the birds, and some quadrupeds which are almost entirely supported by them, worms seem to be great promoters of vegetation...
Page 96 - A great wave swept over the coast of Spain, and is said to have been sixty feet high at Cadiz. At Tangier, in Africa, it rose and fell eighteen times on the coast; at Funchal, in Madeira, it rose full fifteen feet perpendicular above high-water mark, although the tide, which ebbs and flows there seven feet, was then at half-ebb.
Page xliii - Many horses' heads, and bones of several kinds of deer, the horns of the antelope, the heads and tusks of boars, and the heads of beavers, are also found embedded in it.
Page xxix - Worms probably provide new soil for hills and slopes where the rain washes the earth away ; and they affect slopes, probably, to avoid being flooded. Gardeners and farmers express their detestation of worms ; the former, because they render their walks unsightly, and make them much work ; and the latter, because they think worms eat their green corn. But these men would find, that the earth without worms would soon become cold, hardbound, and void of fermentation ; and consequently sterile...
Page xl - ANGER is one of the sinews of the soul: he that wants it hath a maimed mind, and with Jacob sinew-shrunk in the hollow of his thigh, must needs halt. Nor is it good to converse with such as cannot be angry, and with the Caspian Sea, never ebb nor flow.
Page 46 - Lyell has given to the divisions of the tertiary strata the appellations pleiocene, meiocene, eocene, accordingly as they contain a majority of recent species of shells, a minority of such species, or a small proportion of living species, which may be looked upon as indicating the dawn of the existing state of the animate creation. But in this case, he wisely treats his distinctions, not as definitions, but as the marks of natural groups. " The plurality of species indicated by the name pleiocene,...
Page 51 - ... Taragmite series, formed subsequently to the dressings and groovings of the solid rocks, and, where present, reposing on them. They seem to have been formed when violent aqueous movements were taking place, and probably at a period when the state of our island was widely different from the present. The second, or Akumite series, is chiefly characterised by its laminated clays and sands, and indicates the assorting power of water under circumstances of comparative tranquillity. The third, or Phanerite...
Page 96 - There were twenty-three ships and vessels, great and small, in the harbor of Callao, of which nineteen were sunk ; and the other four, among which was a frigate called St. Fermin, were carried by the force of the waves to a great distance up the country, and left on dry ground at a considerable height above the sea.
Page 2 - It is thus, for example, turned to account by the author of the " Vestiges of the Natural History of Creation.