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.