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Fault slip, fault mapping, and age constrains along the North Olympic fault z...
We reconstruct fault slip rates since ~14 ka on the Sadie Creek fault (SCF), north of the Olympic Mountains, Washington using airborne lidar and field mapping of surficial... -
Results of Scarp Profiling on the Lake Creek-Boundary Creek Fault (Table S5_b)
a: Three profiles (tp1, tp20, tp23) originally reported by Nelson et al. (2017), were not able to be confidently measured by this study.b: Measured in meters from West to East,... -
Results of Scarp Profiling on the Sadie Creek Fault (Table S5_a)
a: Measured in meters from West to East, beginning at the SCF fault trace terminus with the West Twin River.b: Quality ranking based on quality of the lidar data and confidence... -
Summary of Strike-Slip displacement along the SCF and LCBCF (Table 1)
a: Measured in meters from West to East, beginning at the SCF terminus with the West Twin River and ending at the LCBCF terminus with Seibert Creek.b: No measurable scarp.... -
Sadie Creek Fault trace Shp (zipped, 31 KB)
This dataset has no description
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Summary of boundary element method model results (Table 4)
a:Positive values show dominantly left-lateral motion (red) and negative values show dominatly right-lateral motion (blue). Boxes are shaded in gray where kinematic sense is not... -
Radiocarbon dating results (Table 3)
a: Sample location shown in Supplemental Figures S1 and S6. -
OSL results (Table 2)
a: OSL and 14C Sample names both begin with “SCF18-”.b: Age analysis using the single-aliquot regenerative-dose procedure of Murray and Wintle (2000) on 1-2mm small-aliquots of... -
Fault planes and striation data collected by compass from the Doña Juana Volc...
The data here contained include strike and dip of the measured fault-planes, and trend and plunge of the linear kinematic indicators (i.e., fault striae, mineral fibers, steps,...