Additional information about Lake Huron sinkholes
The Lake Huron Sinkholes Overview
El Cajon Sinkhole
Middle Island Sinkhole
Isolated Sinkhole
Glossary of terms and concepts
The Lake Huron Sinkholes
This map shows the locations of three sinkholes scientists are studying in northern Lake Huron. The gray area is Michigan and the color gradient represents lake depth. Sinkholes and caves are karst formations created when mildly acidic rain and groundwater dissolve calcium carbonate in the limestone, carving tunnels and holes into the rock. The sinkholes in Lake Huron were most likely formed thousands of years ago, before the formation of the Great Lakes but after glaciers retreated. When the Pleistocene glaciers retreated 10,000 years ago, they scraped the landscape clean of any older karst formations. As a result, karst formations in the Great Lakes region formed between 10,000 and 8,000 years ago when low lake levels exposed the limestone bedrock. The sinkholes in Lake Huron range in diameter from a tabletop to a football field. They lie both near the shoreline and in the deeper waters.