Nature, Том 7Sir Norman Lockyer Macmillan Journals Limited, 1873 |
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Стр. 2
... sides of the mountain becoming necessarily their natural channels . Thus the successive currents have followed very nearly the same channel ... side of the crater are four large sharp - edged steps of more than a 2 Nov. 7 , 1872 NATURE.
... sides of the mountain becoming necessarily their natural channels . Thus the successive currents have followed very nearly the same channel ... side of the crater are four large sharp - edged steps of more than a 2 Nov. 7 , 1872 NATURE.
Стр. 3
... side that the mountain is rent as far as the base of the cone ; however , it has not ejected any lava , this having found its way out by the bottom of the fissure . During the eruption the lava was raised as far as the summit of the ...
... side that the mountain is rent as far as the base of the cone ; however , it has not ejected any lava , this having found its way out by the bottom of the fissure . During the eruption the lava was raised as far as the summit of the ...
Стр. 4
... side , it would seem as if the chief centre of volcanic action was tending towards that point , and there seems little doubt that one of the next eruptions will place the Observatory more or less in danger . Let us hope , however , that ...
... side , it would seem as if the chief centre of volcanic action was tending towards that point , and there seems little doubt that one of the next eruptions will place the Observatory more or less in danger . Let us hope , however , that ...
Стр. 9
... side of the entering gas , and a fall of temperature on the side of the escaping gas . M. Dufour believes this change of temperature does not take place throughout the gaseous mass , but only at the surface of the diaphragm . He ...
... side of the entering gas , and a fall of temperature on the side of the escaping gas . M. Dufour believes this change of temperature does not take place throughout the gaseous mass , but only at the surface of the diaphragm . He ...
Стр. 10
... sides paleozoic schists are presented , analogous to those of Grätz , and connected by veins of crystalline schist . They are less developed on the north side than on the other . Upon the northern slope the Secondary and Tertiary ...
... sides paleozoic schists are presented , analogous to those of Grätz , and connected by veins of crystalline schist . They are less developed on the north side than on the other . Upon the northern slope the Secondary and Tertiary ...
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