Ice-Marginal Delta Formation and Sedimentary Processes Of Kongsvegen Glacier in Kongsfjorden, Svalbard, Norway, 2006
Over the last ca. 15 years, the southeastern portion of Kongsvegen glacier has retreated back onto land and an ice-marginal delta has formed at its terminus. The delta has an annual growth rate of 6.0x105 m3 a-1, determined from bathymetric profiling and aerial photos taken inbound and outbound of N...
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Format: | Dataset |
Language: | unknown |
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Arctic Data Center
2013
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Online Access: | https://doi.org/10.18739/A2WS8HK4Z |