caballo lake water level

0

Mack, G.H., and Seager, W.R., 1990, Tectonic control on facies distribution of the Camp Rice and Palomas Formations (Plio-Pleistocene) in the southern Rio Grande rift: Geological Society of America Bulletin, v. 102, p. 45-53. The basal part is sandstone, conglomerate, mudstone and siliceous volcanic ash. Kues, B.S., 2001, The Pennsylvanian System in New Mexico--overview with suggestions for revision of stratigraphic nomenclature: New Mexico Geology, v. 23, p. 103-122. Access to the lake is via the boat ramp road and the lake level is very low. 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. Policies and Notices, U.S. Department of the Interior | https://waterdata.usgs.gov/nm/nwis/current? 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. United States ; New Mexico (NM) ... Any water in the desert is amazing. Although Caballo Reservoir is shallow (maximum depth of 25 feet), it covers a large area. Longitude: 107.291667° W, Caballo Dam was built to control water releases from Elephant Butte Dam. provided to the NWS by the gauge owner. Highway 187 Warning: Javascript must be enabled to use all the features on this page! Rocks older than early Mississippian in age (>340 million years old) in the Caballo Mountains were tilted toward the southeast and eroded prior to deposition of early Pennsylvanian sediments about 312 million years ago. Following Laramide deformation, sediments shed from andesite volcanoes covered the area. A small gap in the rock record caused by erosion or nondeposition occurs between the Montoya Formation and the overlying Fusselman Dolomite. The Cable Canyon member is interpreted to have been deposited as sand ridges that formed slightly offshore in a shallow sea (Bruno and Chafetz,1988), while the carbonates in the lower to middle part of the unit were deposited further offshore on a ramp covered by shallow, warm ocean water that became cooler and deeper with time (Pope, 2002). Observed water levels also are updated periodically throughout the day. This unit is famous for well-preserved fossils that include brachiopods, echinoderms, horn coral, and bryozoans. Choose from 170 campsites, with plenty of sites with utility hookups for RVs. URL: https://waterdata.usgs.gov/nwis/uv? Paleozoic to Mesozoic sedimentary rocks overlie the Proterozoic rocks and form the eastern dip slope into the Jornada del Muerto basin (Figure 1). Based on the analysis of sedimentary deposits in the southern Caballo Mountains, Doña Ana Mountains, San Diego Mountain, and Sierra de las Uvas (Figure 1), Mack et al. NOTE: Graphical forecasts are not available for the Rio Grande at Caballo Lake. 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. Volcanic rock fragments, including andesitic, dacitic, and felsic clasts, found in the Upper Cretaceous sandstones in the Caballo Mountains may have come from southern Arizona (Seager and Mack, 2003; Cumella, 1983). If you confirm with them, please mark the status below (it will help other RVers). Upchurch, G.R., Jr., and Mack, G.H., 1998, Latest Cretaceous leaf megafloras from the Jose Creek Member, McRae Formation of New Mexico: New Mexico Geological Society Guidebook 49, p. 209-222. The carbonates in the upper part of the unit have been interpreted to be hot spring deposits (Chafetz et al.,1991). Fluvial channels indicate flow toward the northeast and east-southeast. During early to middle Paleozoic time, southern New Mexico was located just south of the equator (Figure 7). Please contact the campground. 2.92   1.5 vaww02. 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. Perhaps because of the low water levels. Temperature, water, degrees Celsius Most recent instantaneous value: 18.6 10-31-2020 23:00 CDT Add up to 2 more sites and replot for "Temperature, water, degrees Celsius" Caballo Reservoir is on the Rio Grande in south-central New Mexico east of Interstate 25 between Socorro and Las Cruces (Figure 1). Basalt flows that are 2 to 4 million years old are interbedded with the sediments. The youngest units adjacent to the Caballo Mountains, the 5 to 0.78 million year old Palomas and Camp Rice Formations, unconformably overlie the Rincon Valley Formation (Mack and Seager, 1990). A stomatolite bed occurs near the top of the unit (Seagar and Mack, 2003). The Copper Flat Stock near Hillsboro (Figure 8) might be a remnant of that volcano (Seager and Mack, 2003; McMillan, 2004). McMillan, N.J., 2004, Magmatic record of Laramide subduction and the transition to Tertiary extension: Upper Cretaceous through Eocene igneous rocks in New Mexico: McMillan, N.J., and McLemore, V.T., 2004, Cambrian-Ordovician magmatism and extension in New Mexico and Colorado: New Mexico Bureau of Geology and Mineral Resources Bulletin 160, p. 1-11. 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). Cortez said water tentatively is slated to be released from Caballo Reservoir — the southernmost of the two reservoirs — on May 31. According to the compact, New Mexico can hold 200,000 acre-feet in Ute Lake before it has to release water to Texas. The lake can now hold 343,000 acre-feet of water. The uppermost carbonates in the unit were deposited in shallow water, perhaps in a lagoonal or tidal setting (Pope, 2002). We will likely return here. The campgrounds are nice and more or less secluded and peaceful. Camping, picnicing, and boating facilities are available at this state park. 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. The Abo Formation grades up into the orange windblown sheet sandstone of the Mesa Blanca Member of the Permian Yeso Formation . NOTICE November 1, 2020 7:45 am ET: We are investigating some real-time data currently behind on the web. Another gap in the rock record exists between Late Silurian and Late Devonian time. 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. The south end of the Caballo Mountains once floored one of the early, broad rift basins (Seager et al., 1984). U.S. Geological Survey *Elevations are in feet above sea level. 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. In contrast, in the middle to upper beds of the Rincon Formation, clasts of Permian Abo Formation and Pennsylvanian Magdalena Group limestones are abundant. The Caballo Mountains were located on the western margin of one of the basins, the Orogrande Basin, so tectonism in this area related to this event was relatively mild. For the latest boating conditions and ramp status, see the New Mexico State Parks website. 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. Mueller, J.E., 1986, History of Elephant Butte Dam and Reservior: New Mexico Geological Society, Guidebook 37, p. 58-59. 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. Privacy Customize table to display other current-condition parameters. Learn more window zoom in, Tap Into Campground Reviews via iOS or Android. Explore the NEW USGS National Water Dashboard; to access real-time data from over 13,500 stations nationwide. All elevation values use Rio Grande Project Datum, which is 43.3 feet less than NGVD29 and 45.5 feet less than NAVD88. The Palm Park Formation appears to represent remnants of distal volcaniclastic aprons shed off of andesitic volcanoes. 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. … The park is open daily to New Mexico residents only. Sea level came up again, leaving the black, shaly deltaic deposits of the D-Cross Tongue of the Mancos Shale.

Natascha Münter Birthdate, 90mm Handlebar Grips, Phil Promised Neverland Reddit, Aidan Holmes Instagram, Menstruation At Forty Poem Analysis, Jacob The Carpetbagger Net Worth, Indoor Skateparks Near Me, Mouse Lemur Pet, Battle For Jalibah Airfield, Gta 5 Mermaid,

Добавить комментарий

Ваш адрес email не будет опубликован. Обязательные поля помечены *