2 edition of Hydrology of the Arbuckle mountains area, south-central Oklahoma found in the catalog.
Hydrology of the Arbuckle mountains area, south-central Oklahoma
Fairchild, Roy W.
|Statement||Roy W. Fairchild, Ronald L. Hanson, Robert E. Davis.|
|Series||Circular / Oklahoma Geological Survey,, 91, Circular (Oklahoma Geological Survey) ;, 91.|
|Contributions||Hanson, Ronald L. 1934-, Davis, Robert E., hydrologist., Geological Survey (U.S.), Oklahoma Geological Survey.|
|LC Classifications||QE153 .A3 no. 91|
|The Physical Object|
|Pagination||v, 112 p. :|
|Number of Pages||112|
|LC Control Number||90623700|
The Arbuckle-Simpson aquifer in the Arbuckle Mountains of south-central Oklahoma is a critical groundwater resource and the Chickasaw National Recreation Area (CHIC) contains numerous freshwater and mineral springs that discharge in the park’s Rock Creek and its principal tributary, Travertine Creek. Abstract. The Cambro-Ordovician Arbuckle Group in the Arbuckle Mountains, south-central Oklahoma, had a complex history of dolomitization that resulted in two different geometries of dolomite bodies: stratal dolomite, of stratigraphically consistent, widespread distribution, and non-stratal dolomite, of stratigraphically inconsistent, local occurrence.
TEXAS. U.S. Geological Survey, , Texas water issues in National Water Summary hydrologic events and issues: U.S. Geological Survey Water-Supply Paper , p Hydrologic Investigations Atlases. Multicolored or black and white maps on topographic or planimetric bases presenting a wide range of geohydrologic data; for both regular and irregular . The Arbuckle Mountains region falls in south-central Oklahoma in the United States. They lie in Carter, Johnston, Murray, and Pontotoc counties.
The Arbuckle Mountains are an ancient mountain range in south-central Oklahoma in the United States. The granite rocks of the Arbuckles date back to the Proterozoic Era some billion years ago which were overlain by sediments during the Paleozoic Era. The range reaches a height of 1, feet above sea level. Davis is located in scenic, south-central Oklahoma. Full of natural beauty, Davis is home to Turner Falls Park, one of the state’s tallest waterfalls, with foot falls that drop into a refreshing swimming hole. Full of wildflowers and breathtaking scenery, both Turner Falls Park and the Arbuckle Mountains are popular camping areas in the.
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Additional Physical Format: Online version: Fairchild, Roy W. (Roy William), Hydrology of the Arbuckle mountains area, south-central Oklahoma. Get this from a library. Hydrology of the Arbuckle Mountain area, south-central Oklahoma. [Roy W Fairchild; Ronald L Hanson; Robert E Davis, (Hydrologist); Oklahoma Geological Survey.; Geological Survey (U.S.)].
Regional geology of the Arbuckle Mountains, Oklahoma: Field-trip guidebook [Ham, William E] on *FREE* shipping on qualifying offers. Regional geology of the Arbuckle Mountains, Oklahoma: Field-trip guidebookAuthor: William E Ham.
The Arbuckle-Simpson Hydrology Study (Study) is a five-year, comprehensive study of the Arbuckle-Simpson aquifer and associated springs and streams in south-central Oklahoma. The Study is funded through a 50/50 state/federal cost-share agreement with the U.S.
Bureau of Reclamation (Bureau) and the Oklahoma Water Resources Board (OWRB).File Size: 2MB. Geology of the Arbuckle Mountains along Interst Carter and Murray counties, Oklahoma (Guidebook 26 / Oklahoma Geological Survey) Paperback – January 1, by Robert Oran Fay (Author) out of 5 stars 1 rating.
See all formats and editions Hide other formats and editions. Price New from Used from 5/5(1). Hydrology of the Arbuckle Mountains area, south-central Oklahoma.
Plate 1. Geologic Map and Sections of the Arbuckle Mountains. Plate 2. Potentiometric map of the Arbuckle Mountains, Oklahoma, Oklahoma Geological Survey, Circu scalePaper Good match with GMAP but stratigraphy doesn’t necessarily. The Arbuckle-Simpson Hydrology Study (Study) is a five-year, comprehensive investigation of the Arbuckle-Simpson aquifer and associated springs and streams in south-central Oklahoma.
A multidisciplinary team of researchers from various agencies and universities is File Size: 3MB. The Arbuckle-Simpson aquifer is the principal water resource for south-central Oklahoma and is designated a sole source aquifer by the U.S. Environmental Protection Agency. The geology that confines the Arbuckle-Simpson aquifer crops out over an area of about square kilometers according to the Oklahoma Water Resource Board at:File Size: 8MB.
Early to middle Paleozoic conodont biostratigraphy of the Arbuckle Mountains, southern Oklahoma (Scott M. Ritter, editor). Guidebook prepared for the Pander Society field trip held Marchpreceeding the Geological Society of America, South-Central Section, 24th annual meeting, Marchpages, 8 plates.
Guidebook The Arbuckle Mountains are an ancient mountain range in south-central Oklahoma in the United States. They lie in Murray, Carter, Pontotoc, and Johnston counties. The granite rocks of the Arbuckles date back to the Precambrian Eon some billion years ago which were overlain by rhyolites during the Cambrian Period.
The range reaches a height of 1, feet above sea : 1, sq mi (2, km²). Plate 2 for Hydrology of the Arbuckle Mountains area, south-central Oklahoma, by Roy W. Fairchild, Ronald L. Hanson, and Robert E. Davis.
pages, 29 figures, 2 plates, 20 tables. Circular 91 Plate 1. A study of the Upper Devonian-Lower Mississippian Woodford Shale was undertaken on samples at low thermal maturity from the Arbuckle Mountains, southern Oklahoma, to dientify poss. Petrology and geochemistry of MVT deposits in the Southwest Davis Zinc Field, Arbuckle Mountains, Oklahoma, USA Article (PDF Available).
Situated in the heart of south-central Oklahoma, the Arbuckle Mountains lie in Murray, Carter, Pontotoc, and Johnston counties. The name honored Gen. Mathew Arbuckle, an early commander at Fort Gibson and namesake to Fort Arbuckle, established in near the Washita River in present Murray County.
Embed Be sure to visit the Arbuckle Wilderness Center, which houses a wide array of native and exotic wildlife. The Arbuckle Mountains are also near a favorite Oklahoma attraction, Turner Falls, with its foot waterfall, Rock Castle, hiking trails, cabins and beaches.
The Arbuckle Mountains also annually hosts the Hills of Oklahoma Tour (HOOT), a cycling event. Gantt SI () Analysis of hypoxic caves in the Arbuckle Mountains of south central Oklahoma. st annual technical meeting of the Oklahoma Academy of Science (abstract) Google Scholar Halihan T, Mouri S, Puckett J () Evaluation of fracture properties of the Arbuckle-Simpson : Kevin William Blackwood.
Experience the spectacular scenic wonders of south-central Oklahoma when you stay at this 1-bed, 1-bath vacation rental cabin.
The property is located less than 1 mile from Turner Falls Park and just minutes from Davis' most popular attractions and the Arbuckle Mountains. Development and Distribution of Hypogenic Caves and Paleokarst Features in the Arbuckle Mountains of South Central Oklahoma, USA* Kevin Blackwood1, Todd Halihan2, R.L.
Hanson, and R.E. Davis,Hydrology of the Arbuckle Mountains area, south-central Oklahoma: Oklahoma Geological Survey Circu p., 2 pls., scaleMap of South Central Oklahoma. South Central Oklahoma is an amorphous region in the state of Oklahoma, perhaps encompassing 10 counties.
It is centered on the Arbuckle Mountains, an ancient, eroded range traversing some 70 miles ( km) across the region, and surrounded by rivers and lakes, notably Lake Texoma, Lake Murray and Lake of the Arbuckles. Arbuckle Mountains. likes 24 talking about this 8, were here. The Arbuckle Mountains are an ancient mountain range in south-central Oklahoma /5().
Two formations illustrate the characteristics of Pennsylva-nian conglomerates in the Arbuckle Mountains of southern Oklahoma the Vanoss Formation and the Conings Ranch Conglomerate.
The Vanoss Formation is exposed on Bromide Hill in Platt National Park which is located on the southern edge of Sulphur and is easily reached by good roads from all.The Arbuckle-Simpson aquifer lies beneath a surface area of about square miles in south-central Oklahoma, USA and is a major source of water for local use.The Arbuckle Mountains area consists of about 1, square miles in south-central Oklahoma.
These low moun - tains rise about to feet above the plains. Unusual rock formations have been created by erosion in the moun - tains. The area is used for cattle grazing. Another region of mountains, the Wichita Mountains, is found in south-File Size: 1MB.