 | 1818 - عدد الصفحات: 484
...up, the banks between which the water is hem med in are, for the whole of this distance, every where precipitous, and composed entirely of masses of slate,...found to be a descending bed of mica slate, whose fall was about 30 feet perpendicular, in a slope of 300 yards. Though in this low state of the river it... | |
 | 1818 - عدد الصفحات: 458
...up, the banks between which the water is hemmed in are, for the whole of this distance, everywhere precipitous, and composed entirely of masses of slate,...found to be a descending bed of mica slate, whose fall was about 30 feet perpendicular, in a slope of 300 yards. Though in this low state of the liver it... | |
 | James Hingston Tuckey - 1818 - عدد الصفحات: 630
...banks, between which the water is thus hemmed in, are, for the whole of this distance, every where precipitous, and composed entirely of masses of slate...distinguish by the name of Yellala. The lowest and the most formidable of these barriers was found to be a descending bed of mica slate, whose fall was... | |
 | William Gifford, Sir John Taylor Coleridge, John Gibson Lockhart, Whitwell Elwin, William Macpherson, William Smith, John Murray, Rowland Edmund Prothero (Baron Ernle), George Walter Prothero - 1818 - عدد الصفحات: 574
...precipitous, and composed entirely of masses of slate, which run in ledges from bank to bank, forming those rapids or cataracts, which the natives distinguish...name of yellala ; the lowest and most formidable of which was a fall of about thirty feet perpendicular tjicular in a sloping bed of mica slate about three... | |
 | 1818 - عدد الصفحات: 590
...precipitous, and composed entirely of masses of slate, which run in ledges from bank to bank, forming those rapids or cataracts, which the natives distinguish by the name of yellala; the lowestand most formidable of which was a fall of about thirty feet perpendicular dicular in a sloping... | |
 | 1818 - عدد الصفحات: 594
...every where precipitous, and composed entirely of masses of slate; which, in several places, run iu ledges across from one bank to the other, forming rapids or cataracts, to which the natives give the name of YeUala. The largest of these barriers was discovered to be an... | |
 | J K Tuckey - 1967 - عدد الصفحات: 638
...banks, between which the water is thus hemmed in, are, for the whole of this distance, every where precipitous, and composed entirely of masses of slate...distinguish by the name of Yellala. The lowest and the most formidable of these barriers was found to be a descending bed of mica slate, whose fall was... | |
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... bristled with rocks. The banks, between which the water is thus hemmed in, are, for the whole of this distance, every where precipitous, and composed entirely of masses of slate ; which, in several places, run in ledges across from one bank to the... 