 | 1854 - 632 Seiten
...and the other 2590 feet above the sea. In no other tract of the world which I have visited, is there seen such a mass of red rocks, (estimated at a thickness of not less than 8000 to 10,000 feet,) so clearly intercalated between the Silurian and the carboniferous strata." In... | |
 | Sir Roderick Impey Murchison - 1854 - 718 Seiten
...2590, feet above the sea. (See Map.) In no other tract of the world which I have visited, is there seen such a mass of red rocks (estimated at a thickness of not less than 8000 to 10,000 feet) so clearly intercalated between the Silurian and the carboniferous strata. For,... | |
 | D. Mackintosh - 1869 - 466 Seiten
...Wales — the Fans of Brecon and Carmarthen, the one 2,860, the other 2,590 feet above the sea ... In no other tract of the world visited by me have...between the Silurian and the Carboniferous strata.' — Siluria, 4th edition, pp. 243, 244. t I was more impressed with the first glimpse of the Brecon... | |
 | William Jerome Harrison - 1878 - 168 Seiten
...South Wales, the Fans of Brecon and Carmarthen — the one 2860, the other 2590 feet above the sea. In no other tract of the world visited by me have...feet) so clearly intercalated between the Silurian and Carboniferous strata.' Whitbach, near Ludlow, is a good locality for fossils, and Leominster, Kingston,... | |
 | Ward, Lock and co, ltd - 1884 - 968 Seiten
...Wales, — the Fans of Brecon, and Carmarthen— the one 2860, and the other 2590 feet above the »ea. In no other tract of the world visited by me have...between the Silurian and the Carboniferous strata. . . Consisting in its lower parts of red and green shale and flagstone, with Mime small ' cornstones... | |
 | Sir John Lubbock - 1902 - 590 Seiten
...2860, the other 2590, feet above the sea. In no other tract of the world which I have visited, is there seen such a mass of red rocks (estimated at a thickness of not less than 8000 to 10,000 feet) so clearly intercalated between the Silurian and the Carboniferous strata." l... | |
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In no other tract of the world visited by me have I seen such a mass of red rocks (estimated at a thickness of not less than 10,000 feet) so clearly intercalated between the Silurian and the Carboniferous strata. 