Trimble Knob
| Trimble Knob | |
|---|---|
 Photo of Trimble Knob, taken December 2011 | |
| Highest point | |
| Coordinates | 38°24′17″N 79°35′16″W / 38.40472°N 79.58778°W |
| Geography | |
| Location | Southwest of Monterey, Virginia |
| Geology | |
| Age of rock | 35.0 ± 0.5 Ma |
| Mountain type | Eroded volcano or diatreme |
| Last eruption | 35 Ma |
Trimble Knob, located southwest of Monterey in Highland County, Virginia, is a conical hill composed of basalt, a volcanic rock, of Eocene (early Tertiary) age. It is the eroded remnant of what was an active volcano or diatreme that last erupted approximately 35 million years ago, making it one of the youngest volcanos on the east coast of North America.[1]
Description
Trimble Knob is an isolated conical hill in an otherwise relatively flat valley, surrounded by farmland. U.S. Route 220 lies along the southeast flank of the hill. Trimble Knob is the most obvious of many igneous intrusions in the area.
The central part of the hill is composed of basalt with a diameter of approximately 150 metres (160 yd). The basalt intrudes through the gently dipping Devonian Needmore Formation (fossiliferous shale and calcareous mudstone), and is near the axis of a syncline in the center of the valley.[2]
Age
The basalt at Trimble Knob (and other igneous dikes in the area) was originally thought to be of Paleozoic age by relative age dating using cross-cutting relationships.[1] In 1993, Southworth and others give a date of 35.0 ± 0.5 Ma for basalt of Trimble Knob, placing it in the Eocene.[3] The basalt intrudes the Devonian Millboro Shale.
Mole Hill, located in Rockingham County, is geologically similar to Trimble Knob and thought to be contemporaneous with it, along with other intrusive igneous rocks near Ugly Mountain in Pendleton County, West Virginia.[1]
References
- 1 2 3 Jonathan L. Tso; Ronald R. McDowell; Katharine Lee Avary; David L. Matchen & Gerald P. Wilkes (2004). "Middle Eocene Igneous Rocks in the Valley and Ridge of Virginia and West Virginia". Circular 1264. United States Geological Survey.
- ↑ Rader, E.K. and Wilkes, G.P., 2001, Geologic map of the Virginia portion of the Staunton 30 X 60 minute quadrangle: Virginia Division of Mineral Resources, Publication 163, scale 1:100000.
- ↑ Southworth, C.S., Gray, K.J., and Sutter, J.F., 1993, Middle Eocene intrusive igneous rocks of the central Appalachian Valley and Ridge province; Setting, chemistry, and implications for crustal structure: U.S. Geological Survey Bulletin 1839, p. J1–J24.
Coordinates: 38°24′17″N 79°35′16″W / 38.40472°N 79.58778°W