 | Royal Society (Great Britain) - 1864 - 636 стор.
...station to the Himmalaya Mountains ; whereas the effect of the Ocean and the Mountains has been shovrn to be very large. This shows that the effect of variations...mountains must be less than that below the plains, and still less than that below the ocean-bed. If solidification from the fluid state commenced at the... | |
 | John Henry Pratt - 1865 - 200 стор.
...nearest station to the Himmalaya Mountains; whereas the effect of the Ocean and the Mountains has been shown to be very large. This shows that the effect...mountains must be less than that below the plains, and still less than that below the ocean-ted. If solidification from the fluid state commenced at the... | |
 | Cambridge Philosophical Society - 1879 - 616 стор.
...has been found that a deflection of the plumb-line exists towards the sea"f. "In fact," he remarks, "the density of the crust beneath the mountains must be less than that below the plains, and still less than that below the ocean-bed. If solidification from a fluid state commenced at the... | |
 | Osmond Fisher - 1881 - 320 стор.
...no doubt that he has demonstrated the existence of increased density beneath the oceans. He says " in fact the density of the crust beneath the mountains must be less than that below the plains and still less than that below the ocean bed 1 . " That part of the theory" (of unequal radial contraction,... | |
 | Osmond Fisher - 1881 - 332 стор.
...has been found that a deflection of the plumb-line exists towards the sea3. " In fact," he remarks, " the density of the crust beneath the mountains must be less than that below the plains, and still less than that below the ocean-bed. If solidification from a fluid 1 "Figure of the Earth,"... | |
 | Archibald Geikie - 1882 - 996 стор.
...deflection of the plumb-line towards the sea, which has in a number of cases been observed, indicates that " the density of the crust beneath the mountains must be less than that below the plains, and still less than that below the ocean-bed." " Apart therefore from the depressions of the earth's... | |
 | Archibald Geikie - 1885 - 1032 стор.
...the plumb-line towards the веа, which has iu a number of cases been observed, indicates that "tho density of the crust beneath the mountains must be less than that below the plains, and still less than that below the ocean-bed." 2 Apart, therefore, from the depressions of the earth's... | |
 | Osmond Fisher - 1889 - 482 стор.
...be no doubt that he has demonstrated the existence of increased density beneath the oceans. He says "in fact the density of the crust beneath the mountains must be less than that below the plains and still less than that below the ocean bed." " That part of the theory * * * * is well illustrated... | |
 | American Philosophical Society - 1906 - 470 стор.
...nearest station to the Himalayan Mountains; whereas the effect of the Ocean and Mountains has been shown to be very large. This shows that the effect...mountains must be less than that below the plains, and still less than that below the ocean-bed." Again :2 "The circumstance already noticed, that at... | |
 | American Philosophical Society - 1906 - 466 стор.
...nearest station to the Himalayan Mountains; whereas the effect of the Ocean and Mountains has been shown to be very large. This shows that the effect...mountains must be less than that below the plains, and still less than that below the ocean-bed." Again :2 " The circumstance already noticed, that at... | |
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This shows that the effect of variations of density in the crust must be very great, in order to bring about this near compensation. In fact the density of the crust beneath the mountains must be less than that below the plains, and still less than that... 
