What is the largest volcano in the world? The highest volcanoes in the world

This route completely destroyed the bridges on the south side of Iceland, the most famous of which was the 900-meter bridge over the river Skedarba, which was officially opened only in the year of its destruction. Connection with the ring road number 1, which is the main artery of Iceland, was interrupted.

Although this is a serious damage, this eruption does not have a negative impact. Science is a scientific question, because the whole process is carefully controlled by glaiologists and volcanoes, a mission that is carried out directly on this site and is supported by satellite sniffing. Hot melt water flowed into the ocean with a lot of organic and inorganic material, which, in the midst of severe erosion, followed the path and deposited it in coastal areas. This will obviously have a positive effect on increasing fish populations in relation to levels of zooplankton and phytoplankton in this area.

The prepared rating is based on the height of volcanoes, measured from sea level to the top. At the end of the statement, as a curiosity, three volcanoes, which also deserve the title of "most". Volcano disc - a type of volcano wide and flattened cone with an adjacent angle of not more than 8 °. Its characteristic feature is the lack strong eruptions. Very rare and very hot lava comes out of its interior.

The largest volcanoes in the world

The lowest of the top ten volcanoes is Ata volcano. The lowest in this case definitely does not mean “low”. It is located on the border of Argentina - Chile, in the Andes. Sayama is a volcanic peak located in the Andes in Bolivia. It is considered among the extinct stratovolcanoes. Mountain is located in national park   Sayama, about 20 km from the Chilean border and about 290 km from the capital of Bolivia, the city of La Paz.

Onboard there were 11 passengers. The plane — an avalanche of snow and thick — has lurked for more than 50 years. Stratovolcano is located on the border of Argentina and the highest volcano in Chile in close proximity to the Earth is Ojos del Salado. Is - and how - in the Central Andes in Argentina, near the border with Chile.

This is mainly a volcanic complex consisting of stratovolcanoes, volcanic domes and lava flows. This is another stratovolcano from the border of Argentina and Chile, lying on the ground and Central. Its highest parts are covered with eternal snow and form the highest boundary of eternal snow. The first eruption of the volcano occurred at least 1, 5 million years ago, the last - 28 thousand years ago. However, subsequent trips confirmed that the array is somewhat lower.

It is located in the province of La Rioja in the Argentine Andes. Also called Nevados Ojos del Salado, which literally means "salty snow-covered eyes." The name comes from the huge salt deposits that in the form of lagoons or "eyes" are found inside this array. Ojos del Salado is the highest volcano on Earth. It is located in the Central Andes, on the border between Argentina and Chile. For this reason, Hoyos del Salado is considered among the inactive volcanoes. The volume of the Tamu massif is 2.5 million M³, the area of ​​which is about 300,000 square meters.

M km ². It is also one of the largest famous volcanoes   in the solar system. It turned out that, contrary to what was previously thought, the Tamus massif is an independent volcano and a complex of smaller volcanoes. Lava flows extending in different directions, originate from a single central source near the center of the massif. Tamu became extinct - its last eruption occurred about 144 million years ago.

Mauna Kea - the highest volcano

It is used for volcanoes. At the top of the volcano are astronomical observatories. Because of their very high position, they allow the study of infrared radiation and microwaves, as well as provide clear images of celestial bodies.

Mauna Loa - the highest active shield volcano

Over the past 170 years, this volcano felt 33 times. Our terrestrial volcanoes   - crumbs in giants found in different parts of the solar system. Cosmic volcanoes can spit not only lava, but also ammonia or methane. Every day, about 20 people on land are in a state of eruption, and 500 exploded in historical times. How much did it explode at the bottom of the oceans? We know, however, that the mid-ocean ridge volcanoes give up to 75 percent. annual production of magma on Earth.

Do volcanoes also exist outside our planet? Many of them have been discovered on other planets and the moons of the solar system and, probably, have also been discovered beyond its borders. So, what do we know about extraterrestrial volcanoes? Today the most famous space volcanoes   are on mars which is famous largest volcanoes   Solar system Volcanic structures — extensive lava flows and lava plateaus — cover large areas of the Red Planet.

The two main volcanic regions of Mars are Tarsis and Elysium. These include disk volcanoes close to the Earth - with gentle slopes and central calderas. Martian volcanoes, however, differ from earthly ones in their colossal proportions.

The volume of this giant is almost 100 times larger than Mauna Loa, the largest circular volcano on Earth. There are three more in the Tarsis region powerful volcanocalled Tarsis Montes: Ascray Mons, Pavonis Mons and Arsia Mons. Some scientists believe that glaciers can be found on powerful Martian volcanoes. Martian volcanoes remain inactive in historical times. The youngest lava flows are estimated at several million years. However, in the southern polar region of Mars, eruptions of geysers erupt black sand and dust during the spring thaw.

The moon is famous for its "lunar" landscape, lined with numerous impact craters. There are several volcanoes - mostly small domes, located after the so-called bright side of our satellite. In turn, the famous lunar seas are nothing but extensive floods of basalt lava.

Their corridors can be up to 10 km in diameter, which means that they would be good for building the future base of the moon. It is estimated that the moon is not volcanically active for 3 billion years. Mercury could be volcanically active in the distant past. This is evidenced by the lines of cracks on the surface of the planet and the eruption holes with a length of 25 km, from which lava erupted.

It is estimated that volcanic activity on Mercury can last a billion years, and then stop forever. Lava during real floods formed vast plateaus resembling the moon of the moon and covered large craters, of which only the edges remained. In the area of ​​the North Pole of the planet there was a powerful flow of lava. Due to this, a volcanic northern plateau was created.

Mercury volcanism ceased when the internal heat of its supply cooled, causing the planet to shrink. However, Mercury, the only rocky planet with a magnetic field, is 100 times weaker than Earth. Most of the volcanic structures were found on Venus among all the solar planets of the solar system. Among the volcanic structures present, scientists discovered disc volcanoes, extensive floods of basaltic lava, the so-called pancake domes and something similar to footed domes - similar to fake arachnids, structures called mites.

The highest volcano is the massive Maat Mons volcano with a height of 8 km with a powerful central caldera of 28 by 31 km in size, which has at least five smaller craters. It is possible that Venus is still volcanically active and that Maat Mons - active volcano. Perhaps it could be bursts of lava, gas clouds or sparkling rocks, proving the current volcanic activity on Venus.

Five lava flows were displayed and identified, which could be active in historical times. Another interesting and still inexplicable astrogeological structure of Venus is the so-called arachnoids, similar to the web. It is not yet clear how they were created, but scientists suspect that they may be strange relatives of volcanoes. Until now, 30 such structures have been identified on the surface of the planet.

The fourth largest moon of Jupiter is the most volcanically active object in the solar system. It has about 400 active volcanoes that generate clouds of sulfur and sulfur dioxide, reaching an altitude of 500 km above the surface of the moon. The cause of such intense volcanism on Io is the tidal forces caused by Jupiter, and are amplified by the gravitational interaction of two other satellites of the gas giant, namely Ganymede and Europe.

This volcano has a crater size of 30 to 20 km and can be a vast and active lake of basaltic lava. Other active volcanic structures in Io identified active eruption centers, volcanic depressions, lava flows and disk volcanoes. He sailed from the northern end of the flood of lava for 501 km, which was called Masubi Flukt.

Moons full of ice volcanoes

There are still examples of the explosive nature of Io. Lava flows from the Amirani volcano occupy an area of ​​about 620 square kilometers. It is the largest flow of lava in the entire solar system. A giant cloud of eruptions over the volcano reached an altitude of 330 km. Cryovapes emit ammonia, water or methane instead of molten rock. They are usually formed on the ice moons of gas giants. They include the moon of Jupiter - Ganymede and Europe, the moons of Saturn - Titan, Enceladus, the moon of Uranus - Miranda and the moon of Neptune - Triton. Cryovulanes can also appear on dwarf planets such as Pluto.

The cryovollans of Enceladus released water vapor, salt crystals and ice particles into space. About 100 geysers were discovered here. Cryovulanes can also appear in Europe, the moon of Jupiter. Also Titan, the largest moon of Saturn, covered with lakes and seas of liquid hydrocarbons, can have its cryovolcano. The best candidates for them are the caldera Sotra Pater, 30 km wide and 1, 7 km deep, and two mountains - Dum Mons and Erebor Mons.

Also on Pluto and its largest moon, Charon, can be cryovolcano and cryoplanets. On Pluto, potential cryovolts are located near its south pole, two mountains with an almost circular shape and deep recesses in the center. We are talking about Wright-Mons and Pikart Mons. Both of these structures are geological.