Harpoon

David Tanner
LIAG Institute for Applied Geophysics, Hannover, Germany

This harpoon structure is caused by inversion of normal fault movement on this listric fault in unconsolidated glacial sands. Trowel is 12cm long.

Credit

David Tanner (distributed via imaggeo.egu.eu)

Statistics

47
Views
52
Likes
1
Stars

Share

Comments

No comments yet. Be the first to share your thoughts.