Named Beech granite for Beech Mountain, Watauga (now Avery) Co., NC. Consists of huge masses of coarse granite, usually porphyritic and seldom fine-grained. In the porphyritic varieties, constituting bulk of formation, the feldspars make greatest part of rock, giving it a dull whitish or light-gray color. Biotite is more prominent in massive portions, and causes a distinct spotted appearance. A third variety, of considerable extent, is a coarse red granite found near border of the area. Unit cuts the Cranberry granite and Blowing Rock gneiss and is youngest massive plutonic rock in the region. It is of Precambrian age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
The Beech Mountain thrust sheet, a part of the Blue Ridge thrust complex of NC and TN, includes numerous intrusions of the Beech Suite, as unit is referred to here. Compositionally the Beech is an alkali granite. Though Rankin grouped it along with other plutonic and volcanic rocks into the Crossnore Plutonic Volcanic Complex, authors here prefer to differentiate the Bakersville, Beech, and Crossnore Suites and volcanic units as distinct subdivisions, as the entire complex is not co-magmatic.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Beech Granite has Rb-Sr whole-rock isochron age of 706 +/-6 Ma (Bryant and Reed, 1970; Odom and Fullagar, 1984).
Source: GNU records (USGS DDS-6; Reston GNULEX).
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