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38-516: The Ouachita Mountains ( / ˈ w ɒ ʃ ɪ t ɔː / ), simply referred to as the Ouachitas , are a mountain range in western Arkansas and southeastern Oklahoma . They are formed by a thick succession of highly deformed Paleozoic strata constituting the Ouachita Fold and Thrust Belt, one of the important orogenic belts of North America . The Ouachitas continue in the subsurface to

76-636: A few broad valleys. Logging is not nearly as intensive as in the commercial pine plantations of the less rugged Athens Plateau. Nutrient, mineral, and biochemical water quality parameter concentrations are low in the surface waters of the Fourche range, but turbidity can be higher than in other mountainous parts of the Ouachitas. Although most streams stop flowing during the driest part of the summer, enduring deep pools, high quality habitat, and good water quality allow sensitive aquatic species to survive through

114-669: A general sense, the Ouachitas are considered an anticlinorium because the oldest known rocks are located towards the center of the outcrop area. The Ouachitas continue in the subsurface to the Black Warrior Basin of Alabama and Mississippi where they plunge towards the Appalachian Mountains . To the southwest, the Ouachitas join with the Marathon area of west Texas where rocks of the Ouachita Fold and Thrust Belt are briefly exposed. Unlike many ranges in

152-627: A mix of different orogenic expressions and terranes , for example thrust sheets , uplifted blocks , fold mountains, and volcanic landforms resulting in a variety of rock types . Most geologically young mountain ranges on the Earth's land surface are associated with either the Pacific Ring of Fire or the Alpide belt . The Pacific Ring of Fire includes the Andes of South America, extends through

190-681: A series of low relief ridges, none exceeding 1,000 feet (300 m). It is located south of the Ouachitas and extends to the Arkansas-Oklahoma border. The Athens Piedmont runs from Arkadelphia, Arkansas into Oklahoma through Clark , Howard , Pike , and Sevier counties in Arkansas and McCurtain County in Oklahoma. The ecoregion's low ridges and hills are widely underlain by Mississippian Stanley Shale in contrast to other parts of

228-403: Is Rich Mountain at 2,681 feet (817 m), which intersects the Arkansas-Oklahoma border near Mena, Arkansas . The Fourche Mountains are the archetypal Ouachita Mountains. Forested ridges are heavily forested with oak–hickory–pine forest; intervening valleys are cut into shale. Ridges are longer, habitat continuity is greater, the lithologic mosaic is different, and the topographic orientation

266-633: Is Raspberry Mountain at 2,358 feet (719 m). The headwaters of multiple rivers are found in this area, including the Caddo , Cossatot , and Little Missouri rivers. The Cross Mountains are located in Polk and Sevier counties, Arkansas and McCurtain County, Oklahoma . The highest natural point is Whiskey Peak at 1,670 feet (510 m). The Crystal Mountains are located primarily in Montgomery County, Arkansas . They are so named because of

304-533: Is a rare North American species of oak in the red oak section of Quercus (known as Lobatae ). It is endemic to just four locations within the Ouachita Mountains of the State of Arkansas . The tree sometimes reaches a height of 15 meters (50 feet). The venation of the leaves shows them to be technically pinnately five-lobed but with the two middle lobes larger than the other three. This makes

342-593: Is also the highest natural point of the Ouachitas and U.S. Interior Highlands . The Frontal Ouachita Mountains are structurally quite different from the rest of the Ouachitas and are sometimes considered a separate range. The Trap Mountains are located primarily in Garland and Hot Spring counties, Arkansas . The highest natural point is Trap Mountain at 1,310 feet (400 m). The Zig Zag Mountains are located in Garland County, Arkansas , and are home to

380-538: Is at work while the mountains are being uplifted until the mountains are reduced to low hills and plains. The early Cenozoic uplift of the Rocky Mountains of Colorado provides an example. As the uplift was occurring some 10,000 feet (3,000 m) of mostly Mesozoic sedimentary strata were removed by erosion over the core of the mountain range and spread as sand and clays across the Great Plains to

418-459: Is composed of the Choctaw words ouac for "bison" and chito for "large", together meaning "country of large bison". At one time, herds of bison inhabited the lowland areas of the Ouachitas. Historian Muriel H. Wright wrote that "Ouachita" is composed of the Choctaw words owa for "hunt" and chito for "big", together meaning "big hunt far from home". According to the article Ouachita in

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456-496: Is more consistent than in other parts of the Ouachitas. Differences in moisture and temperature between north- and south-facing slopes significantly influence native plant communities; they are products of the prevailing topographic trend. Forests on steep, north-facing slopes are more mesic than on southern aspects; the steepest, south-facing slopes contain shallow, moisture deficient soils supporting shrubs and rocky glades or grassy woodlands. Pastureland and hayland are restricted to

494-670: The Encyclopedia of Oklahoma History and Culture , "Ouachita" comes from the French spelling of the Caddo word washita , meaning "good hunting grounds". The Ouachitas are a major physiographic province of Arkansas and Oklahoma and are generally grouped with the Arkansas River Valley . Together with the Ozark Plateaus , the Ouachitas form the U.S. Interior Highlands , one of few mountainous regions between

532-551: The Annamite Range . If the definition of a mountain range is stretched to include underwater mountains, then the Ocean Ridge forms the longest continuous mountain system on Earth, with a length of 65,000 kilometres (40,400 mi). The position of mountain ranges influences climate, such as rain or snow. When air masses move up and over mountains, the air cools, producing orographic precipitation (rain or snow). As

570-610: The Appalachians and Rockies . The Ouachitas are dominated by pine, oak, and hickory. The shortleaf pine ( Pinus echinata ) and post oak ( Quercus stellata ) thrive in dry, nutrient-poor soil and are common in upland areas. The maple-leaf oak ( Quercus acerifolia ) is found at only four sites worldwide, all of which are in the Ouachitas. Some native tree species, such as the eastern red-cedar ( Juniperus virginiana ), are colonizers of human-disturbed sites. The Ouachita National Forest covers approximately 1.8 million acres of

608-612: The Mithrim Montes and Doom Mons on Titan, and Tenzing Montes and Hillary Montes on Pluto. Some terrestrial planets other than Earth also exhibit rocky mountain ranges, such as Maxwell Montes on Venus taller than any on Earth and Tartarus Montes on Mars . Jupiter's moon Io has mountain ranges formed from tectonic processes including the Boösaule , Dorian, Hi'iaka and Euboea Montes . Quercus acerifolia Quercus acerifolia (also called maple-leaf oak )

646-848: The North American Cordillera , the Aleutian Range , on through Kamchatka Peninsula , Japan , Taiwan , the Philippines , Papua New Guinea , to New Zealand . The Andes is 7,000 kilometres (4,350 mi) long and is often considered the world's longest mountain system. The Alpide belt stretches 15,000 km across southern Eurasia , from Java in Maritime Southeast Asia to the Iberian Peninsula in Western Europe , including

684-759: The Ouachita National Recreation Trail , a 223-mile-long (359 km) hiking trail through the heart of the mountains. The trail runs from Talimena State Park in Oklahoma to Pinnacle Mountain State Park near Little Rock . It is a well maintained, premier trail for hikers, backpackers, and mountain bikers (for only selected parts of the trail). The Talimena Scenic Drive begins at Mena , and traverses 54 miles (87 km) of Winding Stair and Rich Mountains, long narrow east-west ridges which extend into Oklahoma. Rich Mountain reaches an elevation of 2,681 feet (817 m) in Arkansas near

722-491: The United States , the Ouachitas are mostly east-west trending. They are unique because metamorphism and volcanism , features that are common in orogenic belts, are notably absent (with the exception of some low-grade metamorphism ). Due to the high degree of folding and faulting, the Ouachitas are clustered into distinct subranges, with ridges separated by relatively broad valleys. The Ouachitas are known for some of

760-473: The Oklahoma border. The two lane winding road is similar in routing, construction, and scenery to the Blue Ridge Parkway of the Appalachian Mountains . Mountain range Mountain ranges are usually segmented by highlands or mountain passes and valleys . Individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology . They may be

798-507: The Ouachita Mountains, but have since been extirpated. Today, there are large populations of white-tailed deer , coyote , and other common temperate forest animals. Though elusive, hundreds of black bear roam the Ouachitas. Several cryptic species of salamander are endemic to the Ouachitas and have traits that vary from one locale to another. The Athens Plateau or Athens Piedmont (EPA Level IV ecoregion 36a) consists of

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836-560: The Ouachitas are as follows (in order of ascending age). The mountains were home to the Ouachita tribe , for which they were named. Later French explorers translated the name to its present spelling. The first recorded exploration was in 1541 by Hernando de Soto . Later, in 1804, President Jefferson sent William Dunbar and Dr. George Hunter to the area after the Louisiana Purchase . Hot Springs National Park became one of

874-700: The Ouachitas were deposited in a narrow, two-sided basin called the Ouachita Trough, which formed as part of a Cambrian failed rift system. Succeeding Pennsylvanian strata of the Ouachitas were deposited in a foreland basin during the early stages of the Ouachita Orogeny . Subduction of the South American Plate beneath the North American Plate resulted in this mountain-building event. Compressional forces caused

912-607: The Ouachitas. Today, pine plantations are widespread; they are far more extensive than in the more rugged parts of the Arkansas Ouachitas. Pastureland and hayland also occur. Cattle and broiler chickens are important farm products. The Caddo , Cossatot , and Missouri mountains are a high, compact group of mountains composed of the weather-resistant Arkansas Novaculite. They are located primarily in Montgomery and Polk counties, Arkansas. The highest natural point

950-1062: The Ouachitas. It is one of the largest and oldest national forests in the Southern U.S. , created through an executive order by President Theodore Roosevelt on December 18, 1907. There are six wilderness areas within the Ouachita National Forest , which are protected areas designed to minimize the impacts of human activities. Several plants are endemic to the Ouachitas, including: Agalinis nuttallii , Cardamine angustata var. ouachitana , Carex latebracteata , Galium arkansanum var. pubifolium , Houstonia ouachitana , Hydrophyllum brownei , Liatris compacta , Quercus acerifolia , Polymnia cossatotensis , Solidago ouachitensis , Spiranthes niklasii (near endemic, also found on Crowley's Ridge ), Streptanthus maculatus subsp. obtusifolius , Streptanthus squamiformis , Valerianella palmerii , and Vernonia lettermanii . Bison and elk once found habitat in

988-627: The air descends on the leeward side, it warms again (following the adiabatic lapse rate ) and is drier, having been stripped of much of its moisture. Often, a rain shadow will affect the leeward side of a range. As a consequence, large mountain ranges, such as the Andes, compartmentalize continents into distinct climate regions . Mountain ranges are constantly subjected to erosional forces which work to tear them down. The basins adjacent to an eroding mountain range are then filled with sediments that are buried and turned into sedimentary rock . Erosion

1026-505: The crust to buckle, producing complex folds at all scale levels and several overturned sequences. The area of greatest deformation occurred in the Benton-Broken Bow Uplift, which extends from Benton, Arkansas to Broken Bow, Oklahoma . The total height of the Ouachitas is not known, though they may have exceeded 10,000 feet (3,000 m) (based loosely on geologic cross-sections). The terrain has been deeply eroded since

1064-485: The east. This mass of rock was removed as the range was actively undergoing uplift. The removal of such a mass from the core of the range most likely caused further uplift as the region adjusted isostatically in response to the removed weight. Rivers are traditionally believed to be the principal cause of mountain range erosion, by cutting into bedrock and transporting sediment. Computer simulation has shown that as mountain belts change from tectonically active to inactive,

1102-594: The late Paleozoic . The Ouachitas are composed of Cambrian through Pennsylvanian sedimentary rocks . The Collier Shale, located at the core of the Benton-Broken Bow Uplift, is the oldest exposed formation of the Ouachitas. The Atoka Formation , which was deposited much later during the Pennsylvanian , has the largest areal extent of any of the Paleozoic formations in Arkansas . The geologic formations of

1140-420: The leaves appear palmately lobed at first glance, similar to many maple leaves. The epithet acerifolia means "maple-leaved." The species is threatened by habitat loss throughout its fragmented range. The four identified native subpopulations of the species are protected; these are Sugarloaf Mountains-Midland Peak Natural Area , Mount Magazine State Park , and the Ouachita National Forest . Groves of

1178-602: The nation's first parks in 1832. The Battle of Devil's Backbone was fought here at the ridge of the same name in 1863. In August 1990, the U.S. Forest Service discontinued clearcutting as the primary tool for harvesting and regenerating short leaf, pine and hardwood forests in the Ouachita National Forest. The Ouachita Mountains contain the Ouachita National Forest , Hot Springs National Park and Lake Ouachita , as well as numerous state parks and scenic byways mostly throughout Arkansas. They also contain

Ouachita Mountains - Misplaced Pages Continue

1216-689: The northeast, where they make a poorly understood connection with the Appalachians and to the southwest, where they join with the Marathon uplift area of West Texas . Together with the Ozark Plateaus , the Ouachitas form the U.S. Interior Highlands . The highest natural point is Mount Magazine at 2,753 feet (839 m). The Ouachita Mountains is a Level III ecoregion designated by the Environmental Protection Agency (EPA). The region has been subdivided into six Level IV ecoregions . Louis R. Harlan claimed that "Ouachita"

1254-566: The occurrence of some of the world's finest quartz . The Crystal Mountains are generally taller than the nearby Zig Zag Mountains, achieving elevations over 1,800 feet (550 m). The Fourche Mountains (EPA Level IV ecoregion 36d) are a long, continuous chain of east-west mountains composed of the weather-resistant Jackfork Sandstone . They extend from Pulaski County, Arkansas to Atoka County, Oklahoma and are home to several popular sites of interest, including Pinnacle Mountain State Park near Little Rock, Arkansas . The highest natural point

1292-619: The ranges of the Himalayas , Karakoram , Hindu Kush , Alborz , Caucasus , and the Alps . The Himalayas contain the highest mountains in the world, including Mount Everest , which is 8,848 metres (29,029 ft) high. Mountain ranges outside these two systems include the Arctic Cordillera , Appalachians , Great Dividing Range , East Siberians , Altais , Scandinavians , Qinling , Western Ghats , Vindhyas , Byrrangas , and

1330-627: The rate of erosion drops because there are fewer abrasive particles in the water and fewer landslides. Mountains on other planets and natural satellites of the Solar System, including the Moon , are often isolated and formed mainly by processes such as impacts, though there are examples of mountain ranges (or "Montes") somewhat similar to those on Earth. Saturn 's moon Titan and Pluto , in particular, exhibit large mountain ranges in chains composed mainly of ices rather than rock. Examples include

1368-628: The summer. They are the only home and namesake of the Fourche Mountain salamander . The Fourche Mountains form a major watershed divide between the Arkansas River Basin to the north and the Red River Basin to the south. The Frontal Ouachita Mountains are located in the Arkansas River Valley and feature a number of isolated landforms. The highest natural point is Mount Magazine at 2,753 feet (839 m), which

1406-532: The thermal springs of Hot Springs National Park . They are so named because of their unique chevron shape when viewed from above, the result of plunging anticlines and synclines . The Zig Zag Mountains are not exceptionally tall, but do reach heights over 1,400 feet (430 m). The Ouachitas are formed by a thick succession of highly deformed Paleozoic strata constituting the Ouachita Fold and Thrust Belt, which crops out for approximately 220 miles (350 km) in western Arkansas and southeastern Oklahoma . In

1444-527: The world's finest quartz , especially around Mount Ida, Arkansas , the quartz capital of the world. The quartz formed after the Ouachita Orogeny when fractures in rocks filled with silica-saturated fluids and, over millions of years, precipitated crystals up to several feet in length. The Ouachitas are also known for novaculite , a variety of chert that has undergone low-grade metamorphism ; particular grades found only in Arkansas are used for making whetstones . Cambrian through Mississippian strata of

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