Images

View westward up Black Rapids Glacier at large landslides.

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.

View west over pass between Canwell and Chistochina Glaciers. Two fault traces here may indicate the glacier ice is influencing the fault trace.

Denali fault crossing stream near headwaters of Chistochina River. Stream offset was 4.8m. Perhaps better than the previous photo.

Denali fault near headwaters of Chistochina River, view to the south. Dark blur at top of photo is rotor blade.

View down west fork of Chistochina Glacier. Denali fault can be seen crossing the glacier, Wrangell volcanoes in the distance.

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.

Near the southeast extent of the surface rupture of the Totschunda fault thrust faulting pushed the frozen sand and gravel over the snow surface.

View south along Tok Cutoff Highway. Here the fault offset the road almost 7 meters.

View southeast along the Totschunda fault.

Fault trace in trees west of the Mentasta Road. Tallest trees are perhaps 40 feet tall.

View eastward along Black Rapids Glacier. The Denali fault follows the trace of the glacier. These very large rockslides went a mile across the glacier on the right side. Investigations of the headwall of the middle landslide indicate a volume at least as large as that which fell, has dropped a meter or two and is almost ready to fall.

Trace of Denali fault along north margin of Canwell Glacier.

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.

View north along Richardson Highway where it was offset by the Denali fault. Trans Alaska Pipeline is in the background.

USGS and university geologists study the walls of a trench across a recently discovered strand of the Seattle fault.

Fault surface trace of the Hector Mine fault after the October 16, 1999 M7.1 rupture. (Photo by Katherine Kendrick, U.S. Geological Survey)

The Landers fault (red lines at left) and the Hector Mine fault and its aftershocks (red lines and circles at right). The Hector Mine earthquake was a magnitude 7.1, and it produced thousands of aftershocks. 

Hector Mine surface rupture after 1999 earthquake in southern California.