freetimecrawler
Debunking old stereotypes
This is the place to put our Mn crawling locations, all listed in 1 spot for easy reference.
Please post location, and terrain, and any pic's if possible.
Also feel free to post any prospective locations, that need scouting.
Prospective: Going to scout this Spring.
Banning St Park I-35 about 2 hours North of the TC metro.
Sounds promising "thumbsup"
Geology
The Kettle River extends the entire length of the park, exposing bedrock for much of the distance. One of the most dominant characteristics of the park is sandstone and the potholes formed by the Kettle River. The sandstone is from the Hinckley formation, known for shallow soil over bedrock and boulders which are exposed or lie just below the surface. In the northern area of the park, the river flows through a relatively shallow and narrow valley. Within a few miles, the river valley narrows to a gorge worn by the river through Precambrian sandstone to a depth of 100 feet. At Hell's Gate, the river flows through sheer cliffs which rise to 40 feet above the water. Below the rapids, the valley once again begins to widen. Beyond the valley walls, the topography is generally level to gently rolling glacial till plain.
Please post location, and terrain, and any pic's if possible.
Also feel free to post any prospective locations, that need scouting.
Prospective: Going to scout this Spring.
Banning St Park I-35 about 2 hours North of the TC metro.
Sounds promising "thumbsup"
Geology
The Kettle River extends the entire length of the park, exposing bedrock for much of the distance. One of the most dominant characteristics of the park is sandstone and the potholes formed by the Kettle River. The sandstone is from the Hinckley formation, known for shallow soil over bedrock and boulders which are exposed or lie just below the surface. In the northern area of the park, the river flows through a relatively shallow and narrow valley. Within a few miles, the river valley narrows to a gorge worn by the river through Precambrian sandstone to a depth of 100 feet. At Hell's Gate, the river flows through sheer cliffs which rise to 40 feet above the water. Below the rapids, the valley once again begins to widen. Beyond the valley walls, the topography is generally level to gently rolling glacial till plain.