Named as part of Fredericksburg Complex, replacing the name Berea quartz monzonite of Neuschel and others (1971); name Berea is preempted by Berea Sandstone. Named for Falls Run (upstream from typical exposures), Salem Church 7.5-min quad, Stafford Co., eastern VA. Occurs in a refolded fold that is on inverted limb of a recumbent fold. Consists of pale-pink to nearly white, coarse-grained, strongly foliated granite gneiss. Intruded by Holly Corner Gneiss of Fredericksburg Complex (both new). Age is Middle Silurian to Early Devonian based on U-Pb and Rb-Sr studies that date the unit as 415 to 385 Ma.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Falls Run Granite Gneiss mapped in southern Stafford and northern Spotsylvania Cos. Fredericksburg Complex not used. Described as pink to white, coarse-grained, strongly-foliated hornblende-biotite granite to monzonite gneiss. Dominant minerals are microcline, plagioclase quartz, biotite, muscovite, and hornblende. Accessories include apatite, epidote, titanite, and magnetite-ilmenite. Intrudes Cambrian Ta River Metamorphic Suite and Late Proterozoic and Cambrian Holly Corners Gneiss. Intruded by Mississippian and Pennsylvanian Falmouth Intrusive Suite. Has been dated at 410 Ma (U-Pb zircon and Rb-Sr whole rock, Pavlides and others, 1982). Map symbol indicates a Silurian age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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