Shenandoah River Stream Study Field Trip
This is the bridge to Deer Rapids in the Posy Hollow section of Shenandoah County. It’s called a low water bridge because you can only use it during low water. There’s a reason why they have foot markers on the signs and the river does rise that high. During flood stage, folks park on the other side and use the footbridge to get home. It’s either that, or be “Rivered In.” Yes, people live here. Go across the bridge and count the mailboxes. You may do a stream study of any site. There are many in the surrounding counties. If you find a low water bridge you don’t have to wade. The bridge here is wide enough for you and a car, but be careful and be ready to answer questions from the natives. Take somebody with you for help and for companionship. Good luck on keeping the kids off the swinging bridge! At the site, the Shenandoah flows at right angles to the orientation (layering) of the shale rock in stream bed, making little waterfalls (they are called riffles) where some of the rock is harder and more resistant to stream erosion. This is the Martinsburg shale of the Ordovician Period. Also make note of the natural levees along the riverbank. What’s a levee? “Drove my Chevy to the levee, but the levee was dry.” Look it up. Also make note of the terraces above the river on the other side.
Return to Field Trips Page Return to Dick's Page |