The Burks Mt. Ultramafic Complex in the serpentinite quarry here has a protolith of olivine and orthpyroxene cut by talc-serpentine veins. The complex contains felsic rocks and amphibolies. The complex may be an ophiolite sequence. Stop 6 Dennis
References
Page 47 - Dennis, A.J., 2016, Structural analysis of the Kiokee belt and its framing elements: Savannah River transect: Geol. Soc. Am. Field Guide 42, p. 37-51.
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