I do not believe in the lapse of a long interval of time between the silurian and carboniferous deposits, — in fact, in a Devonian period. 4th. The same blending of corals has been found in Ireland, the Bas Boulonnais, and in Devonshire, where silurian... Journal of the Geological Society of Dublin - Seite 186von Geological Society of Dublin - 1860Vollansicht - Über dieses Buch
| British Association for the Advancement of Science. Meeting - 1861 - 604 Seiten
...Silurian and Carboniferous deposits, in fact in a Devonian period. " The same blending of corals bus been found in Ireland, the Bas Boulonnais, and in...forms are of common occurrence in the same localities §." It should be remembered that the statement with which we have here to deal is that the "blending... | |
| Sir Francis Leopold M'Clintock - 1859 - 504 Seiten
...be identical with the variety of the Irish carboniferous S. geniculata, in which the corallites are at a distance from each other somewhat exceeding their...the carboniferous beds proper of Melville Island and Bnthurst Island, there were not found, so far as I am aware, any corals of the same character as those... | |
| Sir Francis Leopold M'Clintock - 1860 - 438 Seiten
...distance from each other somewhat exceeding their diam* Vide Arctic Expeditions, 1854-55, p. 254. eters, and in which the connecting tubes are about two diameters...Island, there were not found, so far as I am aware, any corals of the same character as those at Griffith's Island, Cornwallis Island, and Beechey Island,... | |
| Sir Francis Leopold M'Clintock - 1860 - 452 Seiten
...for the following reasons: — 1st. The Syringopores of Griffith's Island were found at an etevation of 400 feet above the sea, and, therefore, could not...Island, there were not found, so far as I am aware, any corals of the same character as those at Griffith's Island, Cornwallis Island, and Beechey Island,... | |
| Royal Geological Society of Ireland - 1860 - 414 Seiten
...specimens were apparently of the same texture and composition as the native rock, whenever the latter waa visible from under the snow. 3rd. I do not believe...Island, there were not found, so far as I am aware, any corals of the same character as those at Griffith's Island, Cornwallis Island, and Beechy Island, which... | |
| 1860 - 400 Seiten
...was visible from under the snow. 4th. The same blending of corals has been found in Ireland, theBas Boulonnais, and in Devonshire, where Silurian and...forms are of common occurrence in the same localities. 3rd. I do not believe in the lapse of a long interval of time between the Silurian and Carboniferous... | |
| American Philosophical Society - 1860 - 524 Seiten
...collected apparently from the same beds, are a curious mixture of silurian and carboniferous types. " The same blending of corals has been found in Ireland, the Bas Boulonnais, and in Devonshire." He concludes by saying, "I do not believe in the lapse of a long interval of time between the silurian... | |
| British Association for the Advancement of Science - 1861 - 602 Seiten
...long interval of time between the Silurian and Carboniferous deposits, in fact in a Devonian period. " The same blending of corals has been found in Ireland,...forms are of common occurrence in the same localities §." It should be remembered that the statement with which we have here to deal is that the " blending... | |
| American Philosophical Society - 1861 - 504 Seiten
...collected apparently from the same beds, arc a curious mixture of silurian and carboniferous types. " The same blending of corals has been found in Ireland, the Bas Boulonnais, and in Devonshire." He concludes by saying, "I do not believe in the lapse of a long interval of time between the silurian... | |
| 1868 - 758 Seiten
...interval of time between the Silurian and Carboniferous deposits — in fact, in a Devonian period. The same blending of corals has been found in Ireland,...are of common occurrence in the same localities."! The truth of this assertion is, perhaps, more than doubtful. It is known that the eminent authorities,... | |
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