List of geysers

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Castle Geyser, Yellowstone Yellowstone Castle Geysir Edit.jpg
Castle Geyser, Yellowstone

This is an alphabetical list of notable geysers, a type of erupting hot spring:

Cold water

The following are carbon dioxide-generated cold water geysers:

See also

Related Research Articles

A caldera is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcano eruption. When large volumes of magma are erupted over a short time, structural support for the rock above the magma chamber is gone. The ground surface then collapses into the emptied or partially emptied magma chamber, leaving a large depression at the surface. Although sometimes described as a crater, the feature is actually a type of sinkhole, as it is formed through subsidence and collapse rather than an explosion or impact. Compared to the thousands of volcanic eruptions that occur each century, the formation of a caldera is a rare event, occurring only a few times per century. Only seven caldera-forming collapses are known to have occurred between 1911 and 2016. More recently, a caldera collapse occurred at Kīlauea, Hawaii in 2018.

<span class="mw-page-title-main">Geyser</span> Natural explosive eruption of hot water

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">Alpine skiing at the 2002 Winter Olympics</span>

Alpine skiing at the 2002 Winter Olympics consisted of ten events held 10–23 February in the United States near Salt Lake City, Utah. The downhill, super-G, and combined events were held at Snowbasin, the giant slaloms at Park City, and the slaloms at adjacent Deer Valley.

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

A mudpot, or mud pool, is a sort of acidic hot spring, or fumarole, with limited water. It usually takes the form of a pool of bubbling mud. The acid and microorganisms decompose surrounding rock into clay and mud.

<span class="mw-page-title-main">Geysir</span> Geyser in Iceland

Geysir, sometimes known as The Great Geysir, is a geyser in southwestern Iceland. It was the first geyser described in a printed source and the first known to modern Europeans. The English word geyser derives from Geysir. The name Geysir itself is derived from the Icelandic verb geysa. Geysir lies in the Haukadalur valley on the slopes of Laugarfjall lava dome, which is also the home to Strokkur geyser about 50 metres (160 ft) south.

<span class="mw-page-title-main">Strokkur</span> Natural geyser located in Haukadalur Valley, Iceland

Strokkur is a fountain-type geyser located in a geothermal area beside the Hvítá River in Iceland in the southwest part of the country, east of Reykjavík. It typically erupts every 6–10 minutes. Its usual height is 15–20 metres (49–66 ft), although it can sometimes erupt up to 40 metres (130 ft) high.

<span class="mw-page-title-main">Kamchatka Peninsula</span> 1,250-kilometre-long peninsula in the Russian Far East

The KamchatkaPeninsula is a 1,250-kilometre-long (777 mi) peninsula in the Russian Far East, with an area of about 270,000 km2 (104,248 sq mi). The Pacific Ocean and the Sea of Okhotsk make up the peninsula's eastern and western coastlines, respectively. Immediately offshore along the Pacific coast of the peninsula runs the 10,500-metre-deep (34,449 ft) Kuril–Kamchatka Trench.

Hidden Valley may refer to:

<span class="mw-page-title-main">Maar</span> Low-relief volcanic crater

A maar is a broad, low-relief volcanic crater caused by a phreatomagmatic eruption. A maar characteristically fills with water to form a relatively shallow crater lake, which may also be called a maar.

<span class="mw-page-title-main">Whakarewarewa</span> Suburb of Rotorua, New Zealand

Whakarewarewa is a Rotorua semi-rural geothermal area in the Taupo Volcanic Zone of New Zealand. This was the site of the Māori fortress of Te Puia, first occupied around 1325, and known as an impenetrable stronghold never taken in battle. Māori have lived here ever since, taking full advantage of the geothermal activity in the valley for heating and cooking.

<span class="mw-page-title-main">Steamboat Springs (Nevada)</span>

Steamboat Springs is a small volcanic field of rhyolitic lava domes and flows in western Nevada, located south of Reno. There is extensive geothermal activity in the area, including numerous hot springs, steam vents, and fumaroles. The residential portions of this area, located mostly east of Steamboat Creek and south of modern-day SR 341, are now known simply as Steamboat.

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

Orakei Korako is a highly active geothermal area most notable for its series of fault-stepped sinter terraces, located in a valley north of Taupō on the banks of the Waikato River in the Taupō Volcanic Zone, New Zealand. It is also known as "The Hidden Valley".

<span class="mw-page-title-main">Ōhakuri Dam</span> Dam in Rotorua, and Hamilton

The Ōhakuri Dam is a dam and hydroelectric power station on the Waikato River, central North Island, New Zealand, midway between Taupō, Rotorua and Hamilton. Its dam is about 5 kilometres (3.1 mi) upstream of the Atiamuri Dam.

<span class="mw-page-title-main">Complex volcano</span> Landform of more than one related volcanic centre

A complex volcano, also called a compound volcano or a volcanic complex, is a mixed landform consisting of related volcanic centers and their associated lava flows and pyroclastic rock. They may form due to changes in eruptive habit or in the location of the principal vent area on a particular volcano. Stratovolcanoes can also form a large caldera that gets filled in by a lava dome, or else multiple small cinder cones, lava domes and craters may develop on the caldera's rim.

<span class="mw-page-title-main">Valley of Geysers</span>

The Valley of Geysers is a geyser field on Kamchatka Peninsula, Russia, and has the second largest concentration of geysers in the world. This six-kilometre-long (3.7 mi) basin with approximately ninety geysers and many hot springs is situated on the Kamchatka Peninsula in the Russian Far East, predominantly on the left bank of the ever-deepening Geysernaya River, into which geothermal waters flow from a relatively young stratovolcano, Kikhpinych. Temperatures have been found to be 250 °C (482 °F), 500 m (1,640 ft) below the caldera ground. It is part of the Kronotsky Nature Reserve, which, in turn, is incorporated into the World Heritage Site "Volcanoes of Kamchatka". The valley is difficult to reach, with helicopters providing the only feasible means of transport.

<span class="mw-page-title-main">Kronotsky Nature Reserve</span> Strict nature reserve in Kamchatka Krai, Russia

Kronotsky (Кроноцкий) Nature Reserve is a Russian 'zapovednik' reserved for the study of natural sciences in the remote Russian Far East, on the coast of the Kamchatka Peninsula. It was created in 1934 and its current boundary contains an area of 10,990 km2 (4,240 sq mi). The largest lake in the reserve is Lake Kronotskoye, which covers an area of 246 square kilometres (95 sq mi). It also has Russia's only geyser basin, plus several mountain ranges with numerous volcanoes, both active and extinct. Due to its often harsh climate and its mix of volcanoes and geysers, it is frequently described as the Land of Fire and Ice.

Located in a geologically active region, New Zealand has numerous geothermal features, including volcanoes, hot springs, geysers and volcanic lakes. Many of these features cluster together geographically, notably throughout the central North Island's Taupō Volcanic Zone. These areas attract scientific interest and tourism; power generators, industry and civil engineering also utilise them.

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<i>Trigonia</i> Extinct genus of bivalves

Trigonia is an extinct genus of saltwater clams, fossil marine bivalve mollusk in the family Trigoniidae. The fossil range of the genus spans the Paleozoic, Mesozoic and Paleocene of the Cenozoic, from 298 to 56 Ma.

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