The Forms of Water in Clouds & Rivers, Ice & GlaciersH.S. King & Company, 1873 - 192 стор. |
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Сторінка xiii
... Pressure 66. Slate Cleavage and Glacier Lamination 67. Conclusion PAGE 122 125 127 132 136 139 140 145 . 147 150 152 · 155 . 155 • 156 · 161 163 · 167 • 171 · 176 183 · • 187 · . 191 THE FORMS OF WATER IN CLOUDS AND RIVERS , ICE ...
... Pressure 66. Slate Cleavage and Glacier Lamination 67. Conclusion PAGE 122 125 127 132 136 139 140 145 . 147 150 152 · 155 . 155 • 156 · 161 163 · 167 • 171 · 176 183 · • 187 · . 191 THE FORMS OF WATER IN CLOUDS AND RIVERS , ICE ...
Сторінка 24
... pressure of the whole atmosphere , being thereby squeezed into a com- paratively small volume . In ascending the mountain , you leave more and more of the atmosphere behind ; the pressure becomes less and less , and by its expansive ...
... pressure of the whole atmosphere , being thereby squeezed into a com- paratively small volume . In ascending the mountain , you leave more and more of the atmosphere behind ; the pressure becomes less and less , and by its expansive ...
Сторінка 65
... ask you to allow , is that you and I are supposed to be making the observations together . The labour F of measuring was undertaken for the most part by Mr. CLOUDS AND RIVERS , ICE AND GLACIERS . 65 Relation of Structure to Pressure.
... ask you to allow , is that you and I are supposed to be making the observations together . The labour F of measuring was undertaken for the most part by Mr. CLOUDS AND RIVERS , ICE AND GLACIERS . 65 Relation of Structure to Pressure.
Сторінка 84
... pressure will shorten the plug ; that the lower part of the Glacier du Géant will to some extent yield to the pressure from behind . 212. Let us test this notion . About three - quarters of a mile above the Tacul , and on the mountain ...
... pressure will shorten the plug ; that the lower part of the Glacier du Géant will to some extent yield to the pressure from behind . 212. Let us test this notion . About three - quarters of a mile above the Tacul , and on the mountain ...
Сторінка 85
... pressure exerted on its front at the rate of about eight inches a day . 217. A river descending the Valley du Géant would behave in substantially the same fashion . It would have its motion on approaching Trélaporte diminished , and it ...
... pressure exerted on its front at the rate of about eight inches a day . 217. A river descending the Valley du Géant would behave in substantially the same fashion . It would have its motion on approaching Trélaporte diminished , and it ...
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Загальні терміни та фрази
Agassiz Aiguille du Dru Aletsch glacier Alps Arveiron beautiful Bergschrund bottom branch glaciers cascade centre chasms cloth cloud Col du Géant Cornhill crevasses crossed Crown 8vo Demy 8vo descend distance eastern side Edition fact fall feet fissures fixed formed freezing Glace Glacier du Géant glacier motion glacier moves Grande Jorasse Grimsel Pass Grindelwald heat ice-fall icebergs icicle Illustrated inches a day labours lake lateral moraine liquefaction liquid London look lower maximum motion measurements medial moraine melting Mer de Glace Mont Montanvert Morteratsch glacier Moulin névé notice numbers observation pass Paternoster Row point of swiftest Pontresina Ponts portion pressure Price produced rate of motion reach regelation Rhone ridge river rocks round sketch sliding slope snow Stake Inches surface swiftest motion Tacul Talèfre telescope temperature thawing theodolite theory transparent Trélaporte Unteraar valley vapour vols waves western width winter yards
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