*The height of the inner edge is the elevation (m, NAVD 88) at the
sharpest inflection in slope along the base of the sea cliff backing
Terrace B.
§Estimated as the difference between the inner edge
height and sediment thickness; C = A – B
†The height of the the modern shoreline angle is the
elevation (m, NAVD 88) at the base of the slope between the modern shore
platform and Terrace A.
#Icy Point RSL change; E = D – C; see text for
explanation. Error calculated as the square-root of the sum of squared
errors of parameters A–C.
**Holocene RSL change and uncertainty reported by Mann and Streveler
(2008).