Shady Dolomite is a geological formation composed of marine sedimentary rocks of early Cambrian age. It outcrops along the eastern margin of the Blue Ridge province in the southeastern United States and can be found in outcrops in the states of Alabama, Georgia, Tennessee, North Carolina, and Virginia. The Shady is predominantly composed of dolomite and limestone with lesser amounts of mudrock. It contains fossils including those of trilobites, brachiopods, and echinoderms. Shady Dolomite was first described by Arthur Keith in 1903 and was named for exposures in the Shady Valley region of Johnson County in the state of Tennessee. Near Austinville Virginia, the Shady hosts ore deposits that have been mined extensively for lead and zinc ore.
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New River Trail is a 57-mile linear park that follows an abandoned railroad right-of-way. The park parallels the scenic and historic New River for 39 miles and passes through four counties and the city of Galax. The trail's gentle slope makes it great for visitors of all ages to hike, bike and ride horseback. The park's Foster Falls area offers canoe and bike rentals; boat launches; gift shops; and a horse arena. Fishing is popular, and primitive campsites are available in designated areas. The park's Hoover Mountain Biking Area is also popular with those seeking extra adventure. There are access points to the trail at Allisonia, Chestnut Yard, Cliffview, Dannelly Park (near Galax), Draper, Dora Junction (near Pulaski), Foster Falls, Fries, Galax, Gambetta, Hiwassee and Ivanhoe. Horse trailer parking is available at Allisonia, Austinville, Cliffview, Dora Junction, Draper, Fries, Ivanhoe and the Mark E. Hufeisen Horse Complex.
This cache is located within the boundaries of New River Trail State Park and placed with permission from Park Management. Parking fees apply, day searching only, please CITO and Leave No Trace