This article needs additional citations for verification .(May 2022) |
Mammoth Spring | |
---|---|
Location | |
Country | United States |
State | Arkansas |
Region | Ozark Plateau |
City | Mammoth Spring |
Physical characteristics | |
Source | Spring River watershed |
• location | Salem Plateau, Ozark Plateau, Missouri |
Mouth | Spring River |
• location | Mammoth Spring, AR |
• coordinates | 36°29′51″N91°32′08″W / 36.49750°N 91.53556°W Coordinates: 36°29′51″N91°32′08″W / 36.49750°N 91.53556°W [1] |
• elevation | 490 ft (150 m) |
Discharge | |
• location | Mammoth Spring(harmonic mean flow)1981-2015 [2] |
• average | 322 cu ft/s (9.1 m3/s)(harmonic mean flow)1981-2015 [3] |
• maximum | 694 cu ft/s (19.7 m3/s) |
Basin features | |
U.S. NNL | Designated 1972 |
Mammoth Spring is a large, first magnitude karst spring that arises in the Ozark Plateau within the state of Arkansas. It is the largest spring in Arkansas and the third-largest spring within the Ozark Plateau region behind Big Spring and Greer Spring. Mammoth Spring is the seventh-largest natural spring in the world.
The spring's outlet pool is contained entirely within Mammoth Spring State Park. The park is located in the town of Mammoth Spring, which lies in extreme north-central Arkansas. The outlet pool is adjacent to US Highway 63, only 500 ft. south of the Missouri border, and it can be readily seen from the highway. The spring's large discharge volume rushes a few hundred feet down the outlet channel before merging with the Warm Fork of the Spring River to form the Spring River. The cold water that emerges from the spring creates excellent trout fishing conditions and ample flow for water sports on the Spring River. Mammoth Spring was declared a National Natural Landmark by the Department of the Interior in June 1972. [4]
Precipitation that falls in southern Missouri seeps into the water table and flows through a vast system of passages and cavities. These cavities form an underground river that ultimately emerges on the surface at the town of Mammoth Spring, Arkansas. The emerging water forms a 10-acre spring pool that drains over a high stone dam. The spring generates a harmonic mean flow of about 9 m³/s (322 cubic feet per second). The water emerges at a constant 14 °C (58 °F). The spring itself cannot be viewed at the Mammoth Spring site because its mouth is more than 21 m (70 ft) below the surface of the large spring pool.
Nine miles northwest of Mammoth Spring, visitors can see a portion of the underground river that feeds the spring at a collapsed cave in Grand Gulf State Park in Missouri. The remains of a portion of the cave are now a 40 m (130 ft) deep chasm with a natural bridge over it. Dye tests have proven that the water flowing through the 40 m (130 ft) chasm at Grand Gulf exits through the existing cave and emerges at Mammoth Spring.
The spring was used to power a gristmill from the times of the earliest European settlement. The Mammoth Spring Milling Company constructed a dam and a water-powered gristmill just downstream of the outlet of the spring lake. In 1925, the dam was purchased by the Arkansas-Missouri Power Company which constructed a hydroelectric plant at the dam. This plant supplied power to the surrounding area until 1972.
In 1957, Mammoth Spring State Park was established. Surrounding land claims could not be acquired until 1972, however. Prior to 1972, the Mammoth Spring Cattle Sales Barn was co-owned and run by local entrepreneur Bert Kenneth Bishop and his associate, roughly on the site of where the Welcome Center now stands. Local farmers would routinely come to the site to sell livestock and other wares, such as Howard Green, who sold home-made walking sticks. Following this period in history, the State legislature voted to condemn the land and join the plot to the state park.
The original Frisco Depot was restored in 1971 and now functions as a repository for artifacts and memorabilia related to the railroad and the spring area. The State Park provides a visitor's center, picnic areas, walking trails, and tour access to the dam and hydro plant.
The United States Fish and Wildlife Service maintains a fish hatchery near the spring.
Missouri, a state near the geographical center of the United States, has three distinct physiographic divisions:
The Ozarks is a physiographic region in northern Arkansas and southern Missouri, United States.
The White River is a 722-mile (1,162 km) river that flows through the U.S. states of Arkansas and Missouri. Originating in the Boston Mountains of northwest Arkansas, it arcs northwards through southern Missouri before turning back into Arkansas, flowing southeast to its mouth at the Mississippi River.
A spring is a point of exit at which groundwater from an aquifer flows out on top of Earth's crust (pedosphere) and becomes surface water. It is a component of the hydrosphere. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall.
The Spring River is a 57-mile (92 km) long river which flows through the U.S. states of Missouri and Arkansas. It consists of two branches, the South Fork of the Spring River and the Spring River proper. The South Fork of the Spring River starts in Howell County, Missouri and flows south through Fulton and Sharp counties in Arkansas. The South Fork of the Spring River joins the Spring River proper near the town of Hardy, Arkansas. The South Fork is a quiet stream with gravelly bars that are ideal for camping.
Mammoth Spring State Park is a 62.5-acre (25.3 ha) Arkansas state park in Fulton County, Arkansas in the United States. The park is located surrounding National Natural Landmark of the same name to provide recreation and interpretation for visitors. The park offers fishing, boating and hiking in addition to an Arkansas Welcome Center and restored 1886 St. Louis–San Francisco Railway (Frisco) depot operating as a railroad museum. The site became a state park in 1957, but the park continued to add area until 1975.
The Green River is a 384-mile-long (618 km) tributary of the Ohio River that rises in Lincoln County in south-central Kentucky. Tributaries of the Green River include the Barren River, the Nolin River, the Pond River and the Rough River. The river was named after Nathanael Greene, a general of the American Revolutionary War.
The Jefferson River is a tributary of the Missouri River, approximately 83 miles (134 km) long, in the U.S. state of Montana. The Jefferson River and the Madison River form the official beginning of the Missouri at Missouri Headwaters State Park near Three Forks. It is joined 0.6 miles (1.0 km) downstream (northeast) by the Gallatin.
The Current River forms in the southeastern portion of the Ozarks of Missouri and becomes a 7th order stream as it flows southeasterly out of the Ozarks into northeastern Arkansas where it becomes a tributary of the Black River, which is a tributary of the White River, a tributary of the Mississippi River. The Current River is approximately 184 miles (296 km) long and drains about 2,641 square miles (6,840 km2) of land mostly in Missouri and a small portion of land in northeastern Arkansas. The headwaters of the Current River are nearly 900 feet (270 m) above sea level, while the mouth of the river lies around 280 feet (85 m) above sea level. The basin drains a rural area that is dominated by karst topography, underlain by dolomite and sandstone bedrock with a small area of igneous rock southeast of Eminence, Missouri. The annual daily mean discharge of the river near Doniphan, Missouri is 2,815 cubic feet (79.7 m3) per second. In 1964, over 134 mi (160 km) of the upper course of the river and its tributaries were federally protected as the Ozark National Scenic Riverways, the first national park in America to protect a river system.
The St. Francis River is a tributary of the Mississippi River, about 426 miles (686 km) long, in southeastern Missouri and northeastern Arkansas in the United States. The river drains a mostly rural area and forms part of the Missouri-Arkansas state line along the western side of the Missouri Bootheel.
Maramec Spring is located on the Meramec River near St. James in the east-central Ozarks of Missouri. The fifth largest spring in the state with an average discharge of 153 cubic feet (4.3 m3) of water per second, it is part of a Karst topographical area, with many springs and caves. The spring and 1800 acres (7.28 km²) are owned by the James Foundation, which maintains the area as a public park, donated by Lucy Wortham James. The Missouri Department of Conservation operates a trout hatchery and fishery at the spring. Ruins of the Maramec Iron Works are still visible at the site; its machinery was partly powered by the spring's waterflow. The spring was declared a National Natural Landmark in October 1971.
Rockbridge is an unincorporated community in northern Ozark County, Missouri, United States. It is the site of an old mill on spring fed Spring Creek, a tributary of Bryant Creek, which still houses the post office. It lies twelve miles north of Gainesville on Missouri Route N, approximately one and one-half miles north of Route 95. The narrow valley floor is only about 650 feet (200 m) wide and at an elevation of 770 feet (230 m) and the Ozark ridges on either side are 200 to 250 feet higher.
The Spring River is a 129-mile-long (208 km) waterway located in southwestern Missouri, southeastern Kansas, and northeastern Oklahoma.
The Roaring River is a 14.9-mile-long (24.0 km) river in Barry County, Missouri, in the Ozarks. It is a tributary of the White River, into which it flows in Eagle Rock, Missouri. This section of the White River is a reservoir called Table Rock Lake.
Optima Lake was built to be a reservoir in Texas County, Oklahoma. The site is just north of Hardesty and east of Guymon in the Oklahoma Panhandle.
The Lost River is a river that rises in Vernon Township, Washington County, Indiana, and discharges into the East Fork of the White River in Lost River Township, Martin County, Indiana. The river's unusual hydrology has led to two of its features being named as National Natural Landmarks.
The geography of Arkansas varies widely. The state is covered by mountains, river valleys, forests, lakes, and bayous in addition to the cities of Arkansas. Hot Springs National Park features bubbling springs of hot water, formerly sought across the country for their healing properties. Crowley's Ridge is a geological anomaly rising above the surrounding lowlands of the Mississippi embayment.
Big Spring is one of the largest springs in the United States and the world. An enormous first magnitude spring, it rises at the base of a bluff on the west side of the Current River valley in the Missouri Ozarks.
Greer Spring is a first magnitude spring located in the southeast portion of the Ozark Plateau, in Oregon County in south-central Missouri within the boundaries of the Mark Twain National Forest. The spring is the second largest spring in the Ozarks, with an average discharge of 360 cubic feet (10 m3) of water per second. Greer Spring was designated a National Natural Landmark in 1980.