Geyser Deutsch

The combination exists in few places on Earth. Yellowstone is the largest geyser locale, containing thousands of hot springs, and approximately to geysers.

It is home to half of the world's total number of geysers in its nine geyser basins. The area was discovered and explored by Tatyana Ustinova in Approximately geysers exist in the area along with many hot-water springs and perpetual spouters.

The area was formed due to a vigorous volcanic activity. The peculiar way of eruptions is an important feature of these geysers.

Most of the geysers erupt at angles, and only very few have the geyser cones that exist at many other of the world's geyser fields.

Velikan Geyser , one of the field's largest, was not buried in the slide and has recently [ quantify ] been observed to be active. The name "El Tatio" comes from the Quechua word for oven.

The valley is home to approximately 80 geysers at present. It became the largest geyser field in the Southern Hemisphere after the destruction of many of the New Zealand geysers see below , and is the third largest geyser field in the world.

In the beginning of the 20th century, the largest geyser ever known, the Waimangu Geyser existed in this zone. It began erupting in and erupted periodically for four years until a landslide changed the local water table.

Due to the high rate of volcanic activity in Iceland, it is home to some famous geysers in the world. There are around 20—29 active geysers in the country as well as numerous formerly active geysers.

Most of the Icelandic geysers are comparatively short-lived, it is also characteristic that many geysers here are reactivated or newly created after earthquakes, becoming dormant or extinct after some years or some decades.

Two most prominent geysers of Iceland are located in Haukadalur. The Great Geysir , which first erupted in the 14th century, gave rise to the word geyser.

By , Geysir was almost dormant before an earthquake that year caused eruptions to begin again, occurring several times a day, but in , eruptions all but ceased.

Throughout much of the 20th century, eruptions did happen from time to time, usually following earthquakes. Some man-made improvements were made to the spring and eruptions were forced with soap on special occasions.

Earthquakes in June subsequently reawakened the giant for a time but it is not currently erupting regularly. Geysers are known to have existed in at least a dozen other areas on the island.

Some former geysers have developed historical farms, which benefitted from the use of the hot water since medieval times. There used to be two large geysers fields in Nevada — Beowawe and Steamboat Springs —but they were destroyed by the installation of nearby geothermal power plants.

At the plants, geothermal drilling reduced the available heat and lowered the local water table to the point that geyser activity could no longer be sustained.

Many of New Zealand's geysers have been destroyed by humans in the last century. Several New Zealand geysers have also become dormant or extinct by natural means.

The main remaining field is Whakarewarewa at Rotorua. There are various other types of geysers which are different in nature compared to the normal steam-driven geysers.

These geysers differ not only in their style of eruption but also in the cause that makes them erupt. In a number of places where there is geothermal activity, wells have been drilled and fitted with impermeable casements that allow them to erupt like geysers.

The vents of such geysers are artificial, but are tapped into natural hydrothermal systems. These so-called artificial geysers , technically known as erupting geothermal wells , are not true geysers.

The geyser erupts from the casing of a well drilled in the late 19th century. According to Dr. He had "simply opened up a dead geyser".

This is a natural hot spring that spouts water constantly without stopping for recharge. Some of these are incorrectly called geysers, but because they are not periodic in nature they are not considered true geysers.

Geysers are used for various activities such as electricity generation, heating and tourism. Many geothermal reserves are found all around the world.

The geyser fields in Iceland are some of the most commercially viable geyser locations in the world. Since the s hot water directed from the geysers has been used to heat greenhouses and to grow food that otherwise could not have been cultivated in Iceland's inhospitable climate.

Steam and hot water from the geysers has also been used for heating homes since in Iceland. In the U. There are many bodies in the Solar System where jet-like eruptions, often termed cryogeysers cryo meaning "icy cold" , have been observed or are believed to occur.

Despite the name and unlike geysers on Earth , these represent eruptions of volatiles , together with entrained dust or ice particles, without liquid.

There is no evidence that the physical processes involved are similar to geysers. These plumes could more closely resemble fumaroles.

From Wikipedia, the free encyclopedia. This article is about volcanic geysers. For CO 2 -driven geysers, see Cold-water geyser.

For other uses, see Geyser disambiguation. Hot spring characterized by intermittent discharge of water ejected turbulently and accompanied by steam.

Strokkur geyser, Iceland. Fountain Geyser erupting from the pool left and Old Faithful geyser cone geyser having mound of siliceous sinter in Yellowstone National Park erupts approximately every 91 minutes right.

Further information: Thermophile and Hyperthermophile. Main article: Valley of Geysers. Play media. Main article: El Tatio. Main article: Taupo Volcanic Zone.

Main article: Iceland. Further information: Cryovolcano. Dark streaks deposited by geysers on Triton. Jets thought to be geysers erupting from Enceladus ' subsurface.

The Cold Geyser Model — a proposed explanation for cryovolcanism [37]. Retrieved Oxford Dictionaries English. Lexico Dictionaries English.

Infobase Publishing. Museum of Unnatural Mystery. Archived from the original on November 16, Proceedings World Geothermal Congress Changes in the activity of Geysir and the surrounding geysers are strongly related to earthquake activity.

In records dated , the geysers erupted so violently that the valley around them trembled. The placename "Geysir" has been first mentioned in written sources in 18th century and, as unusual natural phenomena were of high interest to the society during the Age of Enlightenment , the term became popular and has been used for similar hydrothermal features worldwide since then.

In , the research of Geysir by Robert Bunsen resulted with the explanation of the mechanism of geyser activity.

History of recent centuries shows that earthquakes have tended to revive the activity of Geysir which then subsides again in the following years.

In , it was active every 30 minutes; five years later, the time between the eruptions was as much as six hours, and in , the eruptions all but ceased.

In , a man-made channel was dug through the silica rim around the edge of the geyser vent. This ditch caused a lowering of the water table and a revival in activity.

Gradually this channel became too clogged with silica and eruptions again became rare. In , the ditch was cleared again and eruptions could be stimulated, on special occasions, by the addition of soap.

Due to environmental concerns, the practice of adding soap was seldom employed during the s. During that time, Geysir seldom erupted.

On the Icelandic National Day , authorized government geologists would force an eruption. Initially, eruptions were taking place on average eight times a day.

By July , this activity had again decreased to around three times per day. Strokkur's activity has also been affected by earthquakes, although to a lesser extent than the Great Geysir.

Due to its eruption frequency, online photos and videos of Strokkur are regularly mislabelled as depicting Geysir.

There are around thirty much smaller geysers and hot pools in the area, including one called Litli Geysir 'Little Geysir'. Descriptions of the Great Geysir and Strokkur have been given in many travel guides to Iceland published from the 18th century onwards.

Until , the Geysir area was owned by a local farmer. Initially, he erected large fences around the site and an entrance fee was charged for visitors wishing to view the geysers.

The following year, however, Craig appeared to tire of his project and gave the area as a present to a friend, E. Craig, who dropped the entrance fees.