The most extensive Holocene advance in the Stauning Alper, East Greenland, occurred in the Little Ice Age
The most extensive Holocene advance in the Stauning Alper, East Greenland, occurred in the Little Ice Age
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东格陵兰岛施陶宁阿尔珀地区全新世最广泛的推进发生在小冰河时期
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发表时间：
2008
期刊：
影响因子：
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通讯作者：
G. Denton
中科院分区：
文献类型：
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作者：
B. Hall;C. Baroni;G. Denton
我们提供了关于东格陵兰岛斯图宁阿尔卑斯全新世冰川范围的冰川地质和年代学数据。冰从冰川晚期退回山区的过程至少是在11000卡年前完成的。在此之后唯一有记录的推进发生在过去的几个世纪(小冰期)。因此，我们推测小冰期事件代表了东格陵兰岛这一地区全新世冰川的最大范围。
We present glacial geologic and chronologic data concerning the Holocene ice extent in the Stauning Alper of East Greenland. The retreat of ice from the late-glacial position back into the mountains was accomplished by at least 11 000 cal years B.P. The only recorded advance after this time occurred during the past few centuries (the Little Ice Age). Therefore, we postulate that the Little Ice Age event represents the maximum Holocene ice extent in this part of East Greenland.