*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).