 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 across...  The Edinburgh New Philosophical Journal - Pagina 1051827Volledige weergave - Over dit boek
 | 1828 - 872 pagina’s
...fossil dicotyledonous woods met with in connexion with these strata in Baffin's Bay, and by the fossil wood of Melville Island, Cape York, and Byam Martin...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 pagina’s
...fossil dicotyledonous woods met with in connexion with these strata in Baffin's Bay, and by the fossil wood of Melville Island, Cape York, and Byam Martin...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 pagina’s
...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.... | |
 | Sir William Edward Parry - 1826 - 264 pagina’s
...fossil dicotyledonous woods met with in connexion with these strata in Baffin's Bay, and by the fossil wood of Melville Island, Cape York, and Byam Martin...and we may add, that in the Arctic Regions the only known appearances of this kind are those in Jan Mayen's Island, described by Scoresby. 8. That the... | |
 | 1827 - 932 pagina’s
...strata, m camn s Bay, and by the fossil wood of Melville island, Cape York, and Byam Martin island. G. That the boulders or rolled blocks met with in different...and we may add, that in the Arctic regions the only known appearances of this kind are those in Jan Mayen's island described by Scoresby. 8. That the only... | |
 | 1827 - 700 pagina’s
...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... | |
 | Edinburgh cabinet library - 1830 - 456 pagina’s
...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 pagina’s
...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 pagina’s
...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... | |
 | 1843 - 408 pagina’s
...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... | |
| |
