Proceedings of the Liverpool Geological Society, Band 4

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Seite 248 - The Superficial Geology of the Country adjoining the Coasts of South-West Lancashire.
Seite 370 - Clark, in a paper read before the Geological. and Polytechnic Society of the West...
Seite 36 - Beds of clay and sand, with round ferruginous concretions and numerous beds, seams, and local deposits of lignite ; great numbers of dicotyledonous leaves, stems, etc...
Seite 132 - What though, in solemn silence, all Move round the dark terrestrial ball ; What though no real voice nor sound Amid their radiant orbs be found; In reason's ear they all rejoice, And utter forth a glorious voice, For ever singing as they shine, The hand that made us is divine.
Seite 358 - St. Michael's Mount is an island at every high water, and, with rare exceptions, a peninsula at every low water. It is about one third of a mile from the mainland. Its name in the ancient Cornish language — "Caraclouse in Cowse...
Seite 132 - Amidst their radiant orbs be found, In reason's ear they all rejoice, And utter forth a glorious voice, For ever singing as they shine, THE HAND THAT MADE US IS DIVINE.
Seite 38 - If we were to regard tbeaffinities of the plants merely, and to compare them with the Miocene of other countries, and also to consider the fact that several of the species are identical with those still living, and that the whole faciès of the flora coincides with that of modern temperate America, little hesitation would be felt in assigning the formation in which they occur to the Miocene period. On the other hand, when we consider the fact that the lower beds of this formation hold the remains...
Seite 365 - I anticipate, will be published in the May number of the "Quarterly Journal of the Geological Society...
Seite 38 - ... fact that several of the species are identical with those still living, and that the whole faciès of the flora coincides with that of modern temperate America, little hesitation would be felt in assigning the formation in which they occur to the Miocene period. On the other hand, when we consider the fact that the lower beds of this formation hold the remains of reptiles of Mesozoic types ; that the beds pass downward into...

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