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Unit 3: Introduction to
Fault Scarp Analysis
UNAVCO
Scarp morphology
Modified from Wallace, 1977
Types of scarps
Modified from Stewart and Hancock, 1990
Types of scarps
Modified from Stewart and Hancock, 1990
Scarp morphological evolution
Modified from Stewart and Hancock, 1990
Example scarps
USGS, Chris Crosby
Hebgen Lake (1959) Wasatch Fault (~1985)
El Mayor-Cucapah (2010)
Profile extraction
Chris Crosby
Example profile
Indiana University Geologic Field Station
Rupture length – maximum displacement
Modified from Wells and Coppersmith, 1994
Rupture length – magnitude
Relationship between displacement length and earthquake magnitude M = Magnitude L = Length
All rupture types M = 5.08+1.16*log(L)
Strike slip rupture M = 5.16+1.12*log(L)
Reverse or thrust rupture M = 5.00+1.22*log(L)
Normal rupture M = 4.86+1.32*log(L)
• Variables: fault scarp eroded material height, m (H) erosion rate, m/yr (ER) Recurrence interval, yr (RI)
• H / ER = RI• Use many estimated erosion rates to find
a recurrence interval that seems representative
Recurrence interval
• Variables: dx: spacing between measurements dt: time between each calculation step k: transport rate of sediment
• Israel: 0.1 m2/ka• Basin and Range: 1 m2/ka• California/Michigan: 10 m2/ka
• Use the given spreadsheet, variables above, and your profile to model hillslope diffusion.
Hillslope diffusion
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