The Forms of Water in Clouds & Rivers, Ice & GlaciersH.S. King & Company, 1873 - 192 стор. |
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Сторінка vii
... 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.
... 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.
Сторінка viii
John Tyndall. the mountains where the slopes are steep . The ice - cas- cade of the Géant has suffered much from the general waste . Its crevasses are still wild , but the ice - cliffs and séracs of former days are but poorly represented ...
John Tyndall. the mountains where the slopes are steep . The ice - cas- cade of the Géant has suffered much from the general waste . Its crevasses are still wild , but the ice - cliffs and séracs of former days are but poorly represented ...
Сторінка ix
... mountain . In some places this river was more than sixty yards wide , at others it was con- tracted to less than one - fifth of this width . Broken cascades of great height were formed here and there by successive ledges of ice , the ...
... mountain . In some places this river was more than sixty yards wide , at others it was con- tracted to less than one - fifth of this width . Broken cascades of great height were formed here and there by successive ledges of ice , the ...
Сторінка xi
... Mountain Condensers 9. Architecture of Snow 10. Atomic Poles 11. Architecture of Lake Ice • . 1 , 6 11 14 19 • 23 · 27 29 32 35 • 38 • • 43 • 46 • 48 12. The Source of the Arveiron . Ice Pinnacles , Towers , and Chasms of the Glacier ...
... Mountain Condensers 9. Architecture of Snow 10. Atomic Poles 11. Architecture of Lake Ice • . 1 , 6 11 14 19 • 23 · 27 29 32 35 • 38 • • 43 • 46 • 48 12. The Source of the Arveiron . Ice Pinnacles , Towers , and Chasms of the Glacier ...
Сторінка 2
... Mountains ; the Thames in the Cotswold Hills ; the Danube in the hills of the Black Forest ; the Rhine and the Rhone in the ... mountain side . But you very In soon assure yourself that such springs are also fed by 2 THE FORMS OF WATER IN.
... Mountains ; the Thames in the Cotswold Hills ; the Danube in the hills of the Black Forest ; the Rhine and the Rhone in the ... mountain side . But you very In soon assure yourself that such springs are also fed by 2 THE FORMS OF WATER IN.
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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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