Titlebook: Glacier Fluctuations and Climatic Change; Proceedings of the S Johannes Oerlemans Conference proceedings 1989 Springer Science+Business Med

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,Im Mittelpunkt — der Hautpatient,considerably. This greater “standard variation” remains valid also after an exclusion of those ice streams which are larger than the biggest glaciers in the Alps and of the surging glaciers which are much more numerous in the Asiatic mountains. Only since about the 1920’s can a general decline of th

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Jürgen Freyschmidt,Gisela Freyschmidt balance record into the future to a time period adequate for the testing of glacier dynamics models. Initial analysis indicates a good correlation between mass balance and equilibrium line altitude (ELA).

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Bev?lkerungsentwicklung in Deutschland. Differences between the methods within the 27 year period are probably due to map errors, and indicate the need for caution in this type of comparison..Surveying, rather than photogrammetric, methods for determining the volume change of glaciers is preferable, and density profiles are necessary if

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Episodic Palaeozoic Glaciation in the Cape-Karoo Basin, South Africa,low-latitude temperate glaciation, are interbedded in quartz arenites of the Cape Supergroup. Marine sandstone and stratified diamictite deposited during an interglacial, and soft sediment pavements separate basal massive arenaceous diamictite from upper argillaceous diamictite. Permo-Carboniferous

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Quaternary Glaciations and Palaeoclimate of Mount Kenya, East Africa, to assist in refining the glacial chronology and in reconstructing palaeoclimate. Topographic position of deposits, weathering features, degree of soil development, and radiocarbon assist in assigning ages to Quaternary deposits in the Afroalpine and bamboo forest-Hagenia woodland zones. AD and RD

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Tephrochronological Studies of Holocene Glacier Fluctuations in South Iceland, sections up to 11 m deep, and containing up to 78 tephra layers, were logged to a resolution of 0.25 cm. The chronological framework was completed with 15 radiocarbon dates, and by examining the association of the tephra stratigraphy with moraines representing former ice margins, a chronology of Ho

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Relationship of Land Terminating and Fjord Glaciers to Holocene Climatic Change, South Georgia, Anta. The position of the island between mid-latitude southern South America and coastal Antarctica makes it an important link in the chain of Holocene glacier histories in the Southern Hemisphere. A Neoglacial cooling of 1°C and a Little Ice Age cooling of 0.5°C reflect the increased frequency of sout