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Titlebook: Radioglaciology; V. V. Bogorodsky,C. R. Bentley,P. E. Gudmandsen Book 1985 D. Reidel Publishing Company, Dordrecht, Holland 1985 Radioglac

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Structure and Physical State of Glaciers, 0.83 mg m.. At this point the firn has been transformed, by definition, into glacier ice. Further densification then proceeds by a still slower process—bulk compression; here squeezing leads to a reduction in the pore size. The final result is ice that contains air bubbles, but that nevertheless is
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0924-5006 ology, and particularly glaciology, have expanded. Scientific inves­ tigators have obtained new information about all Antarctic regions and thus have created the opportunity to use the Antarctic in the interests of mankind.978-94-010-8830-5978-94-009-5275-1Series ISSN 0924-5006
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V. V. Bogorodsky,C. R. Bentley,P. E. Gudmandsenerschieden. Auch differenzierte Aussagen über aufgrund theoretischer Überlegungen vermutete Schwankungen der Relevanz im Verlauf des Kaufentscheidungsprozesses sind bei Verwendung eines Globalindikators wie Marktanteil oder Markenwert nicht möglich. Erkenntnisse über diese Fragestellungen jedoch sin
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,A Brief Survey of the Earth’s Ice Cover and Methods for its Investigation,Glaciers are multi-year ice masses capable of movement. They form mainly from solid atmospheric precipitation in those areas of the Earth where there is not melting during a warm season and where rainfall is negligible.
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