# spring

remarks:
The given lat/long is for the spring orifices, not the USGS gaging station.


remarks:
Water reported to flow from crevice in limestone. Formerly used to run power wheel. Temp. 70F. Well E-3 in TWC B-6208. Gaging station downstream of spring orifice.


remarks:
Water reported to flow from many solution cavities in limestone. Well E-4 in TWC B-6208.


spring_nm:
Honey Ck Spring Dws Ref Outlet nr Spring Branch,TX


spring_nm:
Honey Ck Spg at Treatment Otl nr Spring Branch, TX


remarks:
The given lat/long is for the USGS gaging station, not the individual spring orifices.


remarks:
USGS surface-water gaging station for total spring flow to surface water body.


remarks:
Field specific conductance 1530 umhos/cm in 1990.  Field conductance 3560 umhos/cm in 2001. The given lat/long is for the spring orifices, not the USGS gaging station.


remarks:
Spring X-22 in TWC Bull. 6214. Field specific conductance 1550 umhos/cm in 1990. Field specific conductance 3330 umhos/cm in 1997. The given lat/long is for the spring orifices, not the downstream USGS gaging station.


remarks:
Spring X-21 in TWC Bull. 6214. Field specific conductance 1298 umhos/cm in 1990. Field specific conductance 3420 umhos/cm in 2001. The given lat/long is for the spring orifices, not the USGS gaging station.


remarks:
Spring F-58 in TBWE Misc. Pub. 208. Spring P-108 in TBWE Misc. Pub. 209. Spring Q-216 in TBWE Bull. 6106.


remarks:
East spring of three springs which are known as San Felipe Springs.


remarks:
Spring V-7 in Texas Water Commission Bulletin 6216.


remarks:
Located on bank of San Antonio River. Runs 4-inch pipe 1/2 full.


remarks:
Located east of bath house in Southerland Springs Park.


remarks:
Located in old camp grounds east of old Sutherland Springs.


remarks:
Formerly supplied Diamond Shamrock Chemical.


remarks:
Flows from sand-clay contact.  Reported fails in drought.


remarks:
Well I-3-103 in B-5601. Located on bank of Elm Creek.


remarks:
Reported numerous seeps flow into livestock pond.


remarks:
Reported supplied 700 head of cattle from 1888 to 1907.


remarks:
Reported numerous openings in quicksand.


remarks:
Spring B-9-51 in Texas Water Commission Bulletin 6212.


remarks:
Water approximately 200 ft below surface.


remarks:
Spring B-8-27 in Texas Water Commission Bulletin 6212.


remarks:
Field specific conductance 500 umho/cm, 22 degrees C.


remarks:
Field specific conductance 450 umho/cm, 22 degrees C.


remarks:
Flows from seeps in red sandstone.  Reported altitude, 401 feet.


remarks:
Field specific conductance 450 umho/cm, 26 degrees C.


remarks:
Temperature 73 degrees F, 1950.  Well D-7-9 in TBWE B-5601.


remarks:
Plastic barrel around in the spring. Jet pump in the barrel. Pumps to a pressure tank upslope.


remarks:
Reported never to have failed. Temp 72 degrees F.


remarks:
Cement reservoir built around spring. Temp. 71 degrees F.


remarks:
Located on west bank of Seco Creek. Temp.72 degrees F.


remarks:
Reported never to have failed. Temp. 73 degrees F.


remarks:
Discharges into Geronimo Creek.  Temp 69 degrees F.


remarks:
Field specific conductance 600 umho/cm, 25 degrees C.


remarks:
Field specific conductance 550 umho/cm, 25 degrees C.


remarks:
Reported did not go dry in 1956. Earthen dam. No openings inside.


remarks:
Springs discharge into Medina River in 2 locations.


remarks:
Spring at contact between Upper and Lower Glen Rose.


remarks:
Flows from one opening in gravel and sand.


remarks:
In 1963, many seeps and probably flowed into creek below water surface.


remarks:
Spring F-12 in Texas Water Commission Bulletin 6210.  Numerous openings.


remarks:
Spring H-6 in Texas Water Commission Bulletin 6210.


remarks:
Flows from crevice in limestone. Water is piped to house. Temperature 66F.


remarks:
Spring will be covered by Amistad Lake during periods when lake is above elevation 1104 feet. Temperature 23 degrees C.


remarks:
Spring will be covered by Lake Amistad during periods when lake is above elevation 1120 feet. Temperature 24 degrees C.


remarks:
Spring with concrete rings to 8 ft. to form catch basin.


remarks:
Field specific conductance 3000 umho/cm, 21 degrees C.


remarks:
Spring in creek bed near San Marcos River.


remarks:
Flows from a crevice in limestone. Used to cool rock house.


remarks:
Water stands in pit near ground level.  Formerly supplied plantation headquarters.


remarks:
Flows from a crevice in limestone. Supplies water for summer camp.


remarks:
Several springs in bed and banks of Boggy Creek.


remarks:
Well P-33 in TWC B-6208. Seeps from limestone.


remarks:
Flows from limestone. Temperature 66F. Reported never goes dry.


remarks:
Spring in bank of Clear Fork Creek. Curbed and pumped to elevated tank.


remarks:
Well P-23 in TWC B-6208. Spring reported to flow from crevices in limestone.


remarks:
Flows from mouth of cave. Temperature 66F.


remarks:
Flows from a crevice in limestone. Reported goes dry in droughts. Temperature 67F.


remarks:
Flows from 3 openings in limestone. Temperature 65F.


remarks:
Flows from crevice in limestone. Hydraulic ram pumps water to house.


remarks:
Field specific conductance 950 umho/cm, 25 degrees C.


remarks:
Flows from crevice in limestone. Temperature 65F.


remarks:
Temperature 23 degrees C, September 16, 1966.


remarks:
Well P-30 in TWC B-6208. Water flows from base of Edwards limestone. Temp. 74F.


remarks:
Well P-26 in TWC B-6208. Flows from solution cavities in bedding plane of limestone. Temp. 70F, 1955.


remarks:
Flows from crevice in limestone. Temperature 63F.


remarks:
Several springs developed on edge of creek behind concrete wall. Many other springs along creek make head waters of Frio River.


remarks:
Field specific conductance 500 umho/cm, 19 degrees C.


remarks:
Well P-19 in TWC B-6208. Flows from crevice in limestone.


remarks:
Well M-20 in TWC B-6208.  Flows from fracture in limestone.


remarks:
Field specific conductance 470 umho/cm, 19 degrees C.


remarks:
Well P-18 in TWC B-6208. Flows form crevices near base of Edwards limestone. Temp. 70F, 1955.


remarks:
Flows from sand and gravel. Temperature 66F.


remarks:
Well P-11 in TWC B-6208. Water reported to flow from crevice in limestone. Temp. 70 F.


remarks:
Springs in creek bed; field specific conductance 900 umho/cm, 22 degrees C.


remarks:
Lower springs along Boundary Creek; field specific conductance 1100 umho/cm, 22 degrees C.


remarks:
Well P-10 in TWC B-6208. Water reported to flow from crevice in limestone.


remarks:
Upper springs along Boundary Creek; field specific conductance 1000 umho/cm, 22 degrees C.


remarks:
Field specific conductance 600 umho/cm, 27 degrees C.


remarks:
Well P-9 in TWC B-6208. Water reported to flow from crevices near base of Edwards limestone. Temp. 68F, 1939.


remarks:
Well P-7 in TWC B-6208. Flows from solution cavities in bedding plane near base of Edwards limestone. Temp. 70F, 1955.


remarks:
Well J-44 in TWC B-6208. Reported to flow from crevices in limestone.


remarks:
Field specific conductance 900 umho/cm, 24 degrees C.


remarks:
Spring is near head of perennial flow on Devil River. Temperature 22 degrees F.


remarks:
Well J-46 in TWC B-6208. Headwaters of East Fork of Nueces River. Flow from many solution cavities in limestone bed of creek.  Temp. 70F.


remarks:
Well H-41 in TWC B-6208. Rock Spring formerly flowed, but has been dry for several years. Spring for which the city of Rocksprings was named.


remarks:
Spring D-69 in TBWE Bulletin 6004 and 5608.


remarks:
Field specific conductance 880 umho/cm, 24 degrees C.


remarks:
Field specific conductance 600 umho/cm, 28 degrees C.


remarks:
Field specific conductance 485 umhos/cm in 1994.


remarks:
25x100-foot seepage area in creek bed; field specific conductance 940 umho/cm, 27 degrees C.


remarks:
Field specific conductance 900 umho/cm, 23 degrees C.


remarks:
Spring is dammed and piped 2 miles to houses.


remarks:
Seepage area 100 ft in diameter; field specific conductance 1500 umho/cm, 26 degrees C.


remarks:
Along 1/3 mile reach of canyon; field specific conductance 800 umho/cm, 21 degrees C.


remarks:
Seepage area 300 feet long along creek; field specific conductance 800 umho/cm, 21 degrees C.


remarks:
Reported spring dry during 1947-56 drought.  Temp. 21 degrees C.


remarks:
Field specific conductance 850 umho/cm, 22 degrees C.


remarks:
Dug out and brick lined, used from well reservoir.  In used since about 1884, as auxiliary public supply source.  Reported to flow continously. Measured temp. 21 degrees C.


remarks:
Flows from a large opening in clay on hillside. Never fails.


remarks:
Field specific conductance 550 umho/cm, 22 degrees C.


remarks:
Spring B-44 in Texas Board of Water Engineers Bulletin 6004.


remarks:
5 springs in immediate area; field specific conductance 450 umho/cm, 23 degrees C.


remarks:
An aggregate of many seeps in Capote Canyon.


remarks:
Field specific conductance 400 umho/cm, 24 degrees C.


remarks:
On Indian Creek, .5m W of Harper/Kerrville Rd. Never fails. Flow varies with seasons. Flows from limestone.


remarks:
Well (spring) E-11 in TWC B-6208. Spring in South Lano River. Water flows from two openings in bedding plane of limestone. Temp. 68F.


remarks:
Springflow not visable. Tank water backs up over spring. Reported has never gone dry.


remarks:
Water flows from solution cavity in bedding plane at contact of limestone and marl. Well E-9 in TWC B-6208.


remarks:
Dry from 1952 to 1955. Water flows from limestone bluff 20 ft. above bed of South Llano River. A small spring flows about 10 ft. below Deats Spring. Temp. 70F. Well E-10 in TWC B-6208.


remarks:
Water flows from crevices in limestone. Temp. 70F. Well E-5 in TWC B-6208.


remarks:
Dug out spring; once supplied steam driven gin; in use from about 1840 to 1940.


remarks:
5 springs, of which only 2 are now above the level of Town Lake.


remarks:
Intermittent spring from base of limestone at contact with shale.


remarks:
Located on the Mount Bonnell Fault.  It is now largerly beneath Lake Austin.


remarks:
Flows from limestone. Fails in summer. Temperature 60F.


remarks:
At least 25 springs issue from the Mount Bonnell Fault just below the normal level of Lake Austin.


remarks:
About 25 springs.  They are now nearly all inundated by Lake Austin.


remarks:
One mile west of Yarborough. Spring at contact between sand and clay in road ditch.


remarks:
Two miles east of Stoneham. Spring at contact between sand and clay in road ditch.


remarks:
Flows from 1 opening in base of gray limestone on hillside. Temperature 60F.


remarks:
Well D-116 in 1957 Travis County report.


remarks:
Reported strong supply.  Temp. 68 degrees F.


remarks:
Flow decreases each spring season if rain is not plentiful.


remarks:
Reported 3500 ft of pipeline from spring to house.


remarks:
Formerly supplied 2 families and Oak Grove School.  Well D-8 in 1957 Travis County report.


remarks:
Never fails. Strong after rains. Water reported from limestone. Temperature 60F.


remarks:
Flows from 2 openings in fractured rock. Never fails. Temperature 65F.


remarks:
Spring is used to water stock and garden.


remarks:
Spring in conglomerate with several openings.  Another small spring at house. Well A-28 in 1957 Travis County report.


remarks:
Flows from opening in sand on east slope of hill. Box curb.


remarks:
Flows from 3 openings in white sand. Improved with wood box and 3-inch tile.


remarks:
Headquarters supplied by 1.4 miles of 2-in. pipe line from spring.


remarks:
Formerly supplied water for cotton gin and sawmill boilers on hillside 120 feet below hill.


remarks:
Wood curb. Flows from 3 openings in white sand.


remarks:
Flows from numerous openings in white sand.


remarks:
Supplies water for 10 families.  Dug out to increase flow.  On Chinquapin Creek.  Temp. 72 degrees F.


remarks:
Flows from numerous openings in fine white sand. Improved with 1 joint 30-inch vitrified tile. Reported stronger flow in rainy weather.


remarks:
In bed of Navasota River.  Has H2S odor.


remarks:
Strong flow from numerous openings in yellow shaly sand.


remarks:
Supplies Coldspring. Cypress lined pit 8 x 5 feet and 30 feet deep.


remarks:
Flows from opening in hard, fine, brownish-white sand. Numerous springs in this locality.


remarks:
Three spings provide auxiliary water for Coldspring.  Temp. 68 degrees F.


remarks:
Flows from numerous openings in  sand. Reported heavier flow in rainy seasons.


remarks:
Flows from numerous openings in white sand. Reported heavier flow in rainy seasons.


remarks:
Flows from several openings in fine white sand. Stronger flow reported in rainy seasons.


remarks:
Seepy area west of Ash Spring about 40 ft in diameter.


remarks:
Flows from numerous openings in sandstone and iron ore gravel. Reported stronger flow in rainy weather.


remarks:
Forms small pool at mouth of spring. Spring flow is from the base of rocky creek bed.


remarks:
Reported not to be affected by rainfall.


remarks:
Flows from 1opening in sandstone. Gas bubbles at intervals.


remarks:
Flows from white sand. Reported never fails in drought.


remarks:
Flows from numerous openings in white sand. Improved with vitrified tile. Reported never fails in drought.


remarks:
Flows from several openings in mottled light-brown sand. Stronger flow reported in rainy weather.


remarks:
Reported weakens when dry.  Temp. 66 degrees F.


remarks:
Improved with 1 joint of tile. Strong supply.


remarks:
Reported dependable supply since 1860 from several openings in sandstone at base of limestone


remarks:
Flows from numerous openings in brown sand, veined with lignite.


remarks:
Flows from seeps from sandstone. Supplies grammar school swimming pool.


remarks:
Only perennial stream in Davis Mountains. Feeds T & P Lake. Field water quality parameters: ph = 7.26, Conductivity = 351, and temperature = 21.4 degrees C. in 2001.


remarks:
Field specific conductance 102 umhos/cm in 1990.


remarks:
Supplies water for Bold Spring Public School and store.


remarks:
Well No. 50-14-RBL in Bureau Economic Geology report.


remarks:
Field specific conductance 215 umhos/cm in 1990.


remarks:
Flows from 2 openings in loose sand at contact with schist.


remarks:
Spring emerges from 3 places on limestone shelf in creek bed.


remarks:
Flows from many seeps in sandstone blocks.  Temperature 68º F.


remarks:
Flows from seeps in sandstone.  Temperature 72º F.


remarks:
Flows from limestone conglomerate.  Temperature 51º F.


remarks:
Flows from seeps in limestone.  Temperature 56º F.


remarks:
Spring P-107 in TBWE Misc. Pub. 209. Spring B-66 in TBWE Misc. Pub. 208. Spring G-28 in TBWE Bull. 6106.


remarks:
Lower spring below obs. platf. Poss ib.DY4 in UT study (Boghici, 1997).


remarks:
Flows from sand.  Reported not to have failed in 57 years.


remarks:
Flows from openings in bottom of pool.  Irrigates garden.  Temperature 67º F.


remarks:
Flows from seeps in gravel.  Temperature 70º F.


remarks:
Flows from seeps in limestone.  Temperature 52º F.


remarks:
Spring T-15 in TWC Bull. 6214.  Reported to have irrigated 85 acres in 1945 and 30 acres in 1958.


remarks:
Flows from many seeps in limestone. Temperature 71º F.


remarks:
Flows from one opening in limestone.  Temperature 68º F.


remarks:
Slight flow from seeps along joint in limestone.


remarks:
Flows from many openings in limestone.  Reported seldom goes dry.  Temperature 69º F.


remarks:
Spring is in large downthrown faultblock or graben.


remarks:
Flows from 5 openings in limestone.  Temperature 71º F.


remarks:
Flows from 3 openings in limestone.  Temperature 71º F.


remarks:
Flow out of pool occurs about 20 % of year.


remarks:
Flows from one crevice in travertine.  Temperature 69º F.


remarks:
Flows from 1 opening in light, brown sand.


remarks:
Spring is in large downthrown fault block or graben.


remarks:
Flows from one opening in limestone.  Temperature 69º F.


remarks:
Flows from several opening in limestone.  Temperature 67ºF.


remarks:
Flows from sand.  Reported never to have failed.


remarks:
Flows from seeps in limestone.  Temperature 55ºF.


remarks:
Sampling point behind house where two springs come together.


remarks:
Flows from six openings in limestone.  Temperature 66ºF.


remarks:
Flows from openings in gray sand. Temperature 64 F.


remarks:
Water from seepage in alluvium above shale.  Irrigates small garden.


remarks:
Flows from two openings in limestone.  Temperature 71º F.


remarks:
Spring is in small upthrown fault block.


remarks:
Flows from seeps in limestone.  Temperature 71º F.


remarks:
Flows from many openings in conglomerate.  Temperature 66º F.


remarks:
Flows from 1 opening in fine, gray sand.


remarks:
Flows from many seeps in coarse sand end gravel.  Temperature 72º F.


remarks:
Flows from one opening in sand.  Temperature 69ºF.


remarks:
Flows from 1 opening in light gray sand.


remarks:
Seeps from conglomerate.  Temperature 71º F.


remarks:
Flows from several openings in alternating layers of clay, lignite, sand and iron rock. Small deposits of salts on sides of bluff.


remarks:
Flows from seepage in conglomerate.  Temperature 72º F.


remarks:
Flows from 1 opening at clay-sand contact. Located on side of old railroad cut.


remarks:
Temperature 66 F. Located on side of road near bed of creek.


remarks:
Flows from gravel in creek bed and bank.  Reported weak supply.  Temperature 68ºF.


remarks:
Flows from sandstone and clay.  Temperature 69º F.


remarks:
Flows from 1 opening on limestone.  Reported flow affected by pumping of well 365.


remarks:
Flows from concealed openings in gravel.  Located on bank of Colorado River.


remarks:
Reported small flow in 1964. Temp.  65 degrees F.


remarks:
Flows from sandstone.  Sight fluctuation.


remarks:
Flows from one opening in white water sand.


remarks:
Wood box curb.  Flows from one opening in quicksand.


remarks:
No curb; barrel casing.  Reported limited capacity in present condition.


remarks:
Temperature 70 degrees F, Sept. 24, 1970.


remarks:
Reported that it has flowed continuously for 50 years. (1961)


remarks:
Water reported flowing from joints and solution channels in limestone.


remarks:
Reported dry only once in last 65 years.


remarks:
Water from nodular, whitish-gray limestone.  Reported spring fails during periods of extreme drought.


remarks:
Series of seeps. Water from thinbedded, gray limestone.


remarks:
Wood curb.  Flows from two openings in white sand.


remarks:
Wood curb.  Water reported from quicksand.  Nearly fails in drought.


remarks:
Supplies Camp Tonkawa. Temperature 65 degress F. Still flowing 10-5-88.


remarks:
Deussen (1914) reported large flow. Temp. 13.8 degrees C. on 7-14-81.


remarks:
Spring in draw, 100 yards north of South mill.


remarks:
In wall of canyon.  Supplies 1,200 sheep.


remarks:
Flows from fissures in limestone.  Reported flow increases immediately after rains.


remarks:
In wall of canyon.  Supplies 300 to 500 sheep.


remarks:
In wall of canyon.  Supplies several hundred sheep.


remarks:
Flows from joints in limestone.  Reported weak supply.


remarks:
Reported weak supply.  Stone curb; wood cover.


remarks:
Windmill pumps from spring.  Reported has not failed in 36 years.


remarks:
Flows from concealed openings in gravel.


remarks:
In bed of creek.  Supplies several hundred head of stock.


remarks:
Flows from concealed openings in sand.  Stone curb.


remarks:
Reported yield, 4 to 5 barrels a day from fissures in limestone.  Reported failed in 1918.  Reported flow increases after rains.


remarks:
Flows from wooden barrel set in sandstone overlying buff colored shale.  Never fails.


remarks:
Concrete curb set in sand.  Never fails.


remarks:
Water level lowers in summer.  Wood set in sand.


remarks:
Flows from sandstone.  Reported never fails.


remarks:
Constant supply of 10 gallons a minute for past 50 years.  Water from sandstone above shale.


remarks:
Flows from sand and gravel overlaying shale.


remarks:
Concrete curb.  Flows from 1 opening in limestone.


remarks:
Flows from limestone along the right bank just below the Glen Rose-Cleburne Bridge over Wheeler Branch. Flows about 1 foot above channel at 71 F.


remarks:
Water from barrel in sand above hard rock.


remarks:
Flows from sandstone at contact with shale.


remarks:
Flows from sandstone underlain by shale.


remarks:
Stops flowing in summer but never fails.


remarks:
Deepened to 10 feet in 1975 by owner. Concrete box with 4 inch Alum casing through which pump installed. Contact of Antlers and Moran Formation.


remarks:
Reported first known failure occurred in July, 1940.


remarks:
Dug out for tank, shallow water table encountered.


remarks:
At south side of lake. Water highly mineralized.


remarks:
Developed spring; reported spring has stopped flowing.  Temp. 76 degrees F.


remarks:
OFR 82-1 Site No. SE-40. Small spring or seep (ground water inflow) into Lake 1 at western shore.


remarks:
OFR 82-1 Site No. SE-19. Small seep or spring into Lake 7 at northwest shore.


remarks:
Original tank was dug near the turn of the century.


remarks:
Seep in bottom of new excavation for stock pond.


remarks:
OFR 82-1 Site No. NE-16. Small spring or seep into Lake 9 at east shore in 1977.


remarks:
Flows from crevices in massive limestone.


remarks:
Formerly used as a domestic supply and springhouse. Partial rock walls of the springhouse still standing.


remarks:
Temperature 66 degrees F. Water flows from several openings along creek.


remarks:
Several springs and seeps along bluff. Used since first settlement of county.


remarks:
Owner reports flow varies with rainfall, but has never stopped completely.


remarks:
Spring No.8. Contact of red beds (Permian?) just below on either side of canyon.


remarks:
Very slow seep. Flows into creek about 20 yards north of spring.


remarks:
Springs at junction of Spring Creek with Duthcman Creek.


remarks:
Springs in Long's Branch of Ballard Creek.


remarks:
Springs and wells inundated when dam was constructed.


remarks:
Field specific conductance 800 on 1-27-38.


remarks:
Flows northward from approximately the base of the Seymour Formation.


remarks:
Several small springs and seeps along contact of Permian Artesia Group and Quaternary Alluvium.


remarks:
Water seeps from well-cemented coarse gravel and friable sand.


remarks:
Spring in North Fork of South Pole Creek.


remarks:
Numerous seeps.  Reported no flow in summer.  Field specific conductance 21000 micromhos, Feb. 25,1969.  Reported salty water.


remarks:
Water issues from 20-feet deep sinkhole.  Field specific conductance 3400 micromhos.


remarks:
Spring issues from sinkhole.  Field specific conductance 4000 micromhos.


remarks:
Many seeps.  Field specific conductance 3,100 micromhos.


remarks:
Line of seeps. Field conductance 3,000 micromhos, Apr. 21, 1969.


remarks:
Field specific conductance 800 micromhos, Mar. 21, 1969.


remarks:
Water from seep flows to shallow pond. Field specific conductance 2000 micromhos, June 11, 1969.


remarks:
Field specific conductance 45,000 micromhos.  Reported winter yield 100 gpm.


remarks:
Numerous seeps, water reported gypy. Field specific conductance 3900 micromhos Jan. 16,1969.


remarks:
Line of seeps, water flows into stock pond.  Field specific conductance 850 micromhos.


remarks:
Many seeps form recreational pond, held by earthern dam.  Field specific conductance 1,800 micromhos.


remarks:
Line of seeps.  Water impounded by earthen dam. Field specific conductance 1,400 micromhos, Feb. 28, 1969.


remarks:
Water reported too salty for stock use.  Spring issues from small sinkhole.  Field specific conductance 26000 micromhos, Jan.17,1969.


remarks:
Line of seeps, water flows into small pond.  Field specific conductance more than 40,000 micromhos, Jan.22,1969.


remarks:
Springs issues from cavern in flood plain.  Flow contained with dam constructed by Corps of Engineers, 1964.  Conductance 750.


remarks:
Spring issues from mud-filled sinkhole.  Field specific conductance 55000 micromhos, Oct.29,1968.


remarks:
Spring issues from mud-filled sinkhole.  Field specific conductance 42500 micromhos, Oct. 29,1968.


remarks:
Issuing between Ogallala and red beds. Line of seeps.


remarks:
Line of seeps.  Water gyp. field specific conductance 2,600 micromhos, July 30, 1969.


remarks:
Water unsuitable for stock.  Flow is intermittent.  Field specific conductance 12,500 micromhos.


remarks:
Field specific conductance 3,700 micromhos.


remarks:
Formerly flowed fresh water.  No flow since 1965.


remarks:
Field specific conductance 2900 micromhos, Jan.23, 1969.  Flow decreases in summer.


remarks:
Field specific conductance 3800 micromhos, Jan 8,1969.


remarks:
Field specific conductance 800 micromhos.


remarks:
Flows into Buch Creek at Collingsworth-Childress county line. Most of water goes as underflow into alluvium


remarks:
Flows into Dry Salt or Cousins Creek. Field specific conductance of 4200, July 14, 1967.


remarks:
Hole 8 ft. deep. Flow decreases in summer.


remarks:
Seepage pond, partial source is probably from well 12-12-908.


remarks:
Spring supplies 200 acre-foot reservoir on West Salt or Cousin's Creek.


remarks:
Field specific conductance 220 micromhos on Mar.5,1968.


remarks:
Field specific conductance 350 micromhos, 3-5-68.


remarks:
Developed in 1938.  Completed by concrete pipe.


remarks:
Field specific conductance 825 micromhos, Jan.5,1968.


remarks:
Field specific conductance 680 micromhos, Mar.5,1968.


remarks:
Field specific conductance 400 micromhos, Jan.5,1968.


remarks:
Field specific conductance 280 micromhos, Mar.5,1968.


remarks:
Spring developed in concrete within wooden spring house. Used as pool. Field specific conductance 500 micromhos, March 5, 1968.


remarks:
Field specific conductance 1650 micromhos, Mar 5,1968.


remarks:
Field specific conductance 300 micromhos, Dec.19,1967.


remarks:
Field specific conductance 380 micromhos, Dec.19,1967.


remarks:
Water temperature 49 degrees F on Dec.19,1967.


remarks:
Spring at Hay Camp Headquarters. Field specific conductance of 850, Sept. 9, 1967.


remarks:
Spring flows from between two formations. Top bed is coarse sand and gravel; bottom is hard clay.


remarks:
Field specific conductance 550 micromhos, Mar.19, 1968.


remarks:
Flow is lost to channel alluvium within 3 to 4 miles downstream.


remarks:
Summer flow is totally absorbed by evapotranspiration and channel fill.


remarks:
Field specific conductance of 600, May 23, 1967.


remarks:
Field specific conductance 450 micromhos, Dec.29,1967. Spring developed in 1918.


remarks:
Field specific conductance 500 micromhos, temperature 45 degree F, Dec.29, 1967. Spring developed as seep in 1914.


remarks:
Field specific conductance 300 micromhos, Dec. 29,1967.  Spring developed in 1919 and watered 125 steers that year.


remarks:
Field specific conductance 400 micromhos, 1-4-68.


remarks:
Reported springs began in 1941-42, and have since increased in flow.


remarks:
Field specific conductance 625 micromhos, 1-4-68.


remarks:
Flows into McCormick Creek. Field specific conductance of 2900, July 21, 1967.


remarks:
Flows into Hinton Creek.  Field specific conductance of 2200, September 21, 1967.


remarks:
Flows into Big Sandy Creek. Field specific conductance of 3200, April 26, 1967.


remarks:
Flows into Dozier Creek. Field specific conductance of 1200, April 6, 1967.


remarks:
Field specific conductance of 2550, April 20, 1967.


remarks:
Outflow from cave in South Fork of Corral Creek.


remarks:
Flows into unnamed tributary to Elm Creek.


remarks:
Field specific conductance of 850, March 21, 1967.


remarks:
Field specific conductance of 2500, March 21, 1967.


remarks:
Elm Creek base flow.  Field specific conductance of 2350, August 3, 1967.


remarks:
Field specific conductance 490 micromhos in 1968.


remarks:
Field specific conductance of 750, April 18, 1967.


remarks:
Reported perennial supply. Field specific conductance of 1000, July 26, 1967.


remarks:
Field specific conductance 600 micromhos in 1968.


remarks:
Field specific conductance of 650 in 1968.


remarks:
Field specific conductance of 600 in 1968.


remarks:
Reported water in cavernous gypsum beds.


remarks:
Field conductance of 2400, August 31, 1967.


# spring_disc

remarks:
Flow may include surface water upstream of spring orifice.


remarks:
Digital data acquired from Capitol Environmental Services.


remarks:
Includes 2.67 cfs pumpage by city of San Saba.


remarks:
Flow of West Springs only.  No flow in East Springs.


remarks:
Total flow of San Pedro, Cold, and Cedar Springs.


remarks:
Flow in wasteway canal below reservoir into which springs discharge. Includes both springs.  No flow in Pecan Creek above springs.


remarks:
Flow of West Springs only.  Estimated flow of East Springs 0.002 cfs.


remarks:
Springflow measured by International Boundary and Water Commission.


remarks:
From formula for 90 degree V-notch weir.


remarks:
Includes 1.34 cfs pumpage by city of San Saba.


remarks:
Springflow estimated by International Boundary and Water Commission.


remarks:
Springflow estimated by International Boundary and Water Commission. Swimming pool empty.


remarks:
Decrease of 0.74 cfs from tributary which enters 2.0 miles upstream.


remarks:
Springflow measured by International Boundary and Water Commission.  City pumping 500 gpm not included.


remarks:
Includes 2.2 cfs pumpage by city of San Saba.


remarks:
City pumping 500 gpm and highway contractor pumping 200 gpm not included.


remarks:
Springflow measured by International Boundary and Water Commission. City pumping 600 gpm not included.


remarks:
Springflow measured by International Boundary and Water Commission. City pumping 500 gpm and Fort Guest Ranch pumping 500 gpm not included.


remarks:
Includes 2.45 cfs pumpage by city of San Saba.


remarks:
Springflow measured by International Boundary and Water Commission.  City pumping 500 gpm and Fort Clark Guest Ranch pumping 800 gpm not included.


remarks:
Springflow measured by International Boundary and Water Commission.  City pumping 700 gpm and Fort Clark Guest Ranch pumping 800 gpm not included.


remarks:
No flow in Golf Course Creek and Purgatory Creek.


remarks:
500 feet below source (mouth of cave), near Toyahvale, TX.


remarks:
Field estimate.  Control gate below springs closed forming pool with about 10-foot head on springs, retarding flow.


remarks:
Includes 1.8 cfs from deep sulphur artesian well; 1.5 miles southeast of Leon Springs.


remarks:
New concrete lined canal from mouth of springs now eliminates seepage losses to Phantom Lake.


remarks:
Small flow in river channel to right of springs.


remarks:
Barton Creek dry above springs.  Includes flow of Old Mill Spring.


remarks:
Old Mill Spring not flowing.  Barton Creek dry above springs.


remarks:
Main canal 0.25 miles below diversion dam; at Fort Stockton, TX.


remarks:
Measurement made using rod suspension for meter.  All measurements of Comal Springs made prior to this used cable suspension for meter, and discharges are about 4 per cent too high.  Measurements following use rod suspension.  Total flow of springs.


remarks:
Spring openings and channels being cleaned.  Main canal 0.25 miles below diversion dam; at Fort Stockton, TX.


remarks:
Spring water backed up over spring openings by growth in creek channel.  Main canal 0.25 miles below diversion dam, at Fort Stockton, TX.


remarks:
Main canal 0.25 miles below diversion dam; at Fort Stockton, TX.  Total flow of springs.


remarks:
Has not flowed since oil well completed in 1953.


remarks:
Probably affected by pumping from nearby irrigation well.


remarks:
Measurement made soon after rainfall.  The record does not state whether all discharge is from the springs or includes storm water.


remarks:
700 ft below outlet; near Balmorhea, TX.


remarks:
Measured in channel of Barton Creek, below springs.  There was no flow in creek above springs.


remarks:
See both http://waterdata.usgs.gov/nwis/inventory/?site_no=08104290 and http://waterdata.usgs.gov/nwis/inventory/?site_no=08104310; spring flow is the difference between the two at a given point in time


# spring_nm_alt

spring_nm_alt:
USIBW Pinto Spgs at Belcher Rh nr Brackettville,TX


spring_nm_alt:
Smith State Pk in Guadalupe Mtn NP nr Salt Flat,TX


spring_nm_alt:
Boot Spring at Big Bend National Park, TX


spring_nm_alt:
USIBW Mud Springs at Mays Rh nr Brackettville, TX


spring_nm_alt:
Mud Springs at Mays Ranch nr Brackettville, TX


spring_nm_alt:
Dove Creek Spring near Knickerbocker, TX


spring_nm_alt:
Seven Hundred Springs near Telegraph, TX


spring_nm_alt:
Roaring Springs near Roaring Springs, TX


spring_nm_alt:
San Pedro Springs near Fort Stockton, TX


