The Forms of Water in Clouds & Rivers, Ice & GlaciersH.S. King & Company, 1873 - 192 стор. |
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Сторінка 42
John Tyndall. V.COOPER SA PJUSTYNE.DEL . THE MER DE GLACE , SHOWING MONT TACUL AND THE GRANDE JORASSE , WITH OUR CLEFT ABOVE TRÉLAPORTE TO THE RIGHT . THE FORMS OF WATER IN CLOUDS , RIVERS , ETC.
John Tyndall. V.COOPER SA PJUSTYNE.DEL . THE MER DE GLACE , SHOWING MONT TACUL AND THE GRANDE JORASSE , WITH OUR CLEFT ABOVE TRÉLAPORTE TO THE RIGHT . THE FORMS OF WATER IN CLOUDS , RIVERS , ETC.
Сторінка 44
... Trélaporte to the right you see a most angular cleft in the rocks , in the middle of which vands an isolated pillar , hewn out by the weather . Per next object is to get to the tower of rock to the left that cleft , for from that ...
... Trélaporte to the right you see a most angular cleft in the rocks , in the middle of which vands an isolated pillar , hewn out by the weather . Per next object is to get to the tower of rock to the left that cleft , for from that ...
Сторінка 46
... Trélaporte , and walked right up the Glacier du Géant . We should have found ice under our feet up to the bottom of the cascade . It is not so compact as the ice lower down , but you would not think of refusing to call it ice . 120. As ...
... Trélaporte , and walked right up the Glacier du Géant . We should have found ice under our feet up to the bottom of the cascade . It is not so compact as the ice lower down , but you would not think of refusing to call it ice . 120. As ...
Сторінка 74
... Trélaporte . Here the convex curvature of the valley turns again to the east . Across this por- tion of the glacier a line was set out on July 28 , and from measurements on the 31st , the rate of motion per 24 hours was determined ...
... Trélaporte . Here the convex curvature of the valley turns again to the east . Across this por- tion of the glacier a line was set out on July 28 , and from measurements on the 31st , the rate of motion per 24 hours was determined ...
Сторінка 76
... Trélaporte the eastern half of the glacier again moves more rapidly than the western half . 4. That these changes in ... Trélaporte this line would lie east of the centre ; at the Ponts it would lie west of the centre ; hence in passing ...
... Trélaporte the eastern half of the glacier again moves more rapidly than the western half . 4. That these changes in ... Trélaporte this line would lie east of the centre ; at the Ponts it would lie west of the centre ; hence in passing ...
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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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