The Forms of Water in Clouds & Rivers, Ice & GlaciersH.S. King & Company, 1873 - 192 páginas |
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Página vii
... present surface lying far below . The visible and continual breaking away of the moraines , left thus stranded on the mountain flank , explains the absence of ancient ridges on 累 E the mountains where the slopes are steep . The ice.
... present surface lying far below . The visible and continual breaking away of the moraines , left thus stranded on the mountain flank , explains the absence of ancient ridges on 累 E the mountains where the slopes are steep . The ice.
Página 45
... present position , and leading directly up to the cleft . But these gullies , or couloirs , are very dangerous , being the pathways of stones falling from the heights . We will therefore take the rocks to the left of the gully , by ...
... present position , and leading directly up to the cleft . But these gullies , or couloirs , are very dangerous , being the pathways of stones falling from the heights . We will therefore take the rocks to the left of the gully , by ...
Página 57
... present one undoubtedly existed here in 1820. But was it the identical crevasse now existing ? Is the ice riven here to - day the same as that riven fifty - one years ago ? By no means . How is this proved ? By the fact that more than ...
... present one undoubtedly existed here in 1820. But was it the identical crevasse now existing ? Is the ice riven here to - day the same as that riven fifty - one years ago ? By no means . How is this proved ? By the fact that more than ...
Página 103
... present Glacier du Géant , where the slope would become gentle once more . 263. Think of the névé moving over such a surface . It descends from the Col till it reaches the brow just referred to . It crosses the brow , and must bend down ...
... present Glacier du Géant , where the slope would become gentle once more . 263. Think of the névé moving over such a surface . It descends from the Col till it reaches the brow just referred to . It crosses the brow , and must bend down ...
Página 110
... present bowledge will enable you to master it in a moment . Da remember at an early period of our researches that we crossed the Mer de Glace from the Chapean side to the Montanvert side . I then desired you to notice that the Chapeau ...
... present bowledge will enable you to master it in a moment . Da remember at an early period of our researches that we crossed the Mer de Glace from the Chapean side to the Montanvert side . I then desired you to notice that the Chapeau ...
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Términos y frases comunes
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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