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- W2031882322 abstract "Little North Mountain, the western boundary of the Shenandoah Valley in northern Virginia, is an overturned monocline, with steep southeast dips, bounded on the east by a thrust fault. The formations involved, Upper Ordovician to Lower Devonian, show pronounced variations in thickness, and one or more units are absent at different locations along the mountain. Such discontinuous distribution of sediments, especially the ridge-making Tuscarora sandstone, is thought to have acted as a weakened zone during deformation and determined the locus of the fault and the uplifting and overturning of the formations. Numerous water and wind gaps mark locations where the Tuscarora formation is thin or absent, and the higher altitudes correspond to a thickening of this sandstone." @default.
- W2031882322 created "2016-06-24" @default.
- W2031882322 creator A5036906158 @default.
- W2031882322 date "1940-07-01" @default.
- W2031882322 modified "2023-09-27" @default.
- W2031882322 title "Origin of Little North Mountain in Northern Virginia" @default.
- W2031882322 doi "https://doi.org/10.1086/624908" @default.
- W2031882322 hasPublicationYear "1940" @default.
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