The Neoglacial landscape and human history of Glacier Bay, Glacier Bay National Park and Preserve, southeast Alaska, USA

被引:23
|
作者
Connor, Cathy [1 ]
Streveler, Greg [2 ]
Post, Austin [3 ]
Monteith, Daniel [4 ]
Howell, Wayne
机构
[1] Univ Alaska SE, Dept Nat Sci, Juneau, AK USA
[2] Icy Strait Environm Serv, Gustavus, AK USA
[3] US Geol Survey, Tacoma, WA USA
[4] Univ Alaska SE, Dept Social Sci, Juneau, AK USA
来源
HOLOCENE | 2009年 / 19卷 / 03期
关键词
Glacier Bay; southeastern Alaska; Neoglacial; 'Little Ice Age'; outwash plain; ethnographic landscape; Tlingit history; HOLOCENE HISTORY; BERING GLACIER; MUIR INLET;
D O I
10.1177/0959683608101389
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The Neoglacial landscape of the Huna Tlingit homeland in Glacier may is recreated through new interpretations of the lower may's fjordal geomorphology, late Quaternary geology and its ethnographic landscape. Geological interpretation is enhanced by 38 radiocarbon dates compiled from published and unpublished sources, as well as 15 newly dated samples. Neoglacial changes in ice positions, outwash and lake extents are reconstructed for c. 5500-200 cal. yr ago, and portrayed as a set of three landscapes at 1600-1000, 500-300 and 300-200 cal. yr ago. This history reveals episodic ice advance towards the may mouth, transforming it from a fjordal seascape into a terrestrial environment dominated by glacier outwash sediments and ice-marginal lake features. This extensive outwash plain was building in lower Glacier may by at least 1600 cal. yr ago, and had filled the lower bay by 500 cal. yr ago. and had filled the lower bay by 500 cal. yr ago. The geologic landscape evokes the human-described landscape found in the ethnographic literature. Neoglacial climate and landscape dynamism created difficult but endurable environmental conditions for the Huna Tlingit people living there. Choosing to cope with environmental hardship was perhaps preferable to the more severely deteriorating conditions outside of the may as well as conflicts with competing groups. The central portion of the outwash plain persisted until it was overridden by ice moving into Icy Strait between 1724-1794. This final ice advance was very abrupt after a prolonged still-stand, evicting the Huna Tlingit from their Glacier may homeland.
引用
收藏
页码:381 / 393
页数:13
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