|Hot Springs National Park|
Pool of hot spring water in Hot Springs National Park
|Location||Garland County, Arkansas, United States|
|Nearest city||Hot Springs|
|Area||5,550 acres (22.5 km2)|
|Established||April 20, 1832 (designated as a national park on March 4, 1921)|
|Governing body||National Park Service|
|Website|| Official website |
Hot Springs National Park is an American national park in central Garland County, Arkansas, adjacent to the city of Hot Springs, the county seat. Hot Springs Reservation was initially created by an act of the United States Congress on April 20, 1832 to be preserved for future recreation. Established before the concept of a national park existed, it was the first time that land had been set aside by the federal government to preserve its use as an area for recreation. The hot spring water has been popularly believed for centuries to possess medicinal properties, and was a subject of legend among several Native American tribes. Following federal protection in 1832, the city developed into a successful spa town. Incorporated January 10, 1851, the city has been home to Major League Baseball spring training, illegal gambling, speakeasies and gangsters such as Al Capone, horse racing at Oaklawn Park, the Army and Navy Hospital, and 42nd President Bill Clinton. The area was made a national park on March 4, 1921.Until the redesignation of Jefferson National Expansion Memorial as Gateway Arch National Park in 2018, Hot Springs was the smallest national park by area in the United States. Since Hot Springs National Park is the oldest park maintained by the National Park Service, it was the first to receive its own US quarter in April 2010 as part of the America the Beautiful Quarters coin series.
A national park is a park in use for conservation purposes. Often it is a reserve of natural, semi-natural, or developed land that a sovereign state declares or owns. Although individual nations designate their own national parks differently, there is a common idea: the conservation of 'wild nature' for posterity and as a symbol of national pride. An international organization, the International Union for Conservation of Nature (IUCN), and its World Commission on Protected Areas (WCPA), has defined "National Park" as its Category II type of protected areas.
Garland County is a county located in the U.S. state of Arkansas. As of the 2010 census, the population was 96,024. The county seat is Hot Springs.
Hot Springs is a city in the state of Arkansas and the county seat of Garland County. The city is located in the Ouachita Mountains among the U.S. Interior Highlands, and is set among several natural hot springs for which the city is named. As of the 2010 United States Census, the city had a population of 35,193. In 2017 the estimated population was 36,915.
The hot springs flow from the western slope of Hot Springs Mountain, part of the Ouachita Mountain range. In the park, the hot springs have not been preserved in their unaltered state as natural surface phenomena. They have instead been managed to conserve the production of uncontaminated hot water for public use. The mountains within the park are also managed within this conservation philosophy to preserve the hydrological system that feeds the springs.
The Ouachita Mountains, 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 the southeast where they make a poorly understood connection with the Appalachians and to the southwest where they join with the Marathon 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.
Following 8,000 years of use by indigenous peoples, European Americans discovered and appropriated the springs. They have used the hot spring water in therapeutic baths for more than 200 years to treat rheumatism and other ailments. While this was a reservation, the area developed into a well-known resort nicknamed The American Spa; it attracted not only the wealthy but indigent health seekers from around the world.
Rheumatism or rheumatic disorder is an umbrella term for conditions causing chronic, often intermittent pain affecting the joints and/or connective tissue. The study of, and therapeutic interventions in, such disorders is called rheumatology. The term "rheumatism", however, does not designate any specific disorder, but covers at least 200 different conditions.
The park includes portions of downtown Hot Springs, making it one of the most accessible national parks. There are numerous hiking trails and camping areas. Bathing in spring water is available in approved facilities at extra cost. The entire Bathhouse Row area is designated as a National Historic Landmark District that contains the grandest collection of bathhouses of its kind in North America, including many outstanding examples of Gilded Age architecture. The row's Fordyce Bathhouse serves as the park's visitor center; the Buckstaff and Quapaw are the only facilities in 2015 still operating as bathhouses. Other buildings of the row are being restored or are used for other purposes.
Bathhouse Row is a collection of bathhouses, associated buildings, and gardens located at Hot Springs National Park in the city of Hot Springs, Arkansas. The bathhouses were included in 1832 when the Federal Government took over four parcels of land to preserve 47 natural hot springs, their mineral waters which lack the sulphur odor of most hot springs, and their area of origin on the lower slopes of Hot Springs Mountain.
A National Historic Landmark (NHL) is a building, district, object, site, or structure that is officially recognized by the United States government for its outstanding historical significance. Of over 90,000 places listed on the country's National Register of Historic Places, only some 2,500 are recognized as National Historic Landmarks.
North America is a continent entirely within the Northern Hemisphere and almost all within the Western Hemisphere; it is also considered by some to be a northern subcontinent of the Americas. It is bordered to the north by the Arctic Ocean, to the east by the Atlantic Ocean, to the west and south by the Pacific Ocean, and to the southeast by South America and the Caribbean Sea.
For many years, this area was visited by chiefs and tribes of numerous indigenous peoples. They called it the "Valley of the Vapors" at the time of Spanish explorer Hernando de Soto's arrival in the area in 1541. He was the first known European to see the springs. Members of many Native American tribes had been gathering in the valley for over 8,000 years to enjoy the healing properties of the thermal springs. Around the 18th century the Caddo settled in the area, followed by the Choctaw, Cherokee, and other tribes from the Southeast across the Mississippi River.There was agreement among the tribes that they would put aside their weapons and partake of the healing waters in peace while in the valley. The Quapaw lived in the Arkansas River delta area and visited the springs.
The Caddo Nation is a confederacy of several Southeastern Native American tribes. Their ancestors historically inhabited much of what is now East Texas, Louisiana, and portions of southern Arkansas and Oklahoma. They were descendants of the Caddoan Mississippian culture that constructed huge earthwork mounds at several sites in this territory. In the early 19th century, Caddo people were forced to a reservation in Texas; they were removed to Indian Territory in 1859.
The Choctaw are a Native American people originally occupying what is now the Southeastern United States. Their Choctaw language belongs to the Muskogean language family group. Hopewell and Mississippian cultures, who lived throughout the east of the Mississippi River valley and its tributaries. About 1,700 years ago, the Hopewell people built Nanih Waiya, a great earthwork mound located in what is central present-day Mississippi. It is still considered sacred by the Choctaw. The early Spanish explorers of the mid-16th century in the Southeast encountered Mississippian-culture villages and chiefs. The anthropologist John R. Swanton suggested that the Choctaw derived their name from an early leader. Henry Halbert, a historian, suggests that their name is derived from the Choctaw phrase Hacha hatak.
The Cherokee are one of the indigenous people of the Southeastern Woodlands of the United States. Prior to the 18th century, they were concentrated in what is now southwestern North Carolina, southeastern Tennessee, and the tips of western South Carolina and northeastern Georgia.
In 1673 Father Marquette and Jolliet explored the area and claimed it for France. The Treaty of Paris 1763 ceded the land back to Spain; however, in 1800 control was returned to France until the Louisiana Purchase of 1803.
Louis Jolliet was a French Canadian explorer known for his discoveries in North America. Jolliet and Jesuit Father Jacques Marquette, a Catholic priest and missionary, were the first non-Natives to explore and map the Mississippi River in 1673.
The Louisiana Purchase was the acquisition of the Louisiana territory of New France by the United States from France in 1803. The U.S. paid fifty million francs ($11,250,000) and a cancellation of debts worth eighteen million francs ($3,750,000) for a total of sixty-eight million francs. The Louisiana territory included land from fifteen present U.S. states and two Canadian provinces. The territory contained land that forms Arkansas, Missouri, Iowa, Oklahoma, Kansas, and Nebraska; the portion of Minnesota west of the Mississippi River; a large portion of North Dakota; a large portion of South Dakota; the northeastern section of New Mexico; the northern portion of Texas; the area of Montana, Wyoming, and Colorado east of the Continental Divide; Louisiana west of the Mississippi River ; and small portions of land within the present Canadian provinces of Alberta and Saskatchewan. Its non-native population was around 60,000 inhabitants, of whom half were African slaves.
In December 1804 William Dunbar and George Hunter made an expedition to the Ouachita Mountains and the springs at the request of President Thomas Jefferson, to study the native peoples and flora and fauna. They found one log cabin and a few rudimentary shelters used by people visiting the springs for their healing properties. In 1807 Jean Emmanual Prudhomme, of French colonial descent, became the first European-American settler of modern Hot Springs. After he regained his health following two years of bathing in the hot water and eating local foods, he returned home to his plantation on the Red River in Louisiana.Not long afterward trappers John Perciful and Isaac Cates arrived; Perciful put up more cabins for visitors.
On August 24, 1818, the Quapaw Indians ceded the land around the hot springs to the United States in a treaty after having been forced to a reservation south of the site.They were removed to Indian Territory in the 1830s. After Arkansas became a territory in 1819, the Arkansas Territorial Legislature requested in 1820 that the springs and adjoining mountains be set aside as a federal reservation. Twelve years later, in 1832, the 22nd United States Congress formed the national reservation, granting federal protection of the thermal waters and giving Hot Springs the honor of being the first area to be designated for federal government protection. The Hot Springs Reservation was set aside for public use as a park on June 16, 1880.
Although Hot Springs National Park is the oldest park managed by the National Park System, by act of Congress in 1921, the site's name was officially changed from the Hot Springs Reservation to the Hot Springs National Park. 900 acres (360 ha), including Hot Springs Mountain, North Mountain, West Mountain, Sugarloaf Mountain and Whittington Lake Park. It later was expanded to 5,000 acres (2,000 ha).The government acquired more land, expanding it to more than
The springs are all grouped about the base of the Hot Springs Mountain, with a flow of well over a half million gallons a day. The hot water is supplied to the various bathhouses, with resulting income from concession fees going to the U.S. Treasury. The park has miles of roads and trails over the mountains. The park is open throughout the year.
The first bathhouses were little more than brush huts and log cabins placed over excavations cut in the rocks to receive hot water that flowed from the springs. Entrepreneurs soon developed more elaborate bathing facilities, featuring wooden troughs delivering water from hillside springs to bathhouses along the east bank of Hot Springs Creek. Some of the tufa covering the hillside was excavated to accommodate the bathhouses. The narrow street along the west side of the creek was connected to the bathhouses by narrow bridges.
After direct federal supervision was exercised beginning in 1877, major improvements were made. The creek was covered with stone arches, and above it a street 100 feet wide was built. All the squatters were evicted, rubbish cleaned up, and a centralized plumbing system was begun.This was completed around 1890. In 1950 central cooling towers limited the maximum temperature of the springs to a safe level, so individual bathhouses no longer needed their own cooling systems.
The park operates a public campground at Gulpha Gorge, about two miles (3 km) from downtown Hot Springs.
The city of Hot Springs (incorporated 1851) is governed under State and municipal law. In the 1870s, African Americans in town were concentrated in Happy Valley, north of Hot Springs Mountain. There were churches of various denominations, including Baptist for white and black congregations.
The National Park Service exercises no control or supervision over any matters connected with the city. The city starts on the other side of Central Avenue from Bathhouse Row. Its development has extended beyond the narrow valley in which the springs are located, spreading out over the open plain to the south and east. The climate is good throughout the year. The elevation of the city is 600 feet (180 m) above sea level, with surrounding hills rising another 600 feet. In the first half of the 20th century, the city operated primarily as a summer resort, but hotels have now long stayed open during the winter due to many northerly patrons coming to escape the winter cold.
During the peak popularity of the hot springs, until the 1950s, the many patients staying for three weeks, six weeks, or longer were a large source of business for the numerous hotels, boarding houses, doctors, and drugstores. As the daily treatments required only an hour or two, the visitors' idle time created opportunities for other businesses in the town.
It was believed the waters benefited diseases of the skin and blood, nervous affections, rheumatism and kindred diseases, and the "various diseases of women". In the case of tuberculosis and lung diseases, and acute and inflammatory diseases, the use of the waters was considered injurious and in many cases very dangerous.
The earliest bathing procedure consisted of merely reclining in natural pools of hot springs and cool creek water for long periods of time. During the 1820s crude vapor baths stood over the springs, and bathers breathed in the vapors for extended periods of time. Wooden tubs were added to some bathhouses in the 1830s. Physicians began arriving in the 1850s, although many visitors did without their services; visitors remained from one week to two months. After the Civil War a tub bath of 15 to 20 minutes was common.
During the 1870s the bathing regimen became more diverse, and physicians prescribed various types of baths for patients. The period of time for tub baths became six to ten minutes and the time in the steam bath shortened to two minutes, with only one bath a day.
The treatment was by drinking and bathing in the waters, producing a profuse perspiration, which was considered an active agent in fighting disease. The advice of a physician who was familiar with the use of the waters was considered necessary to avoid injury. In many cases medicine was required before using the waters, although it had been observed that the amount of drugs given was "enough to sicken a well man."
The hot baths were usually taken once a day for three weeks, when a rest was necessary (often with a week at the sulphur springs near the Ouachita River). A second three weeks' course was then taken, followed again by an abstinence from bathing for several days. The usual stay at the springs was from one to three months, but many invalids stayed a year and longer.
The process described in 1878 was a hot bath of 90 to 95 °F (32 to 35 °C) for about 3 minutes (timed with a sand-glass). This was followed by another three minutes with all but the head in a steam box, or if milder treatment was prescribed, sitting atop the steam box covered with a blanket. During this the bather is also drinking hot water from their coffee-pot. After these eight to ten minutes of treatment, the bather is well rubbed down and thoroughly dried. The blanket-covered customer then would walk briskly back to their quarters to lie down for at least a half-hour to let the body recover its normal temperature. Sleeping at this stage was considered dangerous.
The bathhouses began using vapor cabinets around 1884. The bather sat in the cabinet for 10–20 minutes with the lid closed tightly around the neck, with vapor from the hot water rising through the floor of the cabinet, with temperatures around 110–130 °F (43–54 °C). Toward the end of the 1880s Russian and Turkish baths were offered, and in the 1890s German needle baths and Scotch douches (concentrated stream of hot or cold water, often used on the back) were added.
Although details of services were left to bathhouse operators, the Park's superintendent set various rules. In the 1930s a tub bath could not take more than 20 minutes and shower no more than 90 seconds. During the next decade shower time was reduced to a minute, with maximum temperatures specified for several services. After a bath of about 98 °F (37 °C), the patient might spend 2–5 minutes in a vapor cabinet, get 15 minutes of packs (wet, hot or cold), followed by a tepid needle shower and light massage and alcohol rub.
By 1980 one reporter described getting a 20-minute bath, two minutes in a steam bath, 15 minutes wrapped with hot packs, and resting in a cooling room for 20–30 minutes.
The current modern facilities are oriented toward spa style or pool services.
There have been nearly two dozen pay bathhouses operating at the same time, with about nine of those within the park's "Bathhouse Row." (Facilities have been reworked over the years, and the Quapaw operate a bath incorporating two previously separate bathhouses). Nine of the bathhouses were associated with hotels, hospitals, or sanatoria. The water is the same for all, but the prices charged for the baths have varied according to the equipment, accommodations and services offered by each facility. The charges for the services of the attendants are the same and include the necessities except towels, blankets, bathrobes, laundering, rubbing mercury, and handling of invalids.
The area was popular with baseball players in the early 20th century, and was used by some teams for spring training. In 1929, prices for single baths ranged from $1 to $1.40, while a course of 21 baths was $16 to $24. Facilities were segregated until civil rights legislation in the 1960s. Baths were offered for whites at the Arlington Hotel, Fordyce, Buckstaff, the 500-room Eastman Hotel, Maurice, La Mar, Majestic Hotel, Quapaw, Hale, Imperial, Moody Hotel, Ozark, St. Joseph's Infirmary, Superior, Ozark Sanatorium, Rockafellow, and Alhambra, and for people of color at the Pythian, Woodmen of Unionand National Baptist Hotel and Sanitorium.
At present on Bathhouse Row only the Buckstaff and Quapaw are operating as bathhouses. The Fordyce is open as a visitors center; its staff gives tours of the facilities that have been historically renovated to their original appearance. The Ozark is housing the Museum of Contemporary Art; its space can be rented as reception hall. The Arlington Hotel, Austin Hotel and Convention Center, and The Springs Hotel & Spa also offer hot spring baths using the Park water.
The Army and Navy General Hospital (now the Rehabilitation Center) was also supplied with water from the springs. It is located behind the south end of Bathhouse Row along the base of Hot Springs Mountain. It was administered by the War Department for the benefit of military members, officers of the Public Health Service, and honorably discharged veterans. The waters of the hot springs had an established reputation in benefiting. Admission to the hospital was reserved for cases "of a serious and obstinate character, which, though resisting ordinary methods of relief, were promised a rapid and permanent recovery from the use of the waters of the spring."
The facility now known as the Hot Springs Rehabilitation Center was built in 1933 as the second Army-Navy hospital. It has been used and operated by the state for over 50 years.It is listed on the National Register of Historic Places.
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In November 1864 during the American Civil War, a large part of "the valley" (the central portion of the city along Hot Springs Creek) was burned - presumably by Union troops.
As in many other cities, fire has been a risk, especially before city services were developed. On March 5, 1878 a large fire burned for eight hours in the city, claiming nearly 150 buildings, including hotels, bath houses, and restaurants. On February 26, 1905, a fire started in the Grand Central Hotel on Chapel Street and burned 25 blocks of the southern section of Hot Springs. On September 5, 1913, a laundry worker was ironing and accidentally started a fire at 424 Church Street, which spread rapidly due to strong winds and burned nearly 60 blocks of the south part of the city.
The city has also been subject to flooding because of the narrow valley. On May 14, 1923, a severe rainstorm hit the city. With mountains surrounding three sides of the city, water flooded down the slopes of the mountains, funneling to Central Avenue and reaching a depth of nine feet. A lightning strike during the storm caused a fire that destroyed several commercial businesses in downtown Hot Springs. On February 15, 1956, a severe flood filled Central Avenue with three feet of rushing water, causing significant property damage. On May 19, 1990, a series of storms dropped more than 13 inches (330 mm) of rain into the city, causing flash floods. A wave of water six feet high washed through downtown Hot Springs, causing extensive damage. During the flood, Carpenter Dam Bridge was washed away.
On February 27, 2014, fire broke out at the Majestic Hotel on Park Avenue just outside the boundaries of the national park. It took 75 firefighters over 22 hours to extinguish the blaze in the oldest section of the hotel, and in the end the building was a total loss. Just days later, the city of Hot Springs had the "red brick" portion of the building razed. It was believed that trespassers had started the blaze. The remainder of the Majestic was razed in the Fall of 2016.
Congress established a free bathhouse for the indigent here on December 16, 1878. The Ral Hole mudpit and pool were closed, and the first Government Free Bathhouse operated at the site. [ citation needed ] Applicants for free baths were required to make an oath that they were without and unable to obtain means to pay for the baths, with violations being a misdemeanor subject to fine and/or imprisonment.[ citation needed ] Tickets were issued to those who, after examination, were found to be suffering from diseases which were reasonably expected to be benefited from the baths.[ citation needed ]The Government free bathhouse was a concrete building fully equipped for bathing large numbers of people under sanitary conditions. In 1878 the Army and Navy opened a free dispensary on the second floor, which remained open for two years. In 1916 the Public Health Service opened a clinic for the examination and treatment of indigents taking the free baths. 100,000 baths a year were given to the poor.
During the 1880s a few of the open springs gradually dried up. Corn Hole, a popular spring where people soaked their feet, dried up in 1882.Other open springs were either covered over by the National Park Service or the bathhouse owners to prevent their pollution.
A new free bathhouse was built in 1904, with separate facilities for black and white patrons. The materials used in construction were of poor quality. A new bathhouse was built off the reservation in 1922.The Park Service reminded people that they had to provide their own board and lodging and to have return travel fare, due to many destitute invalids who arrived each year in the mistaken belief that there was a public institution at which they would be cared for free of charge. The free bathhouse closed in 1957, as it was more economical to have the few indigent customers served by the commercial bathhouses. The poor applied at park headquarters and upon approval by a physician were sent to a participating bathhouse, which was reimbursed by the government.
The area is primarily forest. The northern slopes of the ridges and basins provide a suitable habitat for deciduous forest dominated by oak and hickory. Pines predominate on the south sides of the ridges. There are 230 acres (93 ha) of unlogged pine and oak forests on North and Hot Springs Mountains, and 90 acres (36 ha) on Sugarloaf Mountain. These old-growth forests contain shortleaf pine, blackjack oak, and white oak; many of the trees over 130 years old, and a few over 200 years old.
Plains bison, elk, cougar and red wolf left the region after European settlement. Present day fauna include white tail deer, wild turkey, squirrel, rabbit, Virginia opossum, gray fox, coyote, skunk, raccoon, gopher, long-tailed weasel, mink, rat, chipmunk, frog, and nine-banded armadillo. Some migratory birds following the Mississippi Flyway spend part of the year in the vicinity.
The thermal springs are situated in the Ouachita Mountains of central Arkansas. The springs emerge in a gap between Hot Springs Mountain and West Mountain in an area about 1,500 feet (460 m) long by 400 feet (120 m) wide at altitudes from 576 to 683 feet (176 to 208 m). The springs predominantly are composed of hot water from thousands of feet underground mixed with some shallow cold ground water. Currently, there are 43 thermal springs in the park that are presumed to be flowing. Thermal water from 33 of the thermal springs is collected and monitored at a central reservoir, which distributes the combined discharge for public use and consumption. Rock types in the area include shale units which generally impede ground-water movement, while fractured chert, novaculite, and sandstone units generally support ground-water movement.
The water comes from rain which falls in mountains to the north and northeast. Flowing downward through cracked rock at about one foot per year, the meteoric water migrates to estimated minimum depths of 4,500 to 7,500 ft (1,400 to 2,300 m) and achieves high temperatures in the deep section of the flow path before rising along fault and fracture conduits. Under artesian pressure, the thermal waters rise and emerge through the Hot Springs Sandstone between the traces of two thrust faults, along several northeast-trending lineaments. Some rainwater from near the springs mixes with the deep hot water before discharge. The trip down takes about 4,000 years while the hot water takes about a year to reach the surface.
The heat comes from the natural heating of rocks as depth increases. The composition of the water indicates it is heated rainwater which has not approached a magmatic source, so no volcanic action is involved in the formation of these hot springs. The result is the mildly alkaline, pleasant tasting solution with dissolved calcium carbonate.
The exposed rock types in the vicinity of the thermal springs are sedimentary rocks of Mississippian to Ordovician age, with the exception of younger igneous rocks (Cretaceous age) exposed in two small areas about 6 and 11 miles (9.7 and 17.7 km) southeast of the thermal springs (Potash Sulphur Spring and Magnet Cove, respectively), and in many small dikes and sills. Most dikes are less than 5 ft (1.5 m) wide. There have been 80 dikes noted about 4 miles (6.4 km) southeast of Hot Springs, on and near the Ouachita River. There is no indication that igneous rock occurs where the thermal springs discharge.
The sedimentary rocks in the vicinity of the thermal springs consist of shale, chert, novaculite, sandstone, and conglomerate.
During most of the Paleozoic Era, what became the Ouachita Mountains was the bottom of a shallow sea, where several sedimentary layers were created. About 500 million years ago a collision of the South American Plate with the North American Plate caused the shale and sandstone layers to fracture and fissure, creating mountains of the folded rocks. 9,200 ft (2,800 m) onto the southeast flank of North Mountain, and dips about 26 degrees north. At the northern extent of the thermal springs, this fault is suggested to form along the bedding contact of the Hot Springs Sandstone and Stanley Shale, with the Stanley Shale forming the hanging wall of the fault. The southern fault extends northeastward about 9,000 ft (2,700 m) roughly along the axis of the Hot Springs anticline, and dips about 44 degrees north. It has been proposed that a fault splits away from the southern fault, trends west and connects with the northern fault. A natural ravine trends along the location of this fault. Extensive cracks, joints, and fissures in the Bigfork Chert, Arkansas Novaculite, and the Hot Springs Sandstone allow the water to flow in the thermal springs area. Dissolved minerals in the water precipitate to form the white to tan travertine or "tufa rock" seen near the openings of the hot springs.The thermal springs emerge from the plunging crest line of a large overturned anticline in the Zigzag Mountains of the Ouachita anticlinorium. The overturned anticline plunges toward the southwest into the Mazarn Basin. There are two recognized major thrust faults trending nearly parallel to fold axes that define the northern and southern limits of the thermal springs discharge area. The northern fault extends nearly parallel to Fountain Street northeastward about
The water all comes from the same deep source, but surface appearance of the springs differed. What was called Mud Spring had a tepid ooze where there was no danger of being scalded. Springs acquired names such as Magnesia, Big Iron, and Arsenic. Big Iron's water, with significant dissolved iron, would precipitate ocherous crusts and stains. 750,000 to 950,000 US gallons (2.8 to 3.6 ML) a day. The temperature averages about 143 °F (62 °C). Maximum temperatures have declined about 5 °F (2.8 °C) since records have been kept.Arsenic Spring, on the other hand, contains no detectable traces of that substance. The water from many springs is now combined in one supply, with the total amount of water varying from
In 1905 curative characteristics were being ascribed to radium and Bertram Boltwood of Yale examined these waters. There is a measurable level of radioactivity primarily due to dissolved radon gas, with some radium. At the time collection and distribution equipment was designed to retain the radon gas, while now it is designed to allow it to escape. The level of exposure to radiation that results from bathing appears to be similar to the level that would result from sitting in the sun for the same period of time. The park water is considered well within safe limits and similar to other natural waters throughout the world.
Drinking water is dispensed from several hot water jug fountains. The hot water is naturally potable. Two cold water springs (Happy Hollow and Whittington Springs) are treated using ozone filtration. Regulations prohibit private individuals from selling the park's waters.
|Chemical||Parts per million|
|Free carbon dioxide (CO2)||9.7|
An onsen (温泉) is a Japanese hot spring; the term also extends to cover the bathing facilities and traditional inns frequently situated around a hot spring. As a volcanically active country, Japan has thousands of onsens scattered throughout all of its major islands.
Mount Magazine, officially named Magazine Mountain, is the highest point of the U.S. Interior Highlands and the U.S. state of Arkansas, and is the site of Mount Magazine State Park. It is a flat-topped mountain or mesa capped by hard rock and rimmed by precipitous cliffs. There are two summits atop the mountain: Signal Hill, which reaches 2,753 feet (839 m), and Mossback Ridge, which reaches 2,700 ft (823.0 m).
The Roman Baths complex is a site of historical interest in the English city of Bath. It is a well-preserved Roman site once used for public bathing.
Thermae Bath Spa is a combination of the historic spa and a contemporary building in the city of Bath, England, and re-opened in 2006. Bath and North East Somerset council own the buildings, and, as decreed in a Royal Charter of 1590, are the guardians of the spring waters, which are the only naturally hot, mineral-rich waters in the UK. The Spa is operated by YTL Hotels.
Public baths originated from a communal need for cleanliness at a time when most people did not have access to private bathing facilities. The term "public" is not completely accurate, as some types of public baths are restricted depending on membership, gender, religious affiliation, or other reasons. As societies have changed, the need for public baths has reduced: dwellings now have their own private bathroom. Public baths have also become incorporated into the social system as meeting places. As the title suggests, public bathing does not refer only to bathing. In ancient times public bathing included saunas, massages and relaxation therapies, comparable to today's spas.
A spa is a location where mineral-rich spring water is used to give medicinal baths. Spa towns or spa resorts typically offer various health treatments, which are also known as balneotherapy. The belief in the curative powers of mineral waters goes back to prehistoric times. Such practices have been popular worldwide, but are especially widespread in Europe and Japan. Day spas are also quite popular, and offer various personal care treatments.
Novaculite, also called Arkansas Stone, is a microcrystalline to cryptocrystalline rock type that consists of silica in the form of chert or flint. It is commonly white to grey or black in color, with a specific gravity that ranges from 2.2 to 2.5. It is used in the production of sharpening stones. It occurs in parts of Arkansas, Oklahoma, and Texas, as well as in Japan and parts of the Middle East. The name novaculite is derived from the Latin word novacula, meaning a sharp knife, dagger, or razor in reference to its use in sharpening.
Berkeley Springs State Park is situated in the center of Berkeley Springs, West Virginia, USA. The centerpiece of the Park is its historic mineral spa. These waters were celebrated for their medicinal or restorative powers and were generally taken internally for digestive disorders, or bathed in for stress relief. Native peoples visited these springs as did George Washington. Berkeley Springs is the only state-run spa in the United States and is operated by the West Virginia Division of Natural Resources.
Banff Upper Hot Springs are commercially developed hot springs located in Banff National Park in Alberta, Canada, near the Banff townsite. Discovered in 1883, the hot pool is outdoors and while in the pool, visitors can look across the valley to Mount Rundle. It is located at 1,585 metres (5,200 ft) of elevation, which makes it the highest hot spring in Canada.
Bathing played a major part in ancient Roman culture and society. It was one of the most common daily activities in Roman culture, and was practiced across a wide variety of social classes.
The Ouachita orogeny was a mountain building event that resulted in the folding and faulting of strata currently exposed in the Ouachita Mountains. The more extensive Ouachita system extends from the current range in Arkansas and Oklahoma southeast to the Black Warrior Basin in Alabama and to the southwest through the Llano, Marathon, and Solitario uplifts in Texas on into Coahuila and Chihuahua in Mexico.
The Arlington Resort Hotel & Spa is a resort in the Ouachita Mountains of Hot Springs National Park, Arkansas, home of Oaklawn Race Track and the Arkansas Derby. The Arlington's sister hotel was the Baker Hotel in Mineral Wells, Texas. The hotel is located at the north end of "Bathhouse Row".
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.
Beppu Onsen (別府温泉) is a group of hot springs in the city of Beppu, Ōita in Japan. Beppu Onsen is divided into eight major hot spring areas known as "Beppu Hatto".
The Central Avenue Historic District is the historic economic center of Hot Springs, Arkansas, located directly across Central Avenue from Bathhouse Row. Built primarily between 1886-1930, the hotels, shops, restaurants and offices on Central Avenue have greatly benefited from the city's tourism related to the thermal waters thought to contain healing properties. Built in a variety of architectural styles, the majority of the buildings constituting the district are two- or three-story structures. The district was listed on the National Register of Historic Places in 1985, at which time forty contributing structures were identified; 101 Park Avenue was added in 2007.
Bimini Baths was a geothermal mineral water public bathhouse and plunge in what is now Koreatown, Los Angeles, California, US. It was situated just west of downtown, near Third Street and Vermont Avenue. Bimini Baths contained a natatorium, swimming pools, swimming plunge, Turkish baths, a medical treatment department, and bottling works.
The Stanley Shale, or Stanley Group, is a Mississippian stratigraphic unit in the Ouachita Mountains of Arkansas and Oklahoma. First described in Arkansas in 1892, this unit was not named until 1902 by J.A. Taff in his study of the Ouachita Mountains of Oklahoma. Taff assigned the town of Stanley in Pushmataha County, Oklahoma as the type locality, but did not designate a stratotype. After introduction into Arkansas in 1909 by Albert Homer Purdue, the unit was redefined in 1918, when the formation known as the Fork Mountain Slate was abandoned and partially combined into the Stanley Shale. As of 2017, a reference section for the Stanley Shale has yet to be designated.