Abstract
During the 1993 cruise of R/V Polar Duke, seismic data were collected from Seno De Las Montañas (Fig. 1), a fjord that is isolated from outflow of the South Patagonia Ice Cap by a prominent bedrock ridge and contains significant deposits from late glacial readvances which flowed into the fjord from the south.
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References
DaSilva, J. L., J. B. Anderson, and J. A. Strayers, Seismic facies changes along a 24° latitudinal transect, the Inland Passage of Chile to the northern Antarctic Peninsula, Marine Geology, in press, 1996.
Laventer, A., J. Strayers, S. Aavang, S. Ishman, and L. Krissek, Holocene sedimentation rates on the southern Chileancontinentalmargin,AntarcticJournal, in press, 1996.
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© 1997 Chapman & Hall
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Stravers, J.A., Anderson, J.B. (1997). A Late Glacial Readvance Moraine in the Central Chilean Fjords. In: Davies, T.A., et al. Glaciated Continental Margins. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-5820-6_35
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DOI: https://doi.org/10.1007/978-94-011-5820-6_35
Publisher Name: Springer, Dordrecht
Print ISBN: 978-0-412-79340-0
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