List of volcanoes in Iran

Last updated

Map all coordinates using: OpenStreetMap  
Download coordinates as: KML

This is a list of active and extinct Volcanoes in Iran.

A fumarole near the summit of Damavand, emitting sulfur Damavand Fumarole.JPG
A fumarole near the summit of Damavand, emitting sulfur
NamePhotographElevationLocationLast eruption
metersfeet Coordinates
Bazman BazmanNASA.jpg 3,60011,808 28°04′N60°00′E / 28.07°N 60.00°E / 28.07; 60.00 -
Damavand Damavand in winter.jpg 577618,945 35°57′04″N52°06′32″E / 35.951°N 52.109°E / 35.951; 52.109 Holocene,
from ca. 60 Ka
to 7 Ka [1]
Qal'eh Hasan Ali Qal'eh Hasan Ali.jpg 422513,858 29°24′N57°34′E / 29.40°N 57.57°E / 29.40; 57.57 Holocene
Sabalan Sab dalj1.JPG 490016,072 38°15′N47°55′E / 38.25°N 47.92°E / 38.25; 47.92 Holocene
Sahand SahandNASA.jpg 384412,608 37°45′N46°26′E / 37.75°N 46.43°E / 37.75; 46.43 Holocene
Sar'akhor Sarakor362511,890 Pliocene
Taftan Taftan.jpg 396913,018 28°36′N61°08′E / 28.60°N 61.13°E / 28.60; 61.13 1993
Darazu Koh-E-Darazu30259922 28°10′N60°40′E / 28.17°N 60.67°E / 28.17; 60.67 Holocene
Shahsavaran Koh-E-Savaran25008200 28°10′N59°06′E / 28.17°N 59.1°E / 28.17; 59.1 2020

See also

Related Research Articles

Olympus Mons Martian volcano, tallest point on Mars

Olympus Mons is an enormous shield volcano on Mars. The volcano has a height of over 21.9 km as measured by the Mars Orbiter Laser Altimeter (MOLA). Olympus Mons is about two and a half times Mount Everest's height above sea level. It is the largest and highest mountain and volcano of the Solar System, and is associated to the Tharsis Montes, a large volcanic region on Mars.

Mýrdalsjökull Glacier in Iceland

Mýrdalsjökull is an ice cap in the south of Iceland. It is to the north of Vík í Mýrdal and to the east of the smaller ice cap Eyjafjallajökull. Between these two glaciers is Fimmvörðuháls pass. Its peak reaches 1,493 m (4,898 ft) in height and in the year 1980 it covered an area of approximately 595 km2 (230 sq mi).

Alba Mons Martian volcano

Alba Mons is a volcano located in the northern Tharsis region of the planet Mars. It is the biggest volcano on Mars in terms of surface area, with volcanic flow fields that extend for at least 1,350 km (840 mi) from its summit. Although the volcano has a span comparable to that of the United States, it reaches an elevation of only 6.8 km (22,000 ft) at its highest point. This is about one-third the height of Olympus Mons, the tallest volcano on the planet. The flanks of Alba Mons have very gentle slopes. The average slope along the volcano's northern flank is 0.5°, which is over five times lower than the slopes on the other large Tharsis volcanoes. In broad profile, Alba Mons resembles a vast but barely raised welt on the planet's surface. It is a unique volcanic structure with no counterpart on Earth or elsewhere on Mars.

Frosty Peak Volcano Volcano in Alaska, United States

Frosty Peak Volcano, also known as Mt. Frosty, Frosty Volcano, or Cold Bay Volcano, is a 6,299 ft (1,920 m) stratovolcano at the southwest end of the Alaska Peninsula in the U.S. state of Alaska.

Pogromni Volcano is a stratovolcano on Unimak Island in the Aleutian Islands. Near it are 5 cinder cones, and a mountain called Pogromni's Sister.

Tharsis Tholus Martian volcano

Tharsis Tholus is an intermediate-sized shield volcano located in the eastern Tharsis region of the planet Mars. The volcano was discovered by the Mariner 9 spacecraft in 1972 and originally given the informal name Volcano 7. In 1973, the International Astronomical Union (IAU) officially designated it Tharsis Tholus. In planetary geology, tholus is the term for a small domical mountain, usually a volcano.

Ceraunius Tholus Martian volcano

Ceraunius Tholus is a volcano on Mars located in the Tharsis quadrangle at 24.25° north latitude and 262.75° east longitude, part of the Uranius group of volcanoes. It is 130 kilometres (81 mi) across, approximately 8,500 metres (27,887 ft) high and is named after a classical albedo feature name.

Geothermal energy is the second most used form of renewable energy in Russia but represents less than 1% of the total energy production. The first geothermal power plant in Russia, which was the first Binary cycle power station in world, was built at Pauzhetka, Kamchatka, in 1966, with a capacity of 5 MW. the first binary cycle power station The total geothermal installed capacity is 81.9 MW, with 50 MW coming from a plant at Verkhne-Mutnovsky.Two other plants were built on the Kamchatka Peninsula in 1999 and 2002. Two smaller additional plants were installed on the islands of Kunashir and Iturup in 2007. Most geothermal resources are currently used for heating settlements in the North Caucasus and Kamchatka. Half of the geothermal production is used to heat homes and industrial buildings, one third is used to heat greenhouses and 13% is used for industrial processes.

Thordarhyrna is one of seven subglacial volcanoes beneath the Vatnajokull glacier Iceland.

Irnini Mons Mons on Venus

Irnini Mons is a volcanic structure on the planet Venus, and is named after the Assyro-Babylonian goddess of cedar-tree mountains. It has a diameter of 475 km (295 mi), a height of 1.75 km (1.09 mi), and is located in Venus' northern hemisphere. More specifically, it is located in the central Eistla Regio region at in the V-20 quadrangle. Sappho Patera, a 225 km (140 mi) diameter wide, caldera-like, depression tops the summit of Irnini Mons. The primary structural features surrounding Irnini Mons are graben, seen as linear depressed sections of rock, radiating from the central magma chamber. Also, concentric, circular ridges and graben outline the Sappho Patera depression at the summit. The volcano is crossed by various rift zones, including the north-south trending Badb Linea rift, the Guor Linea rift extending to the northwest, and the Virtus Linea rift continuing to the southeast.

Karymshina is a large volcanic caldera located in the southern Kamchatka Peninsula of Russia. It was discovered in 2006 by Vladimir L Leonov and Aleksey N. Rogozin.

References

Iranian Quaternary volcanoes map by Masoud Eshaghpour: https://pangea.stanford.edu/ERE/db/WGC/papers/WGC/2015/12006.pdf