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Deglaciation history of Latvia
2004This chapter discusses the deglaciation history of Latvia. The earliest deglaciation schemes of Latvia were based entirely on morphological features. The spatial distribution of glacial landforms, with crests transverse to glacier movement combined with radiocarbon dates and biostratigraphical evidence, have provided the principal data for the ...
Vitālijs Zelčs, Aivars Markots
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The deglaciation of Maine, U.S.A.
2004Abstract The glacial geology of Maine records the northward recession of the Late Wisconsinan Laurentide Ice Sheet, followed by development of a residual ice cap in the Maine-Quebec border region due to marine transgression of the St. Lawrence Lowland in Canada.
Borns, Harold W., Jr. +8 more
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Deglacial hypsometry of Antarctica
Earth and Planetary Science Letters, 1984Abstract A new and more detailed analysis of the hypsometry of the Antarctic continent, based upon 1° digital data on ice thickness and surface and subglacial elevations, shows that Antarctica, even when deglaciated according to a simple Airy-isostatic model, is an unusual continent.
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A Note on Deglaciation in Tibet
Geological Magazine, 1927Many travellers in Western China have remarked the presence of ancient moraines long since severed from the glaciers which made them, of glacial lakes, ice-worn valleys, perched blocks, and other relics of glaciation. Throughout the Tibetan Marches, in the provinces of Szechuan and Yunnan, such evidence is abundant.
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The chronology of the deglaciation of Scotland
Proceedings of the Geologists' Association, 1950Summary The climatic changes, floral and faunal developments attending the deglaciation of Scotland are considered. The pollen-analysis of peats reveals a forest history and sequence in this country very similar to those in the Baltic area. It confirms and amplifies the deductions drawn from the observations of deposits in sections. These, exposed in
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The last deglaciation of Svalbard
Boreas, 1979Svalbard has been completely covered by an extensive ice sheet at least once, but not in the Late Weichselian (max. 18,000–20,000 years ago). Areas in the western and northwestern parts of Svalbard have been ice‐free for more than 40,000 years. The extension and time of a Barents Shelf glaciation are questions still open for discussion. For most of the
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Sea-glacier retreating rate and climate evolution during the marine deglaciation of a snowball Earth
Global and Planetary Change, 2022Yonggang Liu +2 more
exaly