DS-24
Haeussler et al., 2004, Bulletin of the Seismological Society of America
A dry channel thalweg is right-laterally offset 4.8 +/- 0.5m across the Denali fault near the western margin of the Chistochina Glacier. The fault trends from the left to the upper-right of the photo. The two figures are standing in the channel thalweg as it enters the fault zone. Site DS-24, km 143.52. Photo by D. Schwartz.
A dry channel is right-laterally offset 4.8 +/- 0.5m across the Denali fault near the western margin of the Chistochina Glacier. The fault trends left to right just below the center of the photo. T. Dawson, in the foreground, is standing just left of the thalweg, and P. Montone is standing in the thalweg on the opposite side of the fault zone. Site DS-24, km 143.52. Photo by D. Schwartz.
An oblique aerial view at the Denali fault rupture near the western margin of the Chistochina Glacier. The fault trends from the bottom left toward the top right of the photo. An offset channel is visible at the photo's center. The channel thalweg is right-laterally offset 4.8 +/- 0.5m across the fault. Site DS-24, km 143.52. Photo by H. Stenner.
A dry channel is right-laterally offset 4.8 +/- 0.5m across the Denali fault near the western margin of the Chistochina Glacier. The fault trends left to right just below the center of the photo. P. Montone is standing to the right of the thalweg where it projects into the fault zone in front of her. Site DS-24, km 143.52. Photo by T. Dawson.