Yellowstone

Direct Use Examples in Wyoming

The historic use of geothermal resources in Wyoming is limited to direct use applications. Many native peoples used the warm springs for medicinal and spiritual reasons. The springs subsequently provided similar resources to settlers during the great westward expansion of the 1800s. Although Wyoming’s geothermal resources are still primarily used for recreation and tourism a number of direct use and electrical generation applications have been implemented in recent years.

The Jackson National Fish Hatchery uses geothermal water in their brood stock hatchery outside of Jackson Hole. Natural springs at the hatchery feed the brood stock ponds with geothermal waters. The water used at the hatchery is about 80˚F (26˚C) and flows at 100 gallons per minute (gpm). According to the Geo-heat Center, annual geothermal energy produced by the springs is about 4.9 gigawatt hours per year (GWh/yr).

A greenhouse uses warm water for heat near Lander. The well produces 98˚F (37˚C) water at 50 gpm. The heat from the geothermal water is also used to grow plants. Annually 0.6 GWh are produced from the system.

Near Thermopolis, Wyoming a residence is heated by a warm-water geothermal system. The water used to heat the residence is 124˚F (51˚C) and flows at 100 gpm. The annual geothermal energy output of the system is 0.2 GWh/yr.

The U.S. Department of Energy is currently operating a geothermal testing facility at the Rocky Mountain Oilfield Testing Center (RMOTC) near Teapot Dome in the Powder River Basin of Wyoming. The agency announced plans to sell the property (Naval Petroleum Reserve No. 3), but will continue testing at the facility until July 2014.

Geothermal Tourism In Wyoming
Tourism is the main use of geothermal resources in Wyoming. Of course Yellowstone National Park is the most well known and spectacular, however, there are a number of other publicly accessible hot springs throughout the state. These hot springs are created by high geothermal gradients close to the Earth’s surface. For hundreds of year, these hot springs have been used for recreation and relaxation. A few of the more notable public hot springs in Wyoming are detailed below.

Saratoga Hot Springs
The hot springs in Saratoga have been in use for hundreds of years. They were first “discovered” in June of 1911 and at one time the water was bottled and sold as “Radioactive Mineral Water.” However, Native Americans used the area was prior to settlers in the mid-1880s. There are five springs associated with the Saratoga Hot Springs, two of which are used to form the Saratoga Hot Springs City Park The waters of the Saratoga Hot Springs are considered to originate from Mesozoic rocks and are structurally dominated in the pathway to the surface. The largest spring in the system flows at 120 gpm and is 119˚F (48˚C).

Hot Springs State Park
In addition to Yellowstone National Park, Hot Springs State Park is another area with popular hot springs in Wyoming. The state park was created in 1937 to protect the mineral hot springs. Located in Thermopolis the park contains two commercial pools, a state bathhouse, and numerous geothermal deposits of travertine. There are several springs that make up Hot Springs State Park and numerous private springs and wells associated with the same geothermal system north of the park. Big Spring is the largest of the park’s springs flowing at 2908 gpm with a temperature of 132˚F (56˚C). Big Spring sits atop a large impressive terrace system with steps down to the Bighorn River.

Kendall Warm Springs
Located in the upper Green River Valley, Kendall Warm Springs are a small geothermal system, which flow at about 3600 gpm with water temperatures at 85.1˚F (29.5˚C). The springs formed a terrace system which isolated the Kendall Warm Springs Dace, a species of fish, off from the Green River. The dace evolved into their own species and the springs are now federally protected in order to preserve the habitat of the Dace.

Yellowstone National Park
Yellowstone National Park is made up of 3,472 square miles and 100 hot spring groups. It was designated America’s first national park in 1872, and continues to be one of the most diverse and visited national parks to this day. A total of 318 springs have temperatures over 194˚F (90˚C) and steam vents that reach 280˚F (138˚C). Nearly 100 springs produce superheated water. The entire Yellowstone geothermal system discharges 49,000 gpm. The Yellowstone geothermal system receives its energy from magma near the surface of the Yellowstone Caldera. The caldera is 28 miles (45 km) wide (East to West) and 53 miles (85km) long. Areas of the caldera have been active in the recent geologic past, rhyolitic rocks erupted 60,000 years ago and underlay all the geyser basins in the park.


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