Summary

Goals

  • Being able to describe the causes and effects of post-glacial rebound.
  • Being able to describe different Finnish soil types.

Summary

  • During the last Ice Age, a heavy ice mass caused the Earth's crust to sink into the planet's mantle.
  • When the ice mass retreated and melted, the planet's crust began to rise back to its original level in a process known as post-glacial rebound.
  • The Baltic Sea has experienced great changes after the last Ice Age.
  • Finnish mineral and organic soil types have been formed during and after the last ice age.
  • Key words: mineral soil types, organic soil types, post-glacial rebound, clay valleys, ancient shores, relic species.