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CAROLINA GEOLOGICAL SOCIETY<br />

<strong>Guidebook</strong> for 1995 Annual Meeting<br />

Pages 49-55<br />

GEOLOGY OF MASTERS’ KILN AND HISTORY OF THE MARBLE OCCURRENCES IN LAURENS AND<br />

UNION COUNTIES, SOUTH CAROLINA<br />

John M. Garihan, William A. Ranson, and Kenneth A. Sargent<br />

Department of Earth and Environmental Sciences<br />

Furman University<br />

Greenville, S.C.<br />

Clark A. Niewendorp<br />

South <strong>Carolina</strong> <strong>Geological</strong> Survey<br />

Columbia, S.C.<br />

INTRODUCTION<br />

M<strong>as</strong>ters’ Kiln is one of the known historic kiln sites in<br />

the piedmont of South <strong>Carolina</strong>. This guidebook article is<br />

intended to give a brief historical background of the kiln<br />

sites in Laurens and Union Counties and then a descriptive<br />

overview of the geology of the M<strong>as</strong>ters’ kiln, which concludes<br />

with a brief petrography of the skarn developed along<br />

the contact between marble and country rock. The details of<br />

the metamorphic petrology must await further study. Figure<br />

1 shows the location of the kilns, quarries, and marble locations<br />

described in this section.<br />

HISTORY OF THE LIME KILNS OF LAURENS<br />

AND UNION COUNTIES<br />

Lime w<strong>as</strong> an important commodity in the early 1800’s<br />

for use in both agriculture and the building trades. In agriculture,<br />

lime rendered “…stiff clay land more light and<br />

porous…” (Tuomey, 1844) and helped neutralize acidic<br />

soils. In the building trades, a mortar made from lime and<br />

sand w<strong>as</strong> the most frequently used until the late nineteenth<br />

century. Marble w<strong>as</strong> also quarried and used for building<br />

stones and for monuments.<br />

The first reference found by the authors appears in the<br />

1843 Report of the Commencement and Progress of the<br />

Agricultural Survey of South <strong>Carolina</strong> by Edmund Ruffin.<br />

Ruffin describes the occurrence of a “limestone” on the<br />

south fork of Raiburn’s (sic) Creek on land owned by a J.<br />

Garlington and the erection of a kiln there during 1842-1843.<br />

In Sloan (1908), this kiln is referred to <strong>as</strong> Mahaffey’s Kiln.<br />

Ruffin also reports the occurrence of a white to pale blue,<br />

crystalline marble in three outcroppings within a two mile<br />

extent stretching from the Reedy River to Walnut Creek, a<br />

major south tributary to the Reedy River. These outcroppings<br />

varied from 40 to 100 yards in outcrop extent and up to<br />

10 feet in height. The northernmost end of this trend is the<br />

M<strong>as</strong>ters’ Kiln location. According to Ruffin, the discovery<br />

of this location occurred a few years earlier when a well w<strong>as</strong><br />

dug on an adjacent ridge and “limestone” w<strong>as</strong> discovered at<br />

a depth of 64 feet. He does not mention whether a kiln w<strong>as</strong><br />

present by 1843.<br />

The 1844 Report of the <strong>Geological</strong> and Agricultural<br />

Survey of the State of South <strong>Carolina</strong> by M. Tuomey<br />

describes the occurrence of a 15 by 20 foot thick bed of limestone<br />

with a N30E strike and SE40 dip outcropping along a<br />

tributary to the Saluda River one half mile south of Ware<br />

Mill (located at Ware Shoals). This outcropping later became<br />

the location of Raysor’s Kiln but in 1844 no quarrying operations<br />

had been initiated. Tuomey also mentioned the occurrence<br />

on Reaburn’s (sic) Creek and noted that it w<strong>as</strong> being<br />

worked.<br />

The 1848 Report on the Geology of South <strong>Carolina</strong> by<br />

M. Tuomey describes the occurrence of a 15 to 20 foot thick<br />

bed of limestone between beds of gneiss outcropping along<br />

the Saluda River south of Ware Mill and along an adjacent<br />

creek. Two other occurrences located approximately two<br />

miles to the northe<strong>as</strong>t (probably those along Walnut Creek)<br />

were also mentioned. No quarrying operations were yet<br />

active at any of these locations. Tuomey describes the limestone<br />

<strong>as</strong> a “white crystalline rock… colored by streaks of<br />

chlorite, and groups of crystals of actinolite.” Tuomey<br />

describes the Reaburn’s (sic) Creek location in greater detail<br />

and includes a figure depicting the outcrop. He also discussed<br />

the kiln located there. The limestone is described <strong>as</strong> a<br />

blue limestone <strong>as</strong>sociated with soapstone and gneiss. The<br />

middle 10 feet of the bed w<strong>as</strong> composed of “good limestone”<br />

but the material above and below w<strong>as</strong> of poor quality. The<br />

kiln w<strong>as</strong> described <strong>as</strong> being “unfavorable to the quality of<br />

lime produced, and to the economy of the operation.”<br />

Tuomey also included a discourse on the burning of lime and<br />

the construction of kilns. A portion of this discussion is<br />

reproduced in Appendix A.<br />

Raysor’s Kiln commenced operations sometime during<br />

the interval between 1848 and 1860. the November 6, 1860<br />

issue of the Laurensville Herald contains an advertisement<br />

by Raysor for the best “southern made lime” from his kiln at<br />

Arnold’s Old Quarry at 30 to 34 cents a bushel depending on<br />

the number of bushels. The January 18, 1861 issue of the<br />

Herald contains a similar advertisement for lime from G. W.<br />

Sullivan’s Kiln near Popular Springs. Around 1870, Sullivan’s<br />

Kiln w<strong>as</strong> acquired by Dr. Jake M<strong>as</strong>ters and the kiln<br />

w<strong>as</strong> renamed.<br />

Additional references to these localities occur in the<br />

49

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