Abstract
A combination of the directional surveys of the Camp Century borehole from 1966, 1967, 1969 and 1989 has revealed a deformation pattern similar to that measured at Dye-3, South Greenland and Byrd Station, Antarctica showing high deformation rate for Wisconsin ice. Compared to the Dye-3 profile, the deformation shows the same pattern even in details. The surface velocity obtained by integrating the bore hole deformation is in agreement with that obtained from satellite measurements
Udgivelsesdato: jan
Udgivelsesdato: jan
Originalsprog | Engelsk |
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Tidsskrift | Cold Regions Science and Technology |
Vol/bind | 21 |
Udgave nummer | 2 |
Sider (fra-til) | 187-193 |
ISSN | 0165-232X |
DOI | |
Status | Udgivet - 1993 |