Slip and strain accumulation along the Sadie Creek fault, Olympic Peninsula, Washington
Upper-plate faulting in the Olympic Peninsula of Washington State reflects the interaction of crustal blocks within the Cascadia forearc as well as contributions from various earthquake cycle processes along the Cascadia subduction zone (CSZ). These processes include interseismic coupling, megathrus...
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| Format: | Text |
| Language: | English |
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Western CEDAR
2019
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| Online Access: | https://cedar.wwu.edu/wwuet/896 https://cedar.wwu.edu/cgi/viewcontent.cgi?article=1917&context=wwuet |
| Summary: | Upper-plate faulting in the Olympic Peninsula of Washington State reflects the interaction of crustal blocks within the Cascadia forearc as well as contributions from various earthquake cycle processes along the Cascadia subduction zone (CSZ). These processes include interseismic coupling, megathrust earthquakes, and aseismic slow slip events. In this study I utilize high resolution airborne lidar, field mapping of deformed surficial deposits and landforms, optically stimulated luminescence (OSL) dating and radiocarbon dating to reconstruct fault slip rates since Late Pleistocene deglaciation on the Sadie Creek fault (SCF), located north of the Olympic Mountains. This mapping reveals the SCF as a ~14 km-long NW-striking, subvertical, dextral strike-slip fault with a subordinate dip-slip component. Field and lidar measurements of 48 scarp profiles and 11 laterally offset stream channels indicate that faulting of late Pleistocene and younger surfaces varies along strike with dextral slip ranging from 4.0–26.0 m (average of 14.3 ± 7.5 m) and dip-slip displacement ranging from 0.7–6.5 m (average of 3.4 ± 1.6 m). Reevaluation of fault slip on the adjacent Lake Creek Boundary Creek fault (LCBCF), which connects with the SCF beneath Lake Crescent, shows a slightly higher range of dextral slip (4.5–29.7 m, average of 15.9 ± 8.9 m) and lower range of dip-slip displacement (0.8–4.6 m, average of 2.3 ± 0.9 m) suggesting that slip on the SCF may be more oblique than on the LCBCF. OSL and radiocarbon ages of deposits deformed by the SCF and LCBCF suggest that channels formed throughout post-glacial time and thus record different amounts of slip depending on channel age. Therefore, channels that record the largest magnitude of slip are interpreted as the oldest channels and produce a preferred dextral slip rate of 1.3–2.3 mm/yr since retreat of the Juan de Fuca lobe of the Cordilleran ice sheet at 14 ka. Comparing this slip rate to geodetically constrained models of forearc deformation, I determine how shorter-term (decadal) ... |
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