 cold area " were to be raised above the surface, so that the deposit at present in progress upon its bottom should become the subject of examination by some Geologist of the future, he would find this to consist of a barren Sandstone, including fragments...  The Student, and Intellectual Observer - Page 741869Full view - About this book
 | Royal Society (Great Britain) - 1869 - 674 pages
...of the current which has furnished their materials, and on the other to the temperature of the water brought by that current. If our "cold area" were to...fragments of older rocks, the scanty Fauna of which would iu great degree bear a Boreal character (§ 11); whilst if a portion of our "warm area" were elevated... | |
 | Royal Society (Great Britain) - 1869 - 658 pages
...of the current which has furnished their materials, and on the other to the temperature of the water brought by that current. If our " cold area " were...which would in great degree bear a Boreal character (§ 11); whilst if a portion of our "warm area" were elevated at the same time with the " cold area,"... | |
 | Royal Institution of Great Britain - 1869 - 646 pages
...the other to the temperature of the water brought by that current. If the " cold area " were to bo raised above the surface, so that the deposit at present...degree bear a boreal character ; whilst if a portion of the " warm area " were elevated at the same time with the " cold area," the Geologist would be perplexed... | |
 | 1869 - 516 pages
...of the current which has furnished their materials, and on the other to the temperature of the water brought by that current. If our " cold area " were...fragments of older rocks, the scanty Fauna of which would iu great degree bear a Boreal character ; whilst if a portion of our " warm area " were elevated at... | |
 | Royal Society (Great Britain) - 1869 - 658 pages
...current which has furnished their materials, and on the other to the temperature of the water hrought by that current. If our "cold area" were to be raised...Sandstone, including fragments of older rocks, the scanty Fauua of which would in great degree bear a Boreal character (§ 11); whilst if a portion of our "warm... | |
 | Royal Institution of Great Britain - 1869 - 636 pages
...raised above the surface, so that tho deposit at present in progress upon its bottom should become tho subject of examination by some Geologist of the future,...degree bear a boreal character ; whilst if a portion of the " warm area " were elevated at the same time with the " cold area," the Geologist would be perplexed... | |
 | 1871 - 398 pages
...cold area were to be raised above the surface, so that the deposit at present in progress upon the bottom should become the subject of examination by...of the future, he would find this to consist of a sandstone formed by the disintegration of the older rocks, the faunae of what would in a great degree... | |
 | 1871 - 372 pages
...cold area were to be raised above the surface, so that the deposit at present in progress upon the bottom should become the subject of examination by...of the future, he would find this to consist of a sandstone formed by the disintegration of the older rocks, the faunae of what would in a great degree... | |
 | 1871 - 372 pages
...cold area were to be raised above the surface, so that the deposit at present in progress upon the bottom should become the subject of examination by...of the future, he would find this to consist of a sandstone formed by the disintegration of the older rocks, the faunae of what would in a great degree... | |
 | Liverpool Geological Society - 1874 - 502 pages
...surface, and the deposit now in progress at the bottom to become dry land, some geologist in future might find this to consist of a barren sandstone, including fragments of older rocks, whose scanty fauna would for the most part bear a boreal character; whilst if a portion of the warm... | |
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