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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ftciteseerx:oai:CiteSeerX.psu:10.1.1.538.7167 2023-05-15T16:40:07+02:00 Hannah Woodson Sponsor Glenn Kroeger The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.538.7167 http://keckgeology.org/files/pdf/symvol/19th/fingerlakes/woodson.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.538.7167 http://keckgeology.org/files/pdf/symvol/19th/fingerlakes/woodson.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://keckgeology.org/files/pdf/symvol/19th/fingerlakes/woodson.pdf text ftciteseerx 2016-01-08T10:56:08Z 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 Text Ice Sheet Unknown |
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Open Polar |
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ftciteseerx |
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English |
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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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The Pennsylvania State University CiteSeerX Archives |
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Text |
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Hannah Woodson Sponsor Glenn Kroeger |
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Hannah Woodson Sponsor Glenn Kroeger |
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Hannah Woodson Sponsor Glenn Kroeger |
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Hannah Woodson |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.538.7167 http://keckgeology.org/files/pdf/symvol/19th/fingerlakes/woodson.pdf |
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Ice Sheet |
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Ice Sheet |
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http://keckgeology.org/files/pdf/symvol/19th/fingerlakes/woodson.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.538.7167 http://keckgeology.org/files/pdf/symvol/19th/fingerlakes/woodson.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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