The Forms of Water in Clouds & Rivers, Ice & GlaciersH.S. King & Company, 1873 - 192 стор. |
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Сторінка ix
... bottom of the torrent was deep soft sand , which , after the water had passed , could be seen to to have been tortured into huge funnels by the whirling eddies overhead . Soon after we reached the Bel Alp , on the occa- sion just ...
... bottom of the torrent was deep soft sand , which , after the water had passed , could be seen to to have been tortured into huge funnels by the whirling eddies overhead . Soon after we reached the Bel Alp , on the occa- sion just ...
Сторінка xii
... Bottom of Glacier 80 30. Longitudinal Compression of a Glacier . 34. Motion of the Grindelwald and Aletsch Glacier 29. Lateral Compression of a Glacier 31. Sliding and Flowing . Hard Ice and Soft Ice 32. Winter on the Mer de Glace 33 ...
... Bottom of Glacier 80 30. Longitudinal Compression of a Glacier . 34. Motion of the Grindelwald and Aletsch Glacier 29. Lateral Compression of a Glacier 31. Sliding and Flowing . Hard Ice and Soft Ice 32. Winter on the Mer de Glace 33 ...
Сторінка 7
... bottom of the glacier the river rushes . In the glacier of the Rhone you thus find the source of the river Rhone . 18. But again we have not reached the real begin- ning of the river . You soon convince yourself that this earliest water ...
... bottom of the glacier the river rushes . In the glacier of the Rhone you thus find the source of the river Rhone . 18. But again we have not reached the real begin- ning of the river . You soon convince yourself that this earliest water ...
Сторінка 46
... 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 we approach the fall , the smooth and un- broken character of the glacier changes more and more . We ...
... 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 we approach the fall , the smooth and un- broken character of the glacier changes more and more . We ...
Сторінка 51
... bottom of the ice - fall , rising as it were from the body of the glacier . Beyond all of these we can notice the lateral moraine of the Mer de Glace . 131. These stripes are the medial moraines of the Mer E 2 CLOUDS AND RIVERS , ICE ...
... bottom of the ice - fall , rising as it were from the body of the glacier . Beyond all of these we can notice the lateral moraine of the Mer de Glace . 131. These stripes are the medial moraines of the Mer E 2 CLOUDS AND RIVERS , ICE ...
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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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