The Age and Origin of the Little Diomede Island Upland Surface
ABSTRACT. Geomorphology and projected uplift rates indicate that the upland surface of Little Diomede Island may represent a high sea level stand that occurred 2.6 million years ago in the Bering Strait. The 350–363 m upland surface of the island could be correlative with the York terrace, an uplift...
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| Format: | Text |
| Language: | English |
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1999
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.506.5265 http://pubs.aina.ucalgary.ca/arctic/Arctic54-1-12.pdf |