2 edition of Geology of the Villamont and Montvale quadrangles, Virginia found in the catalog.
Geology of the Villamont and Montvale quadrangles, Virginia
William S. Henika
by Commonwealth of Virginia, Dept. of Conservation and Economic Development, Division of Mineral Resources in Charlottesville, Va
Written in English
|Statement||William S. Henika.|
|Series||Virginia Division of Mineral Resources publication ;, 35|
|Contributions||Virginia. Division of Mineral Resources.|
|LC Classifications||QE174.B43 H46 1981|
|The Physical Object|
|Pagination||18 p. :|
|Number of Pages||18|
|LC Control Number||82622994|
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W.S. Henika, 6 x 9-inch soft cover book, 18 pages, one plate includes folded x inch color ,scale geologic map, three figures, four tables, Text describes the geologic structure and stratigraphy of the Villamont and Montvale minute quadrangles (portions of.
Additional Physical Format: Online version: Henika, William S. Geology of the Villamont and Montvale quadrangles, Virginia. Charlottesville, Va.: Commonwealth of Virginia, Dept. of Conservation and Economic Development, Division of Mineral Resources, Publication Geology of the Roanoke and Stewartsville Quadrangles, Virginia ; Publication Geology of the Villamont and Montvale Quadrangles, Virginia ; Publication Virginia clay material resources ; Publication Valley and Ridge stratigraphic correlations, Virginia.
Soil survey of Botetourt County, Virginia Roy L. Vick Not In Library. Geology of the Villamont and Montvale quadrangles, Virginia William S. Henika Not In Library. Botetourt Co., Va., will book A,1 book Stephen D. Vassar, 1 book Anne Lowry Worrell, 1 book Conrad Riffle, 1 book.
___,Geology of the Roanoke and Stewartsville Quadrangles, Virginia: Virginia Division of Mineral Resources, Publicat 23 p. Google Scholar ___, a, Geologic Map and Mineral Resources Summary of the Baldwin Gap Quadrangle, North Carolina and Tennessee: North Carolina Division of Mineral Resources, GM NWand MRS NW, 5 by: 2.
The southern Appalachian part of the Cambrian–Ordovician passive margin succession of the great American carbonate bank extends from the Lower Cambrian to the lower Middle Ordovician, is as much as km ( mi) thick, and has long-term subsidence rates exceeding 5 cm (2 in.)/k.y.
Subsiding depocenters separated by arches controlled sediment thickness. Cambrian – Lower Middle Ordovician Passive Carbonate Margin, Southern Appalachians the Mascot Dolomite, begins near or at the ba se of the A.
deltatus – O. costatu s Zone and ranges to at.