MILE 76.2, TWO MILE RUN OVERLOOK. Elevation 2,770 feet. The sketch on shows most of what you can see from here. A graded trail goes to the summit of Rocky Mount from the edge of the Drive a tenth of a mile north of the overlook (Hike HS-3). Diagonally left is Rocky Mountain, with white quartzite cliffs. The sketch shows only the ridge that runs down from it into One Mile Run. Geology: Looking straight out from the overlook to the far end of Two Mile Ridge, you can see two tiers of cliffs - white quartzite of the Erwin formation. The cliffs rise up from the left, level out, and then curve down to the right - evidence of the deep folding of the earth's crust that occurred when these mountains were formed. The cliffs are somewhat easier to see in winter, when the trees are bare.
MILE 76.9, BROWN MOUNTAIN OVERLOOK. Elevation 2,844. Hikes. A long overlook with a large island and a wide view framed by trees. The sketch shows the view from the south end of the overlook - across Big Run to the Rockytop ridge. Rocky Mountain (shown in part at the right-hand edge of the sketch) has two humps, and cliffs and talus of white Erwin quartzite. Farther right is the high point on Two Mile Ridge. Still farther right, and higher, is Rocky Mount. You can't see Brown Mountain from the overlook; it's hidden behind the left-hand end of Rocky Mountain.
Geology: The rocks exposed in the roadcut across the Drive are of the Hampton formation: a coarse-grained quartzite (medium salt-and-pepper gray in a fresh break) and sandstone (finer grained, uniform light gray in a fresh break).
Two hikes that start here are described. First, hike to the top of the talus slope that you can see over there on Rocky Mountain, and return by the same route, Hike HS-4. Second, a rather strenuous circuit hike returning via Big Run Portal Rocky Mountain Run Trails, Hike HS-5. |
CAUTION: Access to lower Big Run valley from the park boundary is NOT an option. Private land along the old Big Run Fire Road is heavily posted "no trespassing." Start your hikes into the Big Run area from Skyline Drive or Madison Run Fire Road which can be accessed on SR 659. See Map MS-5 or PATC Map 11, Shenandoah National Park, South District. MILE 77.5, IVY CREEK OVERLOOK. Elevation 2,890 feet. AT access. Hikes. A pleasant view, framed by trees. Toward the right, outside the sketch, is the northeast summit of Loft Mountain. Farther right is the south summit, with evergreens on its slope.
The AT passes through the overlook, coming in at one end and going out the other. Distances on the AT: north (to the left as you face the view) it's 1.6 miles to Pinefield Gap, mile 75.3; south (to the right) it's 4.9 miles to the Loft Mountain Campstore. Two hikes that start here are described. |
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MILE 78.1, ROCKYTOP OVERLOOK. Elevation 2,860 feet. The view includes a large part of the Big Run watershed. To the left, outside the sketch, the high peak on the horizon is Trayfoot Mountain. If you follow the ridge to the left from Trayfoot you'll see an area of purple-gray talus with larger rocks above it. That, collectively, is Blackrock, which has a spectacular view. You can get there easily by trail. See Hike HS-3. NOTE: According to the Geological Survey, "Rockytop" is the inconspicuous summit to the left of Lewis Peak (see sketch). But in this book, if nowhere else, Rockytop is the higher summit - conspicuously rocky on top - to the right of Lewis Peak. MILE 78.35, GEOLOGY. There's a parking area on the east side of the Drive, at the foot of a small talus slope of Hampton sandstones, some of them phyllitic (that is to say in a fresh break you can see glints or luster caused by tiny flakes of mica). Fifty yards north (uphill) on the Drive is an exposure of Hampton quartzite - medium to dark salt-and-pepper gray in a fresh break; the surface is weathered dark gray, and stained red-brown with iron. MILE 79.4, SERVICE ROAD, east side. This is the service road for Ivy Creek Trail maintenance building. It's part of the circuit Hike HS-9. Geology: You can park in the grass on either side of the Drive near the service road, or in the parking area at the Wayside to the south. From 50 to 150 yards north of the service road are coarse-grained sandstone and quartzite of the Weverton formation. The rocks on the west side have a few thin layers of phyllite, which has a lustrous sheen. Those on the east have nearly white veins of small quartz pebbles. |