Johnson shut in state park from owasso11/22/2023 ![]() ![]() As a day trip from St Louis, MO, the drive is less than 2 hours south of St Louis in Central MO. For more information about trails in Missouri State Parks, please visit here. Johnson Shut Ins Address 148 Taum Sauk Trail, Middle Brook, MO 63656 Johnson Shut Ins State Park is located in Middle Brook, MO which is about 10 minutes north of Leasburg, MO. Where did that lead? We have no idea-nor did other visitors there know either. For quick reference, a map and trail information for each trail is available to download below. Also at the “almost dead end” of the walkway was small blue arrow pointing to a barely perceptible path over big rocks. Where did it go? We climbed it and followed it for some minutes before turning back not knowing to where it led. Where there appeared to be an almost dead end an extensive and mili-level wooden staircase took off to the right. Our only issue was the signage at that point. That was all good-beautiful and soothing scenery. From there on foot, we followed the excellent wooden boardwalk with its substantial steel railing along a trail to where the river waters are trapped to flow and cascade amongst rocks. At the end of the road is a large parking area. Pretty impressive demonstration of the power of water. At the entrance to the park are many huge boulders that were transported to their location by water-floods resulting from an upstream dam break. The park offices were closed when we visited in October, but a map on the outside of the building provided information about where to go. 2021 Ovation Awards Recipients - Northeastern State University Student. It is quite amazing and feels like you are in the mountains here. Water creates chutes and rapids and branches out among the rock field. It was fun to jump around the smoothed down the surface of the dark rock. A shallower area can be found at the front of the rapids and a deeper area can be found farther down for older kids. Judging from some mothers with kids on a pebble beach, it will be fine to take him since he could spend most of his time in the swimming holes that surround the rapids. My main objective today was scouting the area for a future trip with the kid. I wore my flip-flops, but water shoes would also work. ![]() So on my day here has the medium rapids and I can expect some tugging from the water.Įxplore this area with some kind of footwear unless you want to scrape or cut your foot on the rocky terrain. Rapids high, red flag, rapids medium, yellow flag, and the green flag is low rapids. Nearby the store there is a sign of danger. Blue sky reflected off the smooth grey rhyolite while autumn colors reflected in the pool of water below the shut-ins. Sites can accommodate tents, trailers and RVs. Fall Morning On the Black River Black River Reflections 1 This photograph was captured in the fall after the sun was well behind the steep valley hillsides. Campsites can be reserved, but there area also first-come, first-serve sites available. The campground offers basic, electric, full hookup and equestrian sites (with water & electric). Then the river hits the more resistant igneous rock and the valley becomes narrow and steep-sided or “shut in.” Along the banks of the stream look for the Ozark witch hazel which blooms in late winter and early spring.The shut-ins are the most interesting natural water slide in Missouri and the rock here is smooth so mind your step and the rapids move fast. Johnson’s Shut Ins State Park campground has 80 single-family campsites in the beautiful St. Rhyolite rock (another kind of igneous rock) is formed from magma and volcanic ash and debris flows that spewed out onto the earth’s surface and then cooled.Ībove the park the East Fork of the Black River flows through a broader valley formed in dolomite bedrock. Granite rock (a type of igneous rock) is formed from magma that cooled below the earth’s surface and then was exposed later. Igneous rock is one formed from molten rock, magma, and other volcanic materials (e.g., ash deposits). The story of Johnson’s shut-ins starts over a billion years ago when the igneous rocks here, pink granites and blue-gray rhyolites, were formed from volcanic activity.
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