Karst landscapes dissolve into caves as rainwater eats limestone
Karst country forms where rain picks up carbon dioxide, becomes a mild acid, and slowly dissolves limestone or dolomite — carving sinkholes, disappearing streams, and vast cave networks.
Water follows joints and bedding planes, widening them into passages that can hide rivers entirely underground. Towers, poljes, and stone forests are the surface signature of that invisible plumbing.
Stone is not permanent when chemistry has time. Karst shows Earth sculpts some of its wildest rooms by dissolving rock instead of breaking it.
Comments
0 comments