 | Edward T W. Polehampton - 1815 - 546 Seiten
...eighty or one hundred yards lower than the one now appearing, To account for the great depositions of salt in the lower parts of this basin, it is necessary...communication of the waters of the sea with those thus collected; and the general course of the streams, the position of the beds of rock-salt, and the... | |
 | Edward Polehampton - 1815 - 540 Seiten
...depositions of salt in the lower parts of this hasin, it is necessary to suppose that some harrier must have been afterwards interposed to prevent the...communication of the waters of the sea with those thus collected ; and the general course of the streams, the position of the beds of. rock-salt, and... | |
 | John Mason Good - 1819 - 910 Seiten
...hundred yards lower than the one now appearing. To account for the great depositions ofsaltin the lo« er parts of this basin, it is necessary to suppose that...communication of the waters of the sea with those thus collected; and the general course of the streams, the position of the bods of rock-salt, and the... | |
 | Sir Richard Phillips - 1821 - 768 Seiten
...hundred feet than the one now appearing. To account for thegreat depositions of salt in the lower pan of this basin, it is necessary to suppose that some...communication of the waters of the sea with those thus collected : and the general course of the streams, the position of the beds of rock-salt, and... | |
| |
To account for the great depositions of salt in the lower parts of this basin, it is necessary to suppose that some barrier must have been afterwards interposed to prevent the free communication of the waters of the sea with those thus collected; and... 