3701 Gattis School Rd. Round Rock, TX. 78664
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caballo lake water level

Uncategorized / November 3, 2020


Mack et al. The upper McRae Formation contains fewer plant fossils and pedogenic horizons more characteristic of a dry climate (Buck and Mack, 1995). Press enter or select the go button to submit request, International Boundary and Water Commision. The original rocks prior to metamophism were basaltic to rhyolitic volcanic and shallow intrusive rocks interbedded with sandstone and shale that were likely deposited in an extensional basin. Several of the tuffs in the Bell Top Formation and the volcaniclastic sediments and tephras of the Thurman Formation originated from calderas in the Mogollon-Datil volcanic field to the west and northwest of the mountains (McIntosh et al., 1992). Copyright © 2000-2020 CampgroundReviews.com - All Rights Reserved. No Proterozoic granite clasts are found in the Rincon Valley Formation, except for those thought to be reworked from the Eocene Love Ranch Formation.
This compressional phase occurred mainly in the Paleocene to early Eocene (~55 to 45 million years ago), although there is evidence for deformation as early as late Cretaceous and as late as late Eocene. Fine-grained windblown sands appear to be more common in the upper part of the section, heralding the overall drying of the climate in New Mexico during Late Permian time. ; UPDATE November 1, 7:15 pm ET: Real-time data delivery to NWISWeb has been restored at this time. Notes: Water release schedules are updated periodically throughout the day. Floodplain mudstone and siltstone, sinuous channel sandstones, and rare carbonate lake deposits characterize the Permian Abo Formation. Discharges are in cubic feet per second and are reported at the end of the hour.

Latest Reported Water Levels . Eagle Nest Lake: Thomas Lujan, of Santa Fe, caught a 40-inch northern pike using a red Mepps pike spinner Oct. 23.Chris Serrano, of Albuquerque, caught an 18-inch rainbow trout using a Johnson Minnow spoon Oct. 23. The distribution of the McCrae Formation in the Caballo Mountains records the beginning of the third mountain building event in the Caballo Mountains, compressional Laramide deformation. Early to Middle Paleozoic sandstone, limestone, and dolomite deposited in transgressing and regressing shallow, equatorial seas rest on an erosion surface cut on the Proterozoic rocks. Page Contact Information: New Mexico Water Data Maintainer Warning: Javascript must be enabled to use all the features on this page! * We've detected you're using a mobile device. Bruno, L. and Chafetz H.S.,1988, Depositional environment of the Cable Canyon Sandstone: a mid-Ordovician sand wave complex form southern New Mexico: New Mexico Geological Society Guidebook 39, p. 127-134. Water Level (ft) Conservation Pool Elevation (ft) Height Above Conservation Pool (ft) Most recent : 2020-10-30 20:00 : 4,294.30 : 4,406.30 -112.00 below flood pool: 1 hour prior : 2020-10-30 19:00 : 4,294.29 : 4,406.30 -112.01 below flood pool: 2 hours prior The lowest part of the section is composed of sand and shale deposits indicative of rivers flowing toward the east to northeast. An acre-foot is equivalent to 325,829 gallons. McIntosh, W.C., Chapin, C.E., Ratte, J.C., Sutter, J.F., 1992b, Time-stratigraphic framework of the Eocene-Oligocene Mogollon-Datil volcanic field, southwestern New Mexico: Geological Society of America Bulletin, v. 104, p. 851-871. Choose from 170 campsites, with plenty of sites with utility hookups for RVs. Clemons, R.E., 1991, Petrography and depositional environments of the lower Ordovician El Paso Formation: New Mexico Bureau of Mines and Mineral Resources The Dakota Sandstone contains sandstone, shale, and conglomerate. (1994 a,b) note that early unroofing of the Caballo Mountains rift flank uplift, the fourth mountain building episode in the region, is recorded in the Hayner Ranch Formation (approximately 25 to 16 million years old). Next-day release schedules are usually available by 6 p.m. of the current day. We are a research and service division of: Caballo Lake State Park is located approximately 14 miles south of the town of Truth or Consequences. Seager, W.R., Clemons, R.E., Hawley, J.W., and Kelley, R.E., 1982, Geology of the northwest part of the Las Cruces 1°x 2° sheet, New Mexico: New Mexico Bureau of Mines and Mineral Resources Geologic Map 53, scale 1:125,000. Learn more window zoom in, Tap Into Campground Reviews via iOS or Android. Towards the end of Lake Valley sedimentation, the Lake Valley Formation was deposited in shallower water, signaling both a drop in sea level and tectonic tilting of the early Mississippian and older rocks toward the southeast. Framed against the Caballo Mountains, this lake boasts an array of water recreation, such as boating, kayaking, canoeing, sailing, swimming, and fishing. This unit records the unroofing of the Laramide highlands, with andestitic clasts common near the base, Abo siltstone and lower to middle Paleozoic carbonate clasts abundant in the middle part of the section, and Proterozoic clasts appearing near the top of the sequence. A northwest to north-northwest-trending Laramide basement-cored uplift is preserved in the Caballo Mountains; this uplift, which is northeast of the more extensive Rio Grande uplift exposed in San Diego Mountain and in the San Andres Mountains (Seager and Mack, 1986), shed sediments northward into a broad Laramide basin preserved as the Love Ranch Formation in the modern Jornada del Muerto Basin. Covid-19 Status:
The upper third of the Love Ranch Formation was deposited by rivers draining toward the north and northeast. If you confirm with them, please mark the status below (it will help other RVers). The dark brown Cable Canyon sandstone member, the basal unit of the Late Middle to Late Ordovician Montoya Formation, was deposited on an erosion surface cut into the top of the Early Ordovician El Paso Formation. Title: USGS Current Conditions for New Mexico The basal part of the overlying Rincon Valley Formation (about 16 to 6 million years old) is similar to the Hayner Ranch Formation in that it includes Uvas, Bell Top, Palm Park, and Love Ranch clasts. Buck B.J., and Mack, G.H., 1995, Latest Cretaceous (Maastrictian) aridity indicated by paleosols in the McRae Formation, south central New Mexico: Cretaceous Research, v. 16, p. 559-572. The combination of high temperatures and high pressures at great depth in the Earth transformed the volcanic and sedimentary rocks into metavolcanic and metasedimentary rocks. Longitude: 107.291667° W, Access our 10+ million data points plus hundreds of thousands of reviews via the free RV LIFE App. Caballo, NM 87931 Although Caballo Reservoir is shallow (maximum depth of 25 feet), it covers a large area. The basal part is sandstone, conglomerate, mudstone and siliceous volcanic ash. The Caballo Mountains began to assume their final shape starting about 25 million years ago, with the current mountain block rising about 5 million years ago along a major fault on the west side of the range. Most campgrounds are now open but the status of this campground has not been verified recently by other RVers. In the early stages of this tectonic episode, shallow seas persisted in the Caballo Mountain region until ~290 million years ago, when sea level dropped and rivers started to flow southward across the area. Caballo Dam is an earth fill dam that is 96 feet high and 4558 feet long (Figure 2). The Upper Cretaceous rocks preserve a history of the oscillating landward and seaward migration of the shoreline of the Western Interior Seaway across this area about 95 to 80 million years ago. The boating and weekend crowd on a Friday in August is missing in action. … Privacy The retreat of the sea was oscillatory, so that the contact between the Magdalena Group and the Abo Formation is gradational, with limestone interfingering with Abo redbeds. The metamorphic rocks were later intruded by 1.4(?) Lake Meredith is governed by the Canadian River Compact. Seager, W.R., Shafiqullah, M., Hawley, J.W., and Marvin, R.F., 1984, New K-Ar dates from basalts and the evolution of the southern Rio Grande rift: Geological Society of America Bulletin, v. 95, p. 87-99. The greatest storage (346,570 acre-ft.)occurred in March of 1942, when the water level was less than an inch above flood pool elevation. Mack, G.H., Seager, W.R., and Kieling, J., 1994b, Late Oligocene and Miocene faulting and sedimentation, and evolution of the southern Rio Grande rift, New Mexico: Sedimentary Geology, v. 92, p. 79-96. The andesitic debris was eroded from the Caballo Mountains and deposited as conglomerates in the latest Cretaceous McCrae Formation, which crops out on the east side of the range. Syenite of possible Cambrian age intrudes the granite (McLemore, 1986). A stomatolite bed occurs near the top of the unit (Seagar and Mack, 2003). and Giles, K.A., editors, The Geology of New Mexico: A Geologic History: New Mexico Geological Society Special Publication 11, p. 95-136.

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The States of New Mexico, Texas and Oklahoma are all parties to the compact created by agreement of the three states and the federal government in 1950. The orange sandstone is overlain by a package of dolomite, limestone, red siltstone, and gypsum interpreted to have been deposited in a hypersaline lagoon. Triassic, Jurassic, and Early to Middle Cretaceous rocks are not preserved in the Caballo Mountains because the area was on the northeastern flank of a Jurassic to middle Cretaceous rift basin (Bisbee Basin/Chihuahua trough). 2.92   1.5 vaww02. The modern landscape that we see today began to develop following regional volcanism. Kues, B.S., and Giles, K.A., 2004, The late Paleozoic Ancestral Rocky Mountains System in New Mexico, in Mack, G.H. Dolomitization has erased many of the sedimentary structures, so the depositional environment for the Fusselman Dolomite is unclear, although it is most likely shallow marine. The latest Cretaceous McRae Formation is an interesting unit that records sedimentation associated with Late Cretaceous arc volcanism and the earliest phases of Laramide deformation.

Condie, K.C., and Budding, A.J., 1979, Geology and geochemistry of Precambrian rocks, central and south-central New mexico: New Mexico Bureau of Mines and Mineral Resources Memoir 35, 58 pp. The bluish gray limestone, dolomite, and cherty limestone of the Lake Valley Formation was deposited on a south-dipping marine ramp during the transgression that began in Late Devonian time. The rivers preserved in the Crevasse Canyon Formation flowed toward the northeast. The Pennsylvanian to early Permian Magdalena Group (= Madera Group of Kues (2001)), which is divided into the Red House, Nakaye, and Bar B formations by Seager and Mack (2003), consists of fossiliferous limestone, cherty limestone, shale, dolomite, and conglomerate deposited in shallow ocean water, with sea level dropping during early Permian time (~290 to 300 million years ago). A regional drop in sea level is indicated by the stromatolite bed that was deposited near the end of Early Ordovician time. The lagoonal deposits grade up into a fossiliferous limestone, indicating a rise in sea level. We will likely return here. McLemore, V. T., 1986, Geology, geochemistry, and mineralization of syenites in the Red Hills, southern Caballo Mountains, Sierra County, New Mexico—preliminary observations: New Mexico Geological Society, Guidebook 37, p. 151–159.

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