Prospective. Going to scout this Spring.
Geology
The geological makeup of Jay Cooke State Park is one of slate, graywacke and red clay. Streams have exposed the bedrock in many places. Slate beds were formed from original deposits of mud which compacted into shale. Heat, pressure and movement converted the deeply buried shale into slate. Underground movement caused the slate and graywacke beds to fold and fracture. Later, masses of molten rock were forced through fractures in the beds and when they cooled, these intrusions formed dikes which can be seen in the river bed today.
Landscape
The rugged land formations of Jay Cooke State Park enhance the beauty of the hardwood forests. The water-eroded gorge, steep valleys, and massive rock formations are seen throughout the park. In some seasons, the water of the St. Louis River thunders over slabs of ancient, exposed rock. At other times, it slows to a gentle trickle. Visitors enjoy the scenic splendor of Jay Cooke State Park during all seasons.
780 Highway 210, Carlton, Minnesota 55718
tel: (218) 384-4610
Getting There
From the town of Carlton go 3 miles east on State Highway 210.