The purpose of this study was to compare regional patterns of indoor r
adon concentration with uranium-bearing rock zones and county populati
ons in Texas. Zones yielding radon concentrations that are relatively
high for Texas include shale and sandstone in northwest Texas; red bed
s in north-central Texas; felsic volcanic rocks in west Texas; and san
dstone, limestone, and igneous rocks in central Texas. Located in nort
hwest Texas, only five of the 202 counties evaluated have mean indoor
radon concentrations above 4.0 pCi I-1. Two of those counties have pop
ulations above the state median of 20115. The highest county mean conc
entration is 8.8 pCi I-1. Results of this study suggest that (1) regio
nal geology influences indoor radon concentrations in Texas, (2) state
wide, the radon concentrations are relatively low, (3) highly populate
d counties do not coincide with regions of high indoor radon concentra
tion, and (4) regions that may warrant further monitoring include nort
hwest Texas and, to a lesser degree, west and central Texas.