The Forms of Water in Clouds & Rivers, Ice & GlaciersH.S. King & Company, 1873 - 192 páginas |
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Página 105
... exist to throw the ice into a state of strain , and to determine its fracture . The principal of these is the more rapid movement of the centre of the glacier . 268. Helped by the labours of an eminent man , now dead , the late Mr. Wm ...
... exist to throw the ice into a state of strain , and to determine its fracture . The principal of these is the more rapid movement of the centre of the glacier . 268. Helped by the labours of an eminent man , now dead , the late Mr. Wm ...
Página 122
... exist . 316. I was asked to reflect upon the condition of a lake stored with fish and offering its surface to very cold air . It was made clear to me that the water on being first chilled would shrink in volume and become heavier , that ...
... exist . 316. I was asked to reflect upon the condition of a lake stored with fish and offering its surface to very cold air . It was made clear to me that the water on being first chilled would shrink in volume and become heavier , that ...
Página 125
... exist . But both life and its conditions set forth the operations of inscrutable Power . We know not its origin ; we know not its end . And the presumption , if not the degradation , rests with those who place upon the throne of the ...
... exist . But both life and its conditions set forth the operations of inscrutable Power . We know not its origin ; we know not its end . And the presumption , if not the degradation , rests with those who place upon the throne of the ...
Página 152
... exists in three different states : as a solid in ice ; as a liquid in water ; as a gas in vapour . To cause it to pass from one of these states to the next following one , heat is necessary . 380. Dig a hole in the ice of the Mer de ...
... exists in three different states : as a solid in ice ; as a liquid in water ; as a gas in vapour . To cause it to pass from one of these states to the next following one , heat is necessary . 380. Dig a hole in the ice of the Mer de ...
Página 158
... exist in the river . In currents of water the motion is not uniform either throughout their width or throughout their depth . The friction of the bottom and of the sides , with the action of local hindrances , causes the motion to vary ...
... exist in the river . In currents of water the motion is not uniform either throughout their width or throughout their depth . The friction of the bottom and of the sides , with the action of local hindrances , causes the motion to vary ...
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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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