PagfrTABLE 10. Gaging stations in the Comal County area, Texas_________ 11. Runoff of the Guadalupe River.________-______'___________ 12. Discharge of the Guadalupe River near Spring Branch and at New Braunfels and pickup between stations; rainfall at Fischer Store and New Braunfels, Tex., 1928-50-.-_.___ 13. Discharge measurements, Hueco Springs, 3 miles north of New Braunfels, Tex_.._____________________________ 14. Discharge measurements to determine seepage on the Guadalupe River from Comfort, Tex., to New Braunfels, Tex., in January 1928____________-________-_---__---_--____ 15. Discharge measurements to determine seepage on the Guadalupe River from Comfort, Tex., to New Braunfels, Tex., in February 1929____________-___-___-__----_--__---_-_ 16. Discharge measurements to determine seepage on the Guadalupe River from Spring Branch, Tex., to New Braunfels, Tex., in August 1944__________________________________ 17. Average monthly and annual discharge, in second-feet, of Comal Springs at New Braunfels, Tex___________________ 18. Rainfall and runoff, Comal County, Tex., 1946-50__________ 19. Partial analyses of water from wells and springs in Comal County, Tex_____________________________ Travis Peak formation._____________________________ Glen Rose limestone (lower member)__________________ Glen Rose limestone (upper member
States and Mexico, at gaging stations maintained by that agency on the Devils River near Del Rio and the Pecos River near Comstock. The outstanding nature of the flood in the lower Pecos River is shown by the fact that the maximum stage reached at the Comstock gaging station was 97.8 ft on June 27, 1954, whereas the maximum stage reached at this gage between the beginning of record in 1900 a .. d 1954 vas only 38.2 ft.
Introduction._ ____________________________________________________ 2 Location and extent of the area_________________________________ 2 Economic development_________________________________________ 3 Precipitation._________________________________________________ Acknowledgments-____________________________________________ General principles of the occurrence and movement of ground water. _ __ _ Geologic formations and their water-bearing properties.________________ Miocene and Pliocene series___________________________________ Oakville sandstone and Lagarto clay.________________________ Willis sand (and Goliad sand?)______________________________ Pleistocene and Recent series. __________________________________ 11 Lissie formation ___________________________________________ Beaumont clay____________________________________________ 11 Alluvial deposits_________________________________________ Present development of water supplies from wells______________________ Northwestern part of the county, Cleveland-Hightower area________ Northeastern part of the county, Romayor-Rayburn area___________ 13 Southwestern part of the county, Dayton area____________________ 14 South-central part of the county, Liberty, Moss Bluff, Ray wood, and Daisetta areas_________-__^_____________-____________________ 15 Southeastern part of the county, Devers area. ____________________ 16 Estimated withdrawal of ground water.______________________________ 17 Temperature of ground water.______________________________________
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.
hi@scite.ai
10624 S. Eastern Ave., Ste. A-614
Henderson, NV 89052, USA
Copyright © 2024 scite LLC. All rights reserved.
Made with 💙 for researchers
Part of the Research Solutions Family.