Borax Hot Springs

Borax Hot Springs

Borax Hot Springs & Borax Lake

Borax Hot Springs

Borax Hot Springs

A geological phenomenon of southeastern Oregon, Borax Hot Springs is one of the three main geothermal springs of the Alvord Basin. Belonging to the same fault zone, Alvord and Mickey Hot Springs are located 2 and 4 miles north of Borax Hot Springs accordingly. All of those hot springs occur within the valley bounded by rotational fault blocks of Steens and Pueblo Mountains on the west and the Sheepshead and Trout Creek Mountains on the east. Borax Lake, numerous hot springs, and vents are aligned exactly along the active fault line.

The 10-acre Borax Lake, also known as Hot Lake, is created by a powerful spring's flow of the southernmost hot springs outlet that sits deep, 100 feet (32 m) below the lake's surface. The temperature of geothermal springs outflow ranges between 104 and 300°F (40-140°C). The temperature of the lake itself can vary between 61 and 100°F (16-38°C). The Borax Lake overflow nurtures the Little Borax Lake.


Borax Hot Springs
Borax Workstation Ruins

Near the lake, there are rusting ruins of the steel vats, an old Borax workstation where borax was extracted and hauled by a mule train to Winnemucca, Nevada.

A commercial borax producing was open by Charles Taylor and John Fulton in 1898. Those two men moved their business from the Black Rock Desert in Nevada to Hot Lake in Oregon. They built two steel vats and hired 30 Chinese workers. Sodium borate from the desert surface was mixed with the water from the hottest lake's center; also, sulphuric acid as a precipitating agent was added. The mixture in the vats was heated to the boiling point. Later, when the solution cooled, the pure crystalline borax was formed.

In 1907, a quality of sodium borate deposits was declined, borax productions were ceased and, finally, the business was closed.

At the time of a commercial use, the lake and surrounding area acquired a new name - Borax Lake.

Unique Profile of Borax Hot Springs & Borax Lake

Borax Hot Springs
Borax Hot Springs pool

The unique nature of the geothermal ecosystem and mineralizing environment with great sodium borate (borax) deposits in the soil is driving researchers to Borax Lake. Many ecological, geochemical, geological, paleontological, mineralogical, and hydrological studies have been done. Surveys of aquatic invertebrates and geothermal microbes have been taken in Borax Lake and the adjacent hot springs.

Scientists have monitored the population of the rare and endangered species of the Borax Lake Chub that is found near the shore; the chub prefers the cooler temperature - around 85°F. This miraculous cyprinid fish survived and evolved within the last 10,000 years in the extreme environments and can be found in Borax Lake and Lower Borax Lake only.

Borax Hot Springs have a water pH that ranges between neutral and slightly alkaline that is extremely friendly to thermophilic microbes. Colorful edges of the thermal pools are colonies of thermophiles distributed on the basis of temperature and the ratio of chlorophyll and carotenoids. Read more about a variety of pigmented bacteria of the microbial mats in the hot springs.

The water of the hot springs contains the highest concentrations of sodium borate (borax), arsenic and lead which make the water unsafe to drink.

Borax Hot Springs & Borax Lake
Borax Lake

In 1993, The Nature Conservancy bought 160-acre private land including Borax Lake to save endangered species of Borax Lake Chub, as well as the fragile and unique geothermal ecosystem. Currently, the area is managed by The Nature Conservancy, BLM and the Oregon Department of Fish and Wildlife.  Due to Borax Lake is a biological preserve, only foot traffic is allowed from the second gate.

Visitors or tourists are allowed to visit the site, however, swimming in the lake, soaking in the hot springs are forbidden due to health hazards and in order to preserve this exceptional and delicate ecosystem.

Cautions: The scalding temperatures, steam, and fragile ground surface make ground surface unsafe. The posted signs warn about dangers of this area. Watch your step, the thin ground surface could break under your weight and expose you to boiling water.

Borax Lake Hot Springs | General Description

Cautions: Dangerously hot for soaking

Open: Year-round
Managed: BLM
Development: Undeveloped, preserve
Service: None
Accommodations: Not allowed within Borax Lake & Hot Springs area
Distance from a parking: 0.5 miles
Road Access: High-clearance vehicles, the road can be inaccessible during wet weather
Day-use fees: None

Elevation: 4,070 ft (1,240 m)

Borax Hot Springs and Borax Lake are located:

  • 7 miles north of Fields
  • 116 miles south of Burns
  • 381 miles southeast of Eugene
  • 377 miles southeast of Salem
  • 421 miles southeast of Portland.

Water T° (lake): 61°F (16°C) - 100°F (38°C)
Water T° (hot springs): 104°F (40°C) - 300°F (140°C)
Water acidity level: Neutral to Weak Alkaline (pH=7.3 to 8.7)
Type of the springs: Sodium Sulfate Chloride

Average dissolved solids: 1,200 Mg/L

Sodium - 426 Mg/L
Sulfate - 329 Mg/L
Chloride - 265 Mg/L
Silica - 160 Mg/L
Potassium - 29 Mg/L
Calcium - 9.6 Mg/L
Flouride - 6.5 Mg/L
Alkanility - 425 Mg/L

Directions to Borax Lake Hot Springs

  • From Fields, head north 1.4 miles to the junction of Highway 205 and Fields-Denio Road (Folly Farm Road or East Steens Road)
  • From the junction, bear right and go 0.25 miles to the power substation
  • Turn right just after the power substation and follow about 2 miles the dirt road which parallels the power lines
  • Turn left and continue 0.9 miles to the first gate - open and close the gate.
  • Go next 0.5 miles to the second gate.

From this point, the road is closed to all motor vehicles. Park your car and walk 0.5 miles to Borax Lake. Borax Hot Springs are located northwest of Borax Lake.

GPS: N 42°19.642' W 118°36.265' | 42.3274, -118.6044

Navigation Link***

Points of Interest Nearby
A.K. Koski, S.A. Wood The geochemistry of geothermal waters in the Alvord Basin, southeastern Oregon
United StatesDepartment of the Interior Geological Survey. Chemical and Isotopic Data for Water from Thermal Springs and Wells of Oregon. 1980.
Proposed Determination that the Borax Lake Chub is an Endangered Species, Proposal Critical Habitat, Environmental Assessment (EA) B1; Final Rule. 1982.

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