Delayed Bedrock Response Beneath Ice Sheets
q As ice sheets grow, the pressure of their
weight on the underlyingion bedrock
becomes significant.
q Due to the different densities of ice and
rock, a ice sheet of 3000m thickness is
roughly equivalent to the weight of
1000m of solid rock.
q The initial sinking would be elastic and
immediate.
q The bedrock later respond more slowly
and sinks half of the remaining distance
toward the eventual equilibrium every
3000 years.
q The total time to reach the final
depression depth is about 15,000 years.