Candler phyllite and schist. Incidental mention.
Source: US geologic names lexicon (USGS Bull. 1200, p. 604).
Pg. 91 (fig. 1), 93. Candler formation of Evington group. Described as lustrous gray-green phyllite and fine- to coarse-grained schists. Some quartzites and greenstone volcanics(?). Garnet-, staurolite-, and chlorite-bearing facies widespread in eastern areas. Thickness ranges from 1,500 to about 4,000 feet. Underlies Joshua schist (new); also of Evington group (new) of Paleozoic(?) age. Overlies Catoctin greenstone. Type locality designated. Age is Paleozoic(?).
Type locality: Candler Mountain, 2 mi south of Lynchburg, Lynchburg quadrangle, Campbell Co., south-central VA.
Source: US geologic names lexicon (USGS Bull. 1200, p. 604).
Candler formation. Includes Esmont slate facies (new). [Age is Paleozoic(?).]
Source: US geologic names lexicon (USGS Bull. 1200, p. 604).
Pg. 14-16, pl. 1. Candler formation. Thin lenses of white quartzite and white marble and lenses of blue marble locally interbedded with phyllite. Age is Paleozoic(?).
Source: Publication; US geologic names lexicon (USGS Bull. 1200, p. 604).
Pg. 8 (fig. 2), 31-33, 48, pl. 1. Candler formation. Age shown on columnar section as early Paleozoic(?).
Source: US geologic names lexicon (USGS Bull. 1200, p. 604).
Pg. 863 (fig. 1), 864 (table 1). Candler Formation of Evington Group. Age is Early Cambrian and Cambrian(?).
Source: GNC index card files (USGS-Reston).
Pg. 100-101 (fig. 1). Candler Formation. Muscovite, chlorite and paragonite-bearing phyllite, feldspathic schist, quartzite, graywacke metamorphosed at greenschist grade. Contact with overlying Chopawamsic Formation (late Precambrian and Cambrian) gradational from more sedimentary character in west to volcanic in east. Age is late Precambrian.
Source: Publication; GNC index card files (USGS-Reston).
Candler Formation mapped as two separate lithologic units: phyllite and schist, and laminated metasiltstone. Phyllite and schist unit is described as medium- to dark-gray and greenish-gray mica phyllite and sandy laminated schist. Lenses and pods of feldspathic quartzite, metamorphosed quartzarenite, dolomitic marble, and dark-gray to medium-bluish-gray, laminated marble are common in upper part. Outcrop belt of phyllite and schists extends from the VA-NC boundary in Patrick Co., northeastward to at least the north end of Buffalo Ridge on the Amherst-Campbell Co. line. In Orange Co., the Candler includes the True Blue formation of Pavlides (1989, 1990). The laminated metasiltstone unit, found northeast of the Scottsville Mesozoic basin, is grayish-green, fine- to very fine grained, laminated schistose and phyllitic. In southeastern Albemarle Co., unit contains discontinuous interbeds of ferruginous metatuff. This unit conformably overlies the Catoctin Formation. Cambrian age shown here.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Lower Cambrian(?) Candler Formation is probably a continuation of phyllitic rocks of melange zone IV of Mine Run Complex.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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