The fault scarp created a waterfall in the transition region between the Denali fault and the Totschunda fault.
Images
Earthquake Hazards Program images.
The fault scarp created a waterfall in the transition region between the Denali fault and the Totschunda fault.
View southward toward Mt. McGinnis and two large landslides on the northeastern side. These slides had roughly 40 million cubic meters of material and travelled 10 km down glacier. This is the cover photo of the May 16th, 2003, Science.
View southward toward Mt. McGinnis and two large landslides on the northeastern side. These slides had roughly 40 million cubic meters of material and travelled 10 km down glacier. This is the cover photo of the May 16th, 2003, Science.
Peter Haeussler prepares to measure the offset of a crevasse on the Canwell Glacier.
Peter Haeussler prepares to measure the offset of a crevasse on the Canwell Glacier.
The fault scarp created a waterfall in the transition region between the Denali fault and the Totschunda fault.
The fault scarp created a waterfall in the transition region between the Denali fault and the Totschunda fault.
Bone Creek, 5.5 meter offset measured here. The fault trace runs along the sharp bank edge at the right of the photo, from the bottom center toward the upper right.
Bone Creek, 5.5 meter offset measured here. The fault trace runs along the sharp bank edge at the right of the photo, from the bottom center toward the upper right.
Denali fault near headwaters of Chistochina River, view to the south. Dark blur at top of photo is rotor blade.
Denali fault near headwaters of Chistochina River, view to the south. Dark blur at top of photo is rotor blade.
View westward up Black Rapids Glacier at large landslides.
View westward up Black Rapids Glacier at large landslides.
View north of Denali fault trace at Gillette Pass. this view shows that the surface rupture reoccupies the previous fault scarp. Also the right-lateral offset of these stream gullies has developed since deglaciation in the last 10,000 years or so.
View north of Denali fault trace at Gillette Pass. this view shows that the surface rupture reoccupies the previous fault scarp. Also the right-lateral offset of these stream gullies has developed since deglaciation in the last 10,000 years or so.
View west over pass between Canwell and Chistochina Glaciers. Two fault traces here may indicate the glacier ice is influencing the fault trace.
View west over pass between Canwell and Chistochina Glaciers. Two fault traces here may indicate the glacier ice is influencing the fault trace.
View of Denali fault trace in Chistochina River valley.
View of Denali fault trace in Chistochina River valley.
View westward up Black Rapids Glacier at large landslides.
View westward up Black Rapids Glacier at large landslides.
Denali fault crossing stream near headwaters of Chistochina River. Stream offset was 4.8m. Perhaps better than the previous photo.
Denali fault crossing stream near headwaters of Chistochina River. Stream offset was 4.8m. Perhaps better than the previous photo.
View westward up Black Rapids Glacier at large landslides.
View westward up Black Rapids Glacier at large landslides.
West fork of Chistochina Glacier. Denali fault trace here is parallel to the moraine, indicating that the structure of the glacier ice is influencing the surface trace of the fault.
West fork of Chistochina Glacier. Denali fault trace here is parallel to the moraine, indicating that the structure of the glacier ice is influencing the surface trace of the fault.
View down west fork of Chistochina Glacier. Denali fault can be seen crossing the glacier, Wrangell volcanoes in the distance.
View down west fork of Chistochina Glacier. Denali fault can be seen crossing the glacier, Wrangell volcanoes in the distance.
Near the southeast extent of the surface rupture of the Totschunda fault thrust faulting pushed the frozen sand and gravel over the snow surface.
Near the southeast extent of the surface rupture of the Totschunda fault thrust faulting pushed the frozen sand and gravel over the snow surface.
Fault trace in trees west of the Mentasta Road. Tallest trees are perhaps 40 feet tall.
Fault trace in trees west of the Mentasta Road. Tallest trees are perhaps 40 feet tall.
View south along Tok Cutoff Highway. Here the fault offset the road almost 7 meters.
View south along Tok Cutoff Highway. Here the fault offset the road almost 7 meters.
View southeast along the Totschunda fault.
View southeast along the Totschunda fault.
View north along Richardson Highway where it was offset by the Denali fault. Trans Alaska Pipeline is in the background.
View north along Richardson Highway where it was offset by the Denali fault. Trans Alaska Pipeline is in the background.
At pass west of Delta River. Here there was roughly 5 m of offset. Note the push up in the background. There is permafrost at the bottom of the cracks.
At pass west of Delta River. Here there was roughly 5 m of offset. Note the push up in the background. There is permafrost at the bottom of the cracks.