. Annual report of the United States Geological Survey to the Secretary of the Interior . ly pene-trated approximately to the f reservoir,and are incomplete relative to the Trinityreservoirs by 900 feet of penetration. A few miles above Round Rock, in theforks of Brushy Creek, there are someshallow flowing wells about 100 feetdeep, which derive their water from theGlen Rose or t3 reservoir. Mrs. Keens shallow flowing well uponthe North Fork of the San Gabriel andthose at the junction of the branches ofBrushy Creek are shallow wells of theGlen Rose formation similar to those ofthe Lampasas Vall
. Annual report of the United States Geological Survey to the Secretary of the Interior . ly pene-trated approximately to the f reservoir,and are incomplete relative to the Trinityreservoirs by 900 feet of penetration. A few miles above Round Rock, in theforks of Brushy Creek, there are someshallow flowing wells about 100 feetdeep, which derive their water from theGlen Rose or t3 reservoir. Mrs. Keens shallow flowing well uponthe North Fork of the San Gabriel andthose at the junction of the branches ofBrushy Creek are shallow wells of theGlen Rose formation similar to those ofthe Lampasas Valley as described inLampasas County. Mr. T. Cooper reports a flowing wellabout 6 miles east of Georgetown andabout one-third the distance between thelatter town and Taylor, which is said tobe only 279 feet deep. There is notsufficient data at hand to permit any conclusions concerning this following material was penetrated: Section No. 80.—Section op well of T. Cooper, about 6 miles east of George-town, Williamson County, Texas. Thickness. Depth. Feet. 152559 Feet. 15270279 ta. n: o
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