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