GISP2-D Borehole Geometry

Inclination and azimuth was meas. 1993, 1994, 1995 using Univy of Copenhagens geophysical logging system (UCPH), described by Gundestrup et al., (1994). Continued measurements will reveal the rate at which the ice is deforming as a function of depth in the ice sheet; ice deformation measurements are...

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Bibliographic Details
Main Author: Clow, Gary D
Format: Dataset
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 2003
Subjects:
DEPTH, ice/snow
North component
West component
Inclination
Azimuth
-
Drilling/drill rig
GISP
Sampling/drilling ice
Greenland Ice Core Projects GRIP/GISP/NGRIP
Greenland
Greenland ice core
GRIP
ice core
Ice Sheet
NGRIP
Online Access:https://dx.doi.org/10.1594/pangaea.88917
https://doi.pangaea.de/10.1594/PANGAEA.88917
Description
Summary:Inclination and azimuth was meas. 1993, 1994, 1995 using Univy of Copenhagens geophysical logging system (UCPH), described by Gundestrup et al., (1994). Continued measurements will reveal the rate at which the ice is deforming as a function of depth in the ice sheet; ice deformation measurements are needed to constrain ice dynamics models developed for the GISP2 and GRIP sites. Given the slow deformation rates at GISP2, these measurements will need to be continued through at least 1999. Depth is true vertical depth

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