aDepth calculated by multiplying the tangent of the dip angle by the distance between the reverse fault and the Fairweather fault (~5 km) assuming planar fault geometries.
bUplift rate estimated by this study.
cFault-normal (shortening) rate calculated by dividing the uplift rate by the tangent of the dip angle.
dCoseismic uplift estimated from heights of terrace risers measured at Icy Point.
eSlip estimates calculated by dividing the range of uplift estimates by the sine of the dip angle.