| Alvord Hot Springs | |
|---|---|
 Algae matts in drainage area | |
 | |
| Location | Harney County, Oregon |
| Coordinates | 42°32′39″N118°32′02″W / 42.54417°N 118.53389°W [1] |
| Elevation | 4,078 feet (1,243 m) [1] |
| Type | Natural hot spring |
| Temperature | 174 °F (79 °C) |
  Location in Oregon | |
Alvord Hot Springs is a geothermal spring located in Harney County in southeastern Oregon in the United States.
The spring lies at 4,078 feet (1,243 m) elevation on the western edge of the Alvord Desert into which the spring flows and eventually evaporates. To the west of the springs lies Steens Mountain, a north-south running range with a peak of 9,738 ft (2,968 m) above sea level.
The source averages 174 °F (79 °C), but a system of pipes cools and regulates the flow of incoming water so that the pool temperature is maintained about 105 °F (44 °C). The spring smells somewhat of sulfur, yet not enough to dissuade visitors from soaking in one of two small, man-made rectangular concrete soaking pools, which are 3 feet (1 m) deep and either 25 by 50 feet (7.5 x 15 m) [2] or 10 by 20 (3 x 6 m). [3] [4] The soaking pools have a covered, as well as an open portion, the covered portion being rustic in its corrugated sheet metal and wood construction. [2]
Though they are on private property, before 2013, the use of the hot springs was free and open to the public year-round. [5] In early 2013 the property owners (the Alvord Ranch) installed a full-time caretaker in a trailer and started construction of a parking-lot and a small building which will house a store. Access to the hot springs are no longer free.[ citation needed ] Maintenance is volunteered by local residents and all visitors are encouraged to help keep the springs clean. [2]
Belknap Crater is a shield volcano in the Cascade Range in the U.S. state of Oregon. Located in Linn County, it is associated with lava fields and numerous subfeatures including the Little Belknap and South Belknap volcanic cones. It lies north of McKenzie Pass and forms part of the Mount Washington Wilderness. Belknap is not forested and most of its lava flows are not vegetated, though there is some wildlife in the area around the volcano, as well as a number of tree molds formed by its eruptive activity.
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.
The Alvord Desert is a desert located in Harney County, in southeastern Oregon in the Western United States. It is roughly southeast of Steens Mountain. The Alvord Desert is a 12-by-7-mile dry lake bed and averages 7 inches (180 mm) of rain a year. Two mountain ranges separate it from the Pacific Ocean—the Coast Range, and the Cascade Mountains. Along with Steens Mountain, these topographical features create a rain shadow. The Alvord Desert lies at an elevation of approximately 4,000 feet (1,200 m).
Ash Springs is an unincorporated community in the Pahranagat Valley of Lincoln County, Nevada. The community's principal industry is ranching. Ash Springs is named for the desert ash trees growing nearby.
Terwilliger Hot Springs, also known as Cougar Hot Springs, are geothermal pools in the Willamette National Forest in the U.S. state of Oregon, 53 miles (85 km) east of Eugene. The springs drain into Rider Creek, which in turn drains into Cougar Reservoir. They are about a quarter mile from Forest Service Road 19, also known as Aufderheide Memorial Drive.
Umpqua Hot Springs are a group of geothermal springs located along the North Umpqua River in the U.S. state of Oregon at 2,640 feet (800 m) elevation.
Lava Butte is a cinder cone in central Oregon, United States, just west of U.S. Route 97 between the towns of Bend, and Sunriver in Deschutes County. It is part of a system of small cinder cones on the northwest flank of Newberry Volcano, a massive shield volcano which rises to the southeast. The cinder cone is capped by a crater which extends about 60 feet (20 m) deep beneath its south rim, and 160 feet (50 m) deep from the 5,020-foot (1,530 m) summit on its north side. Lava Butte is part of the Newberry National Volcanic Monument.
Belknap Springs is an unincorporated community and private hot springs resort in Lane County, Oregon, United States, near the McKenzie River. The springs were located and initially developed by R. S. Belknap in 1869. A post office named "Salt Springs" was established in the location in 1874, and the name changed to "Belknap Springs" in 1875. The post office closed in 1877 and reopened in 1891, operating intermittently until 1953. Today the location uses a McKenzie Bridge mailing address.
The Bagby Hot Springs are natural hot springs in the Mount Hood National Forest, about 67 miles (108 km) southeast of Portland, Oregon, United States and about 98 miles (158 km) east of Salem, Oregon. The springs are within the Cascade Mountains in a heavily forested area at elevation 2280 ft. They are just outside the boundary of Bull of the Woods Wilderness area.
Hot Lake Hotel is a historic Colonial Revival hotel originally built in 1864 in Hot Lake, Union County, Oregon, United States. The hotel received its namesake from the thermal spring lakes on the property, and operated as a luxury resort and sanitorium during the turn of the century, advertising the medicinal attributes of the mineral water and drawing visitors worldwide. It is also the first known commercial building in the world to utilize geothermal energy as its primary heat source.
Borax Lake is a 10-acre (4.0 ha) alkaline lake in the Alvord Desert of southeastern Oregon in the United States. The lake is fed by geothermal springs 100 feet (30 m) below the surface that range in temperature from 104 to 300 °F. Surface water temperatures usually range from 61 to 100 °F but occasionally go higher. The springs lie along the Steens fault zone, which runs north–south through the Alvord Valley east of Steens Mountain.
Summer Lake Hot Springs are natural hot springs at the south end of Summer Lake in south-central Oregon. They are artesian mineral springs with four surface sources. The springs have complex water chemistry. The temperature of the main source is approximately 123 °F (51 °C) with a water flow of approximately 20 US gallons (76 L) per minute. Over the years, the site has been developed as a rustic family bathing and relaxation resort. The hot springs are 124 miles (200 km) southeast of Bend, Oregon, near the small town of Paisley, Oregon.
Fish Lake Hot Well, also known as Fish Lake Hot Spring and Fish Lake Valley Hot Well is a geothermal hot spring in Nevada.
Baranof Warm Springs are a series of ten geothermal mineral springs located in the small community of Baranof Warm Springs in Sitka, Alaska. The springs are surrounded by the Tongass National Forest.
Baker Hot Springs are a system of geothermal springs located on Fumarole Butte, northwest of the town of Delta, Utah. The springs were formerly known as Crater Springs and Abraham Hot Springs.
Breitenbush Hot Springs, also known as Breitenbusher Hot Springs, is a thermal mineral spring system along the Breitenbush River near the historic town of Breitenbush, Oregon, United States.
McCauley Hot Springs, also known as McCauley Warm Springs is a thermal spring in the Santa Fe National Forest, near the Jemez Springs area of Northern New Mexico.
Big Caliente Hot Springs are a grouping of thermal mineral springs located in the Los Padres National Forest of California.
Truth or Consequences Hot Springs is a thermal spring system located in the Hot Springs Artesian Basin area of Truth or Consequences, New Mexico in Sierra County.
Wiesbaden Hot Springs is a group of three thermal springs and a vapor cave in Ouray, Colorado. The spring water flows from the source at 118 °F and is cooled to between 99 °F and 108 °F in the soaking pools.
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