The Boston Journal of Philosophy and the Arts, 1-3권Cummings, Hilliard, & Company, 1824 |
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107 페이지
... we understand , means to deposit the greater part of the specimens in the British museum , and in that of the Geological So- ciety . ART . XV . - On certain Elevations of Land Mr F. Clissold's successful Ascent of Mont Blanc . 107.
... we understand , means to deposit the greater part of the specimens in the British museum , and in that of the Geological So- ciety . ART . XV . - On certain Elevations of Land Mr F. Clissold's successful Ascent of Mont Blanc . 107.
108 페이지
ART . XV . - On certain Elevations of Land , connected with the Actions of Volcanoes . By J. MAC CULLOCH , M. D. , F. R.S. ... elevation of submarine strata by the action of volcanic force . These also , which appear to be of dates ...
ART . XV . - On certain Elevations of Land , connected with the Actions of Volcanoes . By J. MAC CULLOCH , M. D. , F. R.S. ... elevation of submarine strata by the action of volcanic force . These also , which appear to be of dates ...
110 페이지
... elevation , or by the receding of the waters , as geologists shall hereafter agree or prove . But there is a perfect and com- plete chasm between the two , at least in the case of marine strata . In the terrestrial or fresh water ones ...
... elevation , or by the receding of the waters , as geologists shall hereafter agree or prove . But there is a perfect and com- plete chasm between the two , at least in the case of marine strata . In the terrestrial or fresh water ones ...
113 페이지
... elevation above the level of the water , reaches to ten feet . The soundings , from which the thickness of this bed of rock might be estimated , have not been given , but these are known to be deep throughout all this sea , and may ...
... elevation above the level of the water , reaches to ten feet . The soundings , from which the thickness of this bed of rock might be estimated , have not been given , but these are known to be deep throughout all this sea , and may ...
116 페이지
... elevation above the water ; and accordingly , those which are entirely flat , are scarcely elevated more than five or six feet above the high - water mark . But as many of them are higher , it is necessary to resort to some new princi ...
... elevation above the water ; and accordingly , those which are entirely flat , are scarcely elevated more than five or six feet above the high - water mark . But as many of them are higher , it is necessary to resort to some new princi ...
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