Geothermal areas in Lassen Volcanic National Park

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Map of the geothermal areas Geothermal areas in Lassen area.gif
Map of the geothermal areas
Lassen hydrothermal system Lassen hydrothermal system.jpg
Lassen hydrothermal system

The geothermal areas in Lassen Volcanic National Park include several groups of hot springs and fumaroles, as remnants of former volcanic activity, exist in Lassen Volcanic National Park in northeastern California. Most of these lie in or are closely adjacent to Mount Tehama's caldera. Bumpass Hell is the most spectacular of these, but others of importance are Sulphur Works, Little Hot Springs Valley, Boiling Springs Lake and Devil's Kitchen. In each thermal area, the highest temperature of water generally is close to the boiling temperature at the altitude of the particular spring or fumarole 198 °F (92 °C) at Bumpass Hell and 191 °F (88 °C) on the northwest flanks of Lassen Peak. [1] Temperatures as high as 230 °F (110 °C) have been recorded in the park.

Contents

Spring activity varies with water supply. Abundant water results in clear springs during early summer, but as the season progresses and the water supply decreases, springs change successively to turbid, warm pools, spattering mudpots, and finally steaming fumaroles. There are no true geysers within Lassen Volcanic National Park.

Gases from hot springs are composed mostly of steam and carbon dioxide, with minor amounts of other gases. These react with the rocks around the springs to ultimately form opal if temperature and acidity are high, or kaolin if they are low. Deposits of sulfur, pyrite, quartz and other substances are also found around the springs and in their runoff channels.

Solfataric alteration within the caldera of Mount Tehama covers about five square miles (13 km2), [1] much more extensive than the present hot springs basins. indicative of its former extent and suggestive of its waning activity. It is the altered materials in the caldera that yielded most readily to the forces of erosion. Diamond Peak is a body of unaltered rock that still remains, because it is more resistant.

Sulphur Works and Little Hot Springs Valley

Sulphur Works Sulpher Works in Lassen VNP-750px.JPG
Sulphur Works
Boiling mudpot, Sulphur Works

As in many hydrothermally active areas, the rocks at Sulphur Works and Little Hot Springs Valley in Lassen Volcanic National Park have been chemically altered into bright-colored clays. Sulfurous acid and sulfuric acid have broken down hard, gray-green andesite lavas into red, yellow and buff clays and iron oxides. Many visitors pass through Sulphur Works on their way north on State Route 89 and sense the rotten-egg smell (hydrogen sulfide) when they pass by a hot vent to the east of the road. Sulphur Works is said to be the volcanic center of the ancestral Mount Tehama.

Bumpass Hell

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Bumpass Hell
Boiling Pools Inside Bumpass Hell InsideBumpassHellWaterColors.JPG
Boiling Pools Inside Bumpass Hell
Photo of several hot springs at Bumpass Hell from the perspective of the boardwalk. Bumpass Hell hot springs.jpg
Photo of several hot springs at Bumpass Hell from the perspective of the boardwalk.

Near Little Hot Springs Valley is Bumpass Hell, a hydrothermally altered geothermal area that spans 16 acres (6.5 ha) and has hot springs, fumaroles, and boiling mudpots. As part of Mount Tehama's main vent, Bumpass Hell is the result of fissures that tap the volcanic heat, thought to be a cooling mass of andesite, perhaps three miles (5 km) below the surface.

It is named after Kendall Vanhook Bumpass, a cowboy and early settler who worked in the Lassen Peak area in the 1860s. Bumpass discovered the geothermal feature and was named on a mining claim for the area. In 1865 the editor of the Red Bluff Independent newspaper took a trip with Bumpass to see the locale. During this trip Bumpass broke through a thin crust above a scalding hot mudpot; his leg was badly scalded and eventually had to be amputated. [2] The area was named in his honor.

Devils Kitchen

About 7 mi (11 km) southeast of Lassen Peak is Devils Kitchen. In this geothermal area the hot springs are so acidic that they have eaten pits and holes in the bedrock.

Terminal Geyser

Terminal Geyser Terminal Geyser Lassen NP.jpg
Terminal Geyser

Located in the southeast corner of the park, Terminal Geyser is not actually a geyser, but rather a cold stream flowing over a steam vent. This is about 100 feet (30 m) from the site of a geothermal boring operation that took place in 1962 and 1978. The 4,008-foot (1,222 m) well is now plugged and abandoned.

Boiling Springs Lake

Boiling Springs Lake is acidic and very hot. The first hybrid virus was discovered here in 2012. Genetic hybrids are called "chimera", after mythological creatures like the Griffin or winged horse. Boiling Springs Lake Lassen NP.jpg
Boiling Springs Lake is acidic and very hot. The first hybrid virus was discovered here in 2012. Genetic hybrids are called "chimera", after mythological creatures like the Griffin or winged horse.

Just northwest of Terminal Geyser, large, warm-water Boiling Springs Lake has many hot springs, mudpots, and fumaroles along its west shore. Unlike the more heavily visited areas of the park, this area is not developed with boardwalks or signs and offers a chance to view thermal features in a more natural setting.

In 2012, scientists studying the viruses in Boiling Springs Lake found the first known case of a natural hybrid or "chimera" virus, apparently made of two very different groups of viruses that recombined into a single organism. [4] They named this "mythological beast of a virus" the "Boiling Springs Lake RNA−DNA Hybrid Virus" or "BSL−RDHV". [5] The study showed there is still much to learn about how viruses can evolve. [4] [6] Other types of viral hybrids have since been found elsewhere, and are called the CHIV group ("chimeric viruses"). [7]

See also

Related Research Articles

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A geyser is a spring characterized by an intermittent discharge of water ejected turbulently and accompanied by steam. As a fairly rare phenomenon, the formation of geysers is due to particular hydrogeological conditions that exist only in a few places on Earth. Generally all geyser field sites are located near active volcanic areas, and the geyser effect is due to the proximity of magma. Generally, surface water works its way down to an average depth of around 2,000 metres (6,600 ft) where it contacts hot rocks. The resultant boiling of the pressurized water results in the geyser effect of hot water and steam spraying out of the geyser's surface vent.

<span class="mw-page-title-main">Long Valley Caldera</span> Geologic depression near Mammoth Mountain, California, United States

Long Valley Caldera is a depression in eastern California that is adjacent to Mammoth Mountain. The valley is one of the Earth's largest calderas, measuring about 20 mi (32 km) long (east-west), 11 mi (18 km) wide (north-south), and up to 3,000 ft (910 m) deep.

<span class="mw-page-title-main">Fumarole</span> Volcanic opening that emits hot gases

A fumarole is a vent in the surface of the Earth or other rocky planet from which hot volcanic gases and vapors are emitted, without any accompanying liquids or solids. Fumaroles are characteristic of the late stages of volcanic activity, but fumarole activity can also precede a volcanic eruption and has been used for eruption prediction. Most fumaroles die down within a few days or weeks of the end of an eruption, but a few are persistent, lasting for decades or longer. An area containing fumaroles is known as a fumarole field.

<span class="mw-page-title-main">Geothermal areas of Yellowstone</span> Geyser basins and other geothermal features in Yellowstone National Park

The geothermal areas of Yellowstone include several geyser basins in Yellowstone National Park as well as other geothermal features such as hot springs, mud pots, and fumaroles. The number of thermal features in Yellowstone is estimated at 10,000. A study that was completed in 2011 found that a total of 1,283 geysers have erupted in Yellowstone, 465 of which are active during an average year. These are distributed among nine geyser basins, with a few geysers found in smaller thermal areas throughout the Park. The number of geysers in each geyser basin are as follows: Upper Geyser Basin (410), Midway Geyser Basin (59), Lower Geyser Basin (283), Norris Geyser Basin (193), West Thumb Geyser Basin (84), Gibbon Geyser Basin (24), Lone Star Geyser Basin (21), Shoshone Geyser Basin (107), Heart Lake Geyser Basin (69), other areas (33). Although famous large geysers like Old Faithful are part of the total, most of Yellowstone's geysers are small, erupting to only a foot or two. The hydrothermal system that supplies the geysers with hot water sits within an ancient active caldera. Many of the thermal features in Yellowstone build up sinter, geyserite, or travertine deposits around and within them.

<span class="mw-page-title-main">Mudpot</span> Hot spring, or fumarole, with limited water

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<span class="mw-page-title-main">Lassen Volcanic National Park</span> National park in California, United States

Lassen Volcanic National Park is an American national park in northeastern California. The dominant feature of the park is Lassen Peak, the largest plug dome volcano in the world and the southernmost volcano in the Cascade Range. Lassen Volcanic National Park is one of the few areas in the world where all four types of volcano can be found—plug dome, shield, cinder cone, and stratovolcano.

<span class="mw-page-title-main">Geology of the Lassen volcanic area</span> Geology of a U.S. national park in California

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<span class="mw-page-title-main">Lassen Peak</span> Active volcano in California, United States

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<span class="mw-page-title-main">Chaos Crags</span> Mountain in the Cascade range in California

Chaos Crags is the youngest group of lava domes in Lassen Volcanic National Park, California. They formed as six dacite domes 1,100-1,000 years ago, one dome collapsing during an explosive eruption about 70 years later. The eruptions at the Chaos Crags mark one of just three instances of Holocene activity within the Lassen volcanic center. The cluster of domes is located north of Lassen Peak and form part of the southernmost segment of the Cascade Range in Northern California. Each year, a lake forms at the base of the Crags, and typically dries by the end of the summer season.

<span class="mw-page-title-main">Krafla</span>

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<span class="mw-page-title-main">Kendall Vanhook Bumpass</span> American pioneer

Kendall VanHook Bumpass was a cowboy and early settler, who, in 1865, broke through the surface of a scalding hot mudpot in an active geothermal area and consequently lost a leg by amputation. The geothermal area was later named "Bumpass Hell", and is today located in Lassen Volcanic National Park in California.

<span class="mw-page-title-main">Mount Tehama</span> Eroded Andesitic stratovolcano in Northern California

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<span class="mw-page-title-main">Hveravellir</span> Volcano in Iceland

Hveravellir is a geothermal field of the Oddnýjarhnjúkur-Langjökull [ˈɔtːˌniːjarˌn̥juːkʏr̥] subglacial volcanic system in the north of Langjökull glacier.

<span class="mw-page-title-main">Geothermal activity</span> Activity resulting from underground heat

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References

  1. 1 2 NPS: Lassen Volcanic National Park, Nature & science, Volcanoes / Lava Flows
  2. Entry for "Bumpass, Kendall VanHook" at RootsWeb.com
  3. Devor, Caitlin (12 July 2012)."Scientists discover hybrid virus". Journal of Young Investigators". Retrieved 31 March 2020.
  4. 1 2 Diemer, Geoffrey S.; Stedman, Kenneth M. (11 June 2013). "A novel virus genome discovered in an extreme environment suggests recombination between unrelated groups of RNA and DNA viruses". Biology Direct . Retrieved 29 March 2020.
  5. Thompson, Helen (20 April 2012). "Hot spring yields hybrid genome: Researchers discover natural chimaeric DNA-RNA virus". Nature. Retrieved 27 March 2020.
  6. BioMed Central Limited (18 April 2012). "Could a newly discovered viral genome change what we thought we knew about virus evolution?" ScienceDaily. Retrieved March 31, 2020.
  7. Koonin, Eugene V.; Dolja, Valerian V.; and Krupovic, Mart. (May 2015)."Origins and evolution of viruses of eukaryotes: The ultimate modularity". Virology. p. 26. Retrieved March 31, 2020.

40°27′29″N121°30′06″W / 40.4581°N 121.5018°W / 40.4581; -121.5018