Results 231 to 240 of about 16,487 (268)
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Early deglaciation and paleolake history of Río Cisnes Glacier, Patagonian Ice Sheet (44°S)

Quaternary Research, 2018
The timing, structure, and landscape change during the Patagonian Ice Sheet deglaciation remains unresolved. In this article, we provide a geomorphic, stratigraphic, and geochronological deglacial record of Río Cisnes Glacier at 44°S and also from the ...
J. García   +8 more
semanticscholar   +1 more source

Deglaciation history of Latvia

2004
This 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
openaire   +1 more source

Increasing risk of glacial lake outburst floods from future Third Pole deglaciation

Nature Climate Change, 2021
Guoxiong Zheng   +11 more
semanticscholar   +1 more source

The deglacial hemicycle

Geologische Rundschau, 1964
Absolute age relationships between (a) size reduction of continental ice sheets, (b) glacio-eustatic sea level rise, (c) temperature changes of the ocean surface, and (d) temperature changes on land show that the proper sequence is as follows: first, withdrawal of the ice sheets; second, warming of the land surface; and, third, warming of the ocean ...
openaire   +1 more source

Early Deglaciation of the Labrador Shelf

Science, 1978
Two marine sediment cores from a basin on the southeastern Labrador Shelf penetrate a mud sequence extending back to 21,000 carbon-14 years before the present (B.P.). The benthic foraminifera are dominated by subartic nearshore species indicative of ice-free summer waters.
G, Vilks, P J, Mudie
openaire   +2 more sources

Deglacial hypsometry of Antarctica

Earth and Planetary Science Letters, 1984
Abstract 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.
openaire   +1 more source

Climate Records Covering the Last Deglaciation

Science, 1995
The oxygen-18/oxygen-16 ratio of molecular oxygen trapped in ice cores provides a time-stratigraphic marker for transferring the absolute chronology for the Greenland Ice Sheet Project (GISP) II ice core to the Vostok and Byrd ice cores in Antarctica.
T, Sowers, M, Bender
openaire   +2 more sources

The rapid deglaciation of the Skagafjörður fjord, northern Iceland

Boreas, 2018
The Skagafjörður fjord in northern Iceland is located between the Tröllaskagi Peninsula in the east and the Skagi Peninsula in the west. The tributary valleys of the fjord originate in the highland area about 15 km north of the Hofsjökull icecap.
N. Andrés   +4 more
semanticscholar   +1 more source

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