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Home > History and Archaeology > History > On the Classification and Geographical Distribution of Crustacea; From the Report on Crustacea of the United States Exploring Expedition Under Captain Charles Wilkes, U.S.N., During the Years 1838-1842
On the Classification and Geographical Distribution of Crustacea; From the Report on Crustacea of the United States Exploring Expedition Under Captain Charles Wilkes, U.S.N., During the Years 1838-1842

On the Classification and Geographical Distribution of Crustacea; From the Report on Crustacea of the United States Exploring Expedition Under Captain Charles Wilkes, U.S.N., During the Years 1838-1842


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This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1853 Excerpt: ... either inside of the warmer tropical current, or else on both sides of it. In the Northern Seas, the system of polar currents is mainly the same, though less regular; their influence is felt on both eastern and western coasts, but more strongly on the eastern. In the Atlantic, the latter reduces the temperature of the waters three or four degrees along the north coast of South America, as far nearly as Cape St. Roque. The cold currents are most apparent along the coasts of continents and about islands, because they are here brought to the surface, the submarine slopes lifting them upward, as they flow on. The limits of their influence towards the equator depends often on the bend of the coast; for a prominent cape or a bend in the outline will change the exposure of a coast from that favourable to the polar current to that favourable to the tropical, or the reverse. Thus it is at Cape Hatteras, on the coast of the United States; Cape Verde, on Western Africa; Cape Blanco, on western South America, etc. These are important principles modifying the courses of the oceanic isothermal lines; we may now proceed to the application of them. In the Atlantic, the warm tropical current flowing westward, is trended somewhat northward by the northern coast of South America, and still more so by the West India Islands, and thus it gradually curves around to parallelism with the coast of the United States. But south of Newfoundland, either wholly from the influence of the colder current which it meets with, or in part from meeting with submarine slopes that serve to deflect it, it passes eastward, and afterwards, where it is again free to expand, it spreads both eastward and northeastward. The flexures in the isocrymes of 74 and 68 F., near the United States coast, thus ...


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Product Details
  • ISBN-13: 9781236105905
  • Publisher: Rarebooksclub.com
  • Publisher Imprint: Rarebooksclub.com
  • Height: 246 mm
  • No of Pages: 62
  • Spine Width: 3 mm
  • Width: 189 mm
  • ISBN-10: 1236105907
  • Publisher Date: 01 May 2012
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Weight: 127 gr

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On the Classification and Geographical Distribution of Crustacea; From the Report on Crustacea of the United States Exploring Expedition Under Captain Charles Wilkes, U.S.N., During the Years 1838-1842
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On the Classification and Geographical Distribution of Crustacea; From the Report on Crustacea of the United States Exploring Expedition Under Captain Charles Wilkes, U.S.N., During the Years 1838-1842
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On the Classification and Geographical Distribution of Crustacea; From the Report on Crustacea of the United States Exploring Expedition Under Captain Charles Wilkes, U.S.N., During the Years 1838-1842

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