 | William Grainge - 1859 - 406 lehte
...limestone rock, soaring to a height of about 2500 feet above the vale of Eden, and the level beds of red sand-stone deposited in later times at the foot...relatively depressed portion of the same mountain limestone rocks." "With this communicate two cross lines of dislocation, one of which, under the name of the... | |
 | Sir John Lubbock - 1902 - 580 lehte
...five hundred feet above the vale of the Eden and the plain of Carlisle, and the level beds of the New Red Sandstone deposited in •later times at the foot...relatively depressed portion of the same Mountain Limestone series."1 Phillips considered that the Pennines were elevated at the close of the Palaeozoic and before... | |
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... feet above the vale of the Eden and the plain of Carlisle, and the level beds of the red sandstone deposited in later times at the foot of the ancient escarpment, upon the relatively depressed portion of the same mountain limestone series. 