Danburg granite is an oval-shaped pluton that is coarsely porphyritic and occupies about 50 sq mi in the area. Apophyses of porphyritic granite cross-cut the bounding layered rocks of Little River Series. Porphyritic granite like that at Danburg has intruded granite gneisses of Kiokee Series (new) and earlier nonporphyritic granites near Appling.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Danburg described as coarse-grained and porphyritic. Similar to many other post-metamorphic granites of the southern Piedmont. Age is probably about 300 Ma.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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