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Images
Images
Fractures crossing a wash.
Fracture running along hillside in low-relief topography with offset gullies and tracks.
Fracture running along hillside in low-relief topography with offset gullies and tracks.
Ground view along surface rupture, showing the fracturing of the soil and how pieces have been pushed up within the fault zone.
Ground view along surface rupture, showing the fracturing of the soil and how pieces have been pushed up within the fault zone.
Breaks cutting alluvium, nicely lit.
Fracture cutting across the countryside.
Fracture cutting across the countryside.
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Southeast of maximum displacement site. Here we see 3-4 meters of right-lateral slip have offset a ridge and created a 'shutter' ridge blocking flow in the dry creek channel. The white vertical surface is the fault scarp.
Southeast of maximum displacement site. Here we see 3-4 meters of right-lateral slip have offset a ridge and created a 'shutter' ridge blocking flow in the dry creek channel. The white vertical surface is the fault scarp.
View towards south across Lavic Lake, with the surface rupture running from lower right to upper left. In the middle distance on the right is an ancient lava flow.
View towards south across Lavic Lake, with the surface rupture running from lower right to upper left. In the middle distance on the right is an ancient lava flow.
Fracture cutting across the countryside (left to right) such that the fault scarp is lit up by the sun, appearing as a bold white line.
Fracture cutting across the countryside (left to right) such that the fault scarp is lit up by the sun, appearing as a bold white line.
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Splayed fractures running through loose alluvium.
Splayed fractures running through loose alluvium.
'Apparent' vertical displacement and scarps caused by mainly lateral slip.
'Apparent' vertical displacement and scarps caused by mainly lateral slip.
Downward view onto gullies, gravel bar, and other laterally offset features. Here slip appears to be about 2 meters.
Downward view onto gullies, gravel bar, and other laterally offset features. Here slip appears to be about 2 meters.
Splaying of fractures viewed from above.
Splaying of fractures viewed from above.
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