Contemporary topography of the Finger Lakes Basin in New York is largely due to the retreat of the Laurentide ice sheet over 14,000 years ago. The retreating glaciers carved out steep
| Main Authors: | , |
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.538.7167 http://keckgeology.org/files/pdf/symvol/19th/fingerlakes/woodson.pdf |
| Summary: | Contemporary topography of the Finger Lakes Basin in New York is largely due to the retreat of the Laurentide ice sheet over 14,000 years ago. The retreating glaciers carved out steep |
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