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Kyanite, Sillimanite, and Andalusite Deposits of the Southeastern ...

Kyanite, Sillimanite, and Andalusite Deposits of the Southeastern ...

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ANDALUSITE DEPOSITS 109<br />

cut at Brasstown Church contains about 4 percent<br />

sillimanite (Furcron <strong>and</strong> Teague, 1945). The o<strong>the</strong>r<br />

sillimanite locality is in <strong>the</strong> area <strong>of</strong> massive kyanite<br />

deposits near Old Johnstown, Dawson County,<br />

where small flattened pebblelike masses <strong>of</strong> finegrained<br />

fibrous sillimanite <strong>and</strong> quartz occur in coarse<br />

biotite gneiss; <strong>the</strong> sillimanite content <strong>of</strong> one <strong>of</strong><br />

<strong>the</strong>se small lenses was determined by microscopic<br />

examination to be about 25 percent (Furcron <strong>and</strong><br />

Teague, 1945).<br />

ALABAMA<br />

<strong>Sillimanite</strong> schist was found in R<strong>and</strong>olph <strong>and</strong> Clay<br />

Counties, Ala., by W. T. McDaniel, Jr., <strong>of</strong> <strong>the</strong> Tennessee<br />

Valley Authority, in 1944, according to<br />

Teague (1950); <strong>the</strong> extent <strong>and</strong> quality <strong>of</strong> <strong>the</strong>se deposits<br />

have not been investigated.<br />

ANDALUSITE DEPOSITS<br />

VIRGINIA<br />

<strong>Andalusite</strong> has been found in Fairfax County by<br />

Charles Milton (written communication, 1953), <strong>of</strong><br />

<strong>the</strong> Geological Survey. It occurs with quartz in<br />

quartz-mica schist at <strong>the</strong> edge <strong>of</strong> bodies <strong>of</strong> greenstone;<br />

usually <strong>the</strong> <strong>and</strong>alusite is completely sericitized.<br />

<strong>Andalusite</strong>, kyanite, <strong>and</strong> coarse muscovite<br />

occur in quartz in <strong>and</strong>alusite schist near Difficult<br />

Run, about 1.6 miles north-northwest <strong>of</strong> Oakton.<br />

<strong>Andalusite</strong> schist is also found in <strong>the</strong> old railroad<br />

cut just south <strong>of</strong> Virginia Highway 211, about 1*4<br />

miles east <strong>of</strong> Sisson. <strong>Andalusite</strong> is reported to<br />

occur with kyanite <strong>and</strong> corundum on a knob <strong>of</strong> Bull<br />

Mountain near Stuart in Patrick County (Genth,<br />

1890); we were not able to find this locality.<br />

NOKTH CAROLINA<br />

<strong>Andalusite</strong> occurs in mica schist <strong>and</strong> in sillimanite<br />

quartzite in <strong>the</strong> Kings Mountain district, <strong>and</strong><br />

is present in some abundance in several <strong>of</strong> <strong>the</strong><br />

North Carolina pyrophyllite deposits; it was first<br />

recorded from <strong>the</strong> Gerhardt (Staley) pyrophyllite<br />

mine by Burgess (1936). The pyrophyllite deposits<br />

are lenticular bodies that seem to have been formed<br />

by hydro<strong>the</strong>rmal replacement in silicified zones in<br />

silicic volcanic rocks (Stuckey, 1928). The deposits<br />

all occur in <strong>the</strong> Piedmont belt <strong>of</strong> volcanic<br />

rocks <strong>and</strong> slates (pi. 1). The occurrence <strong>of</strong> <strong>and</strong>alusite<br />

<strong>and</strong> lesser amounts <strong>of</strong> o<strong>the</strong>r high-alumina minerals<br />

(diaspore, topaz, <strong>and</strong> kyanite) in some <strong>of</strong><br />

<strong>the</strong>se pyrophyllite deposits has been described by<br />

Broadhurst <strong>and</strong> Councill (1953). They point out<br />

that in some deposits <strong>the</strong> footwall is nearly pure<br />

quartz rock <strong>and</strong> <strong>the</strong> hanging wall is sericite schist.<br />

The deposits were examined briefly by us, but not<br />

mapped, following <strong>the</strong> discovery <strong>of</strong> <strong>and</strong>alusite by<br />

<strong>the</strong> North Carolina State geologists. The descriptions<br />

given below are taken mainly from our own<br />

field observations <strong>and</strong> petrographic studies.<br />

BOWLINGS MOUNTAIN, GRANVIIXE COUNTY<br />

A pyrophyllite deposit about 1,000 feet long<br />

trends N. 15° E. along <strong>the</strong> ridge <strong>of</strong> Bowlings Mountain,<br />

about 3 miles northwest <strong>of</strong> Stem. Massive <strong>and</strong><br />

crystalline pyrophyllite occur in very fine grained<br />

siliceous zones in sericite schist. Tough white<br />

granular rock containing coarse-grained <strong>and</strong>alusite,<br />

quartz, <strong>and</strong> pyrophyllite is present in parts <strong>of</strong> <strong>the</strong><br />

deposit (fig. 17). Light-gray to tan dense chertlike<br />

topaz, identical in appearance with <strong>the</strong> dense<br />

topaz from <strong>the</strong> Brewer deposit, South Carolina, is<br />

abundant as float to <strong>the</strong> east <strong>of</strong> <strong>the</strong> nor<strong>the</strong>rn end <strong>of</strong><br />

<strong>the</strong> deposit, <strong>and</strong> also occurs as stringers a few<br />

inches thick in pyrophyllite in <strong>the</strong> sou<strong>the</strong>rnmost<br />

opencut. The deposit was prospected by a shallow<br />

opencut shortly before <strong>the</strong> time <strong>of</strong> <strong>the</strong> pyrophyllite<br />

investigation by Stuckey (1928, p. 57); it was <strong>the</strong>n<br />

known as <strong>the</strong> Harris prospect. The Carolina Pyrophyllite<br />

Co. began work here about 1949 or 1950.<br />

The rock is being mined from 2 opencuts <strong>and</strong><br />

trucked to <strong>the</strong> grinding plant at Staley, about 80<br />

miles to <strong>the</strong> southwest.<br />

Ano<strong>the</strong>r deposit <strong>of</strong> pyrophyllite occurs on a prominent<br />

ridge rising nearly 200 feet above <strong>the</strong> surrounding<br />

countryside, about 14 miles nor<strong>the</strong>ast <strong>of</strong><br />

<strong>the</strong> Bowlings Mountain deposit, 9 miles northwest<br />

<strong>of</strong> Oxford, <strong>and</strong> about IVa miles east <strong>of</strong> North Carolina<br />

Highway 96. Float <strong>and</strong> low outcrops <strong>of</strong> dense<br />

siliceous rock are abundant for about three-quarters<br />

<strong>of</strong> a mile along <strong>the</strong> ridge. Chloritoid occurs in<br />

some rock; disseminated hematite <strong>and</strong> magnetite<br />

are also present. Blocks <strong>of</strong> massive pyrophyllite, 1<br />

to 2 feet long, are distributed along a distance <strong>of</strong><br />

600 to 700 feet at <strong>the</strong> north end <strong>of</strong> <strong>the</strong> ridge. O<strong>the</strong>r<br />

aluminous minerals have not been discovered.<br />

HILLSBORO, ORANGE COUNTY<br />

A deposit <strong>of</strong> pyrophyllite on a prominent ridge<br />

just south <strong>of</strong> <strong>the</strong> town <strong>of</strong> Hillsboro, Orange County,<br />

was prospected by <strong>the</strong> North State Pyrophyllite<br />

Co. in <strong>the</strong> fall <strong>of</strong> 1952. Opencut mining was started<br />

here a few years later. The <strong>and</strong>alusite-pyrophyllitequartz<br />

ore is shipped to <strong>the</strong> company's plant at<br />

Pomona, N.C. (near Greensboro), where it is<br />

blended with o<strong>the</strong>r materials <strong>and</strong> used to manufacture<br />

firebrick <strong>and</strong> brickkiln furniture.<br />

A body <strong>of</strong> <strong>and</strong>alusite-pyrophyllite-quartz rock<br />

over 1,200 feet long <strong>and</strong> 50 to 150 feet wide has been

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