Electronic Supplement to
Surface Rupture of the Kunlunshan Earthquake (Ms 8.1), Northern Tibetan Plateau, China

Photo Gallery of Surface Rupture Evidence from the
Kunlunshan Earthquake of 14 November 2001
Page 3 * (Photos 15-21)

Photo 15. The second strand from the south in Photo 13 offset a small channel 1.55 m horizontally (photo toward the south).
Photo 16. The third strand from the south in Photo 13 strikes about N76ºE and consists of a series of N76ºE-trending transtensional fractures which offset the risers and small channels about 2.3 m horizontally (photo toward the south-southeast).
Photo 17. The earthquake surface ruptures cut the glacial lobe front to form a broken zone 23 m wide at the southern piedmont of Yuzhu Feng, a snow-capped summit with an elevation of 6,178 m (photo toward the north).
Photo 18. Pre-earthquake fault scarp, which was produced by paleo-offsets, faces to the north that blocked a south-flowing stream to form a sag pond at site H, north of Hoh Sai Hu Lake. The latest surface ruptures are overprinted on this scarp, showing how a scarp has formed (photo toward the southwest).

Photo 19. Five subparallel ruptures are on the pre-earthquake fault scarp or in front of it. These ruptures are left-lateral slip with a total offset of 4 m. The small single tracklike road left by wild donkeys is offset in a left-lateral sense (photo toward the south).

Photo 20. The earthquake surface rupture zone consists of three subparallel ruptures about 12 m wide which offset the northern shoreline of Hoh Sai Hu Lake 4.7 m in a left-lateral sense (photo toward the north).
Photo 21. Ice cones occur near the surface ruptures on the northern shoreline of Hoh Sai Hu Lake, the same origin as liquefied sand cones (photo toward the south).

[Photos 1-7]  [Photos 8-14]  [Photos 15-21]