 | 1828 - 872 lehte
...deposition of the tertiary strata, thesq now frozen regions supported forests of dicotyledonous plants, as is shown by the fossil dicotyledonous woods met...them, and at a period subsequent to the deposition of tbe newest solid strata, namely, those of the tertiary class. 7. That nowhere are there any discoverable... | |
 | 1828 - 878 lehte
...deposition of the tertiary strata, these now frozen regions supported forests of dicotyledonous plants, as is shown by the fossil dicotyledonous woods met...the passage of water across them, and at a period sobsequent to the deposition of the newest solid strata, namely, those of the tertiary class. 7. That... | |
 | 1827 - 452 lehte
...That the "jouldtrs or rolled blocks met with in different quarters, »d in tracts distant from the original localities, afford evidence of the passage of water across them, and at a peri«4 taosequent to the deposition of the newest solid strata, Diffia'r, those of the tertiary class.... | |
 | 1827 - 456 lehte
...fossil dicotyledonous woods met with in connection with these strata in Baffin's Bay, and by the fossif wood of Melville Island, Cape York, and Byam Martin...we may add, that, in the Arctic Regions, the only appearances of this kind are those in Jan Mayen's Island, described by Scoresby. 8. That the only intimations... | |
 | 1827 - 452 lehte
...forests of dicotyledonous plants, as is shewn by the fossil dicotyledonous woods met with in connection with these strata in Baffin's Bay, and by the fossil...we may add, that, in the Arctic Regions, the only appearances of this kind are those in Jan Mayen's Island, described by Scoresby. 8. That the only intimations... | |
 | 1827 - 700 lehte
...6. That the boulders or rolled blocks met with in diflerent quarters, and in tracts distant from the original localities, afford evidence of the passage...the tertiary class. — 7. That nowhere are there auy discoverable traces of the agency of modern volcanoes : and we may add, that in the Arctic regions... | |
 | 1830 - 484 lehte
...and form of the Arctic lands, and their relations to the magnitude and height of other countries. " 6. That the boulders, or rolled blocks, met with in...afford evidence of the passage of water across them, nnd at a period subsequent to the deposition of the newest Neptunian strata. " 7. That possibly the... | |
 | Edinburgh cabinet library - 1830 - 456 lehte
...magnitude and form of the Arctic lands, and their relations to the magnitude and height of other countries. 6. That the boulders or rolled blocks met with in...period subsequent to the deposition of the newest Neptunian strata. 7. That possibly the distribution of the erratic blocks or boulders, was occasioned... | |
 | 1830 - 482 lehte
...lands, and their relations to the magnitude and height of other couutries. " 6. That the bouldrrs, or rolled blocks, met with in different quarters,...period subsequent to the deposition of the newest Neptunian strata. " 7. That possibly the distribution of the erratic blocks, or boulder«, was occasioned... | |
 | Sir John Leslie, Robert Jameson, Hugh Murray - 1832 - 946 lehte
...magnitude and form of the Arctic lands, and their relations to the magnitude and height of other countries. 6. That the boulders or rolled blocks met with in...period subsequent to the deposition of the newest Neptunian strata. 7- That possibly the distribution of the erratic blocks or boulders was occasioned... | |
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Baffin's Bay, and by the fossil wood of Melville Island, Cape York, and Byam Martin Island. 6. That the boulders or rolled blocks met with in different quarters, and in tracts distant from their original localities, afford evidence of the passage of water... 
