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Glacier   /glˈeɪʃər/   Listen
noun
Glacier  n.  An immense field or stream of ice, formed in the region of perpetual snow, and moving slowly down a mountain slope or valley, as in the Alps, or over an extended area, as in Greenland. Note: The mass of compacted snow forming the upper part of a glacier is called the firn, or névé; the glacier proper consist of solid ice, deeply crevassed where broken up by irregularities in the slope or direction of its path. A glacier usually carries with it accumulations of stones and dirt called moraines, which are designated, according to their position, as lateral, medial, or terminal (see Moraine). The common rate of flow of the Alpine glaciers is from ten to twenty inches per day in summer, and about half that in winter.
Glacier theory (Geol.), the theory that large parts of the frigid and temperate zones were covered with ice during the glacial, or ice, period, and that, by the agency of this ice, the loose materials on the earth's surface, called drift or diluvium, were transported and accumulated.






Collaborative International Dictionary of English 0.48








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"Glacier" Quotes from Famous Books



... proceeded to charge two high glasses. Having indicated an arm-chair to me and placed my refreshment near it, he handed me a long, smooth Havana. Then, seating himself opposite to me, he looked at me long and fixedly with his strange, twinkling, reckless eyes—eyes of a cold light blue, the color of a glacier lake. ...
— The Lost World • Arthur Conan Doyle

... of determining prehistoric {60} time.[3] One is called the (1) geologic method, which is based upon the fact that, in a slowly cooling earth and the action of water and frost, cold and heat, storm and glacier and volcanic eruption, the rocks on the earth are of different ages. If they had never been disturbed from where they were first laid down, it would be very easy to reckon time by geological processes. If you had a stone column ...
— History of Human Society • Frank W. Blackmar

... moist as to be friable to the touch; and upon the ice-floes, commencing with a surface-temperature of-30 deg., I found at two feet deep a temperature of-8 deg., at four feet 2 deg., and at eight feet 26 deg.. ... The glacier which we became so familiar with afterwards at Etah yields an uninterrupted stream throughout the year." And he afterwards shows that even the varying texture and quality of the snow deposited during the earlier and later portions of the Arctic winter have their special ...
— Atlantic Monthly, Vol. 9, No. 52, February, 1862 • Various

... knowingly to himself. When he took her up, he had noted the sparkle in her eyes, the color in her cheeks. His little cage had quite warmed with the glow of her repressed eagerness. And now, on the down trip, it was glacier-like. The sparkle and the color were gone. She was frowning, and what little he could see of her eyes was cold and steel-gray. Oh, he knew the symptoms, he did. He was an observer, and he knew it, too, and some day, when he ...
— Moon-Face and Other Stories • Jack London

... inland-ice which, like those of Greenland and Spitzbergen, with its enormous ice-sheet, levels mountains and valleys, and converts the interior of the land into a wilderness of ice, and forms one of the fields for the formation of icebergs or glacier-iceblocks, which play so great a role in sketches of voyages in the Polar seas. I have not myself visited the inland-ice on the northern part of Novaya Zemlya, but doubtless the experience I have previously gained during an excursion with Dr. Berggren on the inland-ice of Greenland in the month ...
— The Voyage of the Vega round Asia and Europe, Volume I and Volume II • A.E. Nordenskieold


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