Karst Working Group: A Blue-Hole Spring in Orangeville Rise, Indiana
Detailed Description
A blue-hole spring, Orangeville Rise, Indiana. This spring is sixty feet in diameter.
Sources/Usage
Public Domain.
Related
Karst Aquifers: Midwest Paleozoic Carbonate Aquifers
The porosity of carbonate and dolomitic units in Midwest Paleozoic rocks has been enhanced by dissolution, and in many areas these rocks have undergone extensive karst development. This aquifer demonstrates karst features such as disappearing streams, springs, and caves.
Related
Karst Aquifers: Midwest Paleozoic Carbonate Aquifers
The porosity of carbonate and dolomitic units in Midwest Paleozoic rocks has been enhanced by dissolution, and in many areas these rocks have undergone extensive karst development. This aquifer demonstrates karst features such as disappearing streams, springs, and caves.