Fig. 1
From: Isostasy – Geodesy
Airy’s model. The solid Earth topographic features are compensated by roots (t) over land and anti-roots (t′) over ocean areas. The nominal compensation depth (T 0) is set to 30 km
Fig. 1 |
From: Isostasy – Geodesy
Airy’s model. The solid Earth topographic features are compensated by roots (t) over land and anti-roots (t′) over ocean areas. The nominal compensation depth (T 0) is set to 30 km