A report on Volcano

Bromo volcano in Indonesia. This country has more than 130 active volcanoes, one of which is a supervolcano, making Indonesia the country with the most active volcanoes in the world.
Cordillera de Apaneca volcanic range in El Salvador. The country is home to 170 volcanoes, 23 which are active, including two calderas, one being a supervolcano. El Salvador has earned the epithets endearment La Tierra de Soberbios Volcanes, (The Land of Magnificent Volcanoes).
Sabancaya volcano erupting, Peru in 2017
Cleveland Volcano in the Aleutian Islands of Alaska photographed from the International Space Station, May 2006
An eruption of Mount Pinatubo on June 12, 1991, three days before its climactic eruption
Fountain of lava erupting from a volcanic cone in Hawaii, 1983
Aerial view of the Barren Island, Andaman Islands, India, during an eruption in 1995. It is the only active volcano in South Asia.
Map showing the divergent plate boundaries (oceanic spreading ridges) and recent sub-aerial volcanoes (mostly at convergent boundaries)
Lakagigar fissure vent in Iceland, the source of the major world climate alteration of 1783–84, has a chain of volcanic cones along its length.
Skjaldbreiður, a shield volcano whose name means "broad shield"
Izalco volcano, the youngest volcano in El Salvador. Izalco erupted almost continuously from 1770 (when it formed) to 1958, earning it the nickname of "Lighthouse of the Pacific".
Cross-section through a stratovolcano (vertical scale is exaggerated):
Satellite images of the 15 January 2022 eruption of Hunga Tonga-Hunga Haʻapai
Pāhoehoe lava flow on Hawaii. The picture shows overflows of a main lava channel.
The Stromboli stratovolcano off the coast of Sicily has erupted continuously for thousands of years, giving rise to its nickname "Lighthouse of the Mediterranean"
Columnar-jointed basalt lava erupted from a volcano, South Penghu Marine National Park in Taiwan
Light-microscope image of tuff as seen in thin section (long dimension is several mm): The curved shapes of altered glass shards (ash fragments) are well preserved, although the glass is partly altered. The shapes were formed around bubbles of expanding, water-rich gas.
Fresco with Mount Vesuvius behind Bacchus and Agathodaemon, as seen in Pompeii's House of the Centenary
Narcondam Island, India, is classified as a dormant volcano by the Geological Survey of India
Fourpeaked volcano, Alaska, in September 2006 after being thought extinct for over 10,000 years
Mount Rinjani eruption in 1994, in Lombok, Indonesia
Shiprock in New Mexico, US
Capulin Volcano National Monument in New Mexico, US
Koryaksky volcano towering over Petropavlovsk-Kamchatsky on Kamchatka Peninsula, Far Eastern Russia
Schematic of volcano injection of aerosols and gases
Solar radiation graph 1958–2008, showing how the radiation is reduced after major volcanic eruptions
Sulfur dioxide concentration over the Sierra Negra Volcano, Galapagos Islands, during an eruption in October 2005
Comparison of major United States supereruptions (VEI 7 and 8) with major historical volcanic eruptions in the 19th and 20th century. From left to right: Yellowstone 2.1 Ma, Yellowstone 1.3 Ma, Long Valley 6.26 Ma, Yellowstone 0.64 Ma . 19th century eruptions: Tambora 1815, Krakatoa 1883. 20th century eruptions: Novarupta 1912, St. Helens 1980, Pinatubo 1991.
The Tvashtar volcano erupts a plume 330 km (205 mi) above the surface of Jupiter's moon Io.
Olympus Mons (Latin, "Mount Olympus"), located on the planet Mars, is the tallest known mountain in the Solar System.

Rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface.

- Volcano
Bromo volcano in Indonesia. This country has more than 130 active volcanoes, one of which is a supervolcano, making Indonesia the country with the most active volcanoes in the world.

121 related topics with Alpha

Overall

Tuya Lake

2 links

Tuya Lake, located in northwestern British Columbia, Canada, presumably derives its name from the presence of nearby steep-sided, flat-topped volcanoes, known as tuyas.

The north face of Mount Garibaldi rises above The Table and Garibaldi Lake in the Garibaldi Lake volcanic field.

Volcanic field

1 links

The north face of Mount Garibaldi rises above The Table and Garibaldi Lake in the Garibaldi Lake volcanic field.
Karapınar Field in Turkey
SP Crater in the San Francisco volcanic field is a cinder cone with a basalt lava flow that extends for 4 miles (6 km).
El Muweilih Crater in Sudan with natron-rich clay on the crater floor

A volcanic field is an area of Earth's crust that is prone to localized volcanic activity.

Rocks from the Bishop tuff from California, United States, uncompressed with pumice on left; compressed with fiamme on right

Ignimbrite

3 links

Type of volcanic rock.

Type of volcanic rock.

Rocks from the Bishop tuff from California, United States, uncompressed with pumice on left; compressed with fiamme on right
The caprock in this photo is the ignimbrite layer of the Rattlesnake Formation in Oregon.
Rheomorphic flow structures in a welded ignimbrite, Isle of Lipari, Italy
A block of ignimbrite
Light microscope image of a welded ignimbrite, composed of eutaxitic lapilli-tuff as seen in thin section (Long dimension is several mm). The glass shards (mostly brown) sometimes become welded together when the deposit is still hot, and can be deformed by flow and compaction about crystal fragments (clear).

Ignimbrite is the deposit of a pyroclastic density current, or pyroclastic flow, which is a hot suspension of particles and gases flowing rapidly from a volcano and driven by being denser than the surrounding atmosphere.

Elk Calf in the Valle Grande, 2012

Valles Caldera

1 links

Elk Calf in the Valle Grande, 2012
Cerro la Jara (right) in Valle Grande in winter.
Satellite image of Valles Caldera.
A mule resting in Valle Jaramillo during an endurance race; trees in the background lack lower branches due to browsing.
Exterior "town" set in Valle Grande.

Valles Caldera (or Jemez Caldera) is a 13.7 mi wide volcanic caldera in the Jemez Mountains of northern New Mexico.

Earthquake epicenters occur mostly along tectonic plate boundaries, and especially on the Pacific Ring of Fire.

Earthquake

3 links

Shaking of the surface of the Earth resulting from a sudden release of energy in the Earth's lithosphere that creates seismic waves.

Shaking of the surface of the Earth resulting from a sudden release of energy in the Earth's lithosphere that creates seismic waves.

Earthquake epicenters occur mostly along tectonic plate boundaries, and especially on the Pacific Ring of Fire.
Global plate tectonic movement
Aerial photo of the San Andreas Fault in the Carrizo Plain, northwest of Los Angeles
Comparison of the 1985 and 2017 earthquakes on Mexico City, Puebla and Michoacán/Guerrero
Collapsed Gran Hotel building in the San Salvador metropolis, after the shallow 1986 San Salvador earthquake
Magnitude of the Central Italy earthquakes of August and October 2016 and January 2017 and the aftershocks (which continued to occur after the period shown here)
The Messina earthquake and tsunami took as many as 200,000 lives on December 28, 1908, in Sicily and Calabria.
1755 copper engraving depicting Lisbon in ruins and in flames after the 1755 Lisbon earthquake, which killed an estimated 60,000 people. A tsunami overwhelms the ships in the harbor.
Damaged buildings in Port-au-Prince, Haiti, January 2010.
Ruins of the Għajn Ħadid Tower, which collapsed in an earthquake in 1856
Fires of the 1906 San Francisco earthquake
The tsunami of the 2004 Indian Ocean earthquake
Earthquakes (M6.0+) since 1900 through 2017
Earthquakes of magnitude 8.0 and greater from 1900 to 2018. The apparent 3D volumes of the bubbles are linearly proportional to their respective fatalities.
An image from a 1557 book depicting an earthquake in Italy in the 4th century BCE

Earthquakes often occur in volcanic regions and are caused there, both by tectonic faults and the movement of magma in volcanoes.

The Aeolian Islands (part of Salina, Lipari, and Vulcano) seen from space.

Aeolian Islands

1 links

The Aeolian Islands (Isole Eolie ; Ìsuli Eoli; Αιολίδες Νήσοι), sometimes referred to as the Lipari Islands or Lipari group after their largest island, are a volcanic archipelago in the Tyrrhenian Sea north of Sicily, named after the demigod of the winds Aeolus.

The Aeolian Islands (Isole Eolie ; Ìsuli Eoli; Αιολίδες Νήσοι), sometimes referred to as the Lipari Islands or Lipari group after their largest island, are a volcanic archipelago in the Tyrrhenian Sea north of Sicily, named after the demigod of the winds Aeolus.

The Aeolian Islands (part of Salina, Lipari, and Vulcano) seen from space.
View from Vulcano, Lipari in the middle, Salina at the left, Panarea at the right
Sunset at the Aeolian Islands seen from mount Dinnammare, Peloritani
Ancient temple in Salina, 1810
Stromboli in 1810, painted by Luigi Mayer
<center>Lipari</center>
<center>Panarea</center>
Filicudi
Alicudi
<center>Salina</center>
Vulcano
<center>Stromboli</center>

Its subduction underneath the Eurasian plate generates magma, which rises to the surface to form the volcanoes.

Doom Mons, one of the most reliably identified cryovolcanoes on Saturn's moon Titan

Cryovolcano

0 links

Doom Mons, one of the most reliably identified cryovolcanoes on Saturn's moon Titan
Plumes of Enceladus, feeding Saturn's E Ring, seem to arise from the "Tiger Stripes" near the south pole.

A cryovolcano (sometimes informally called an ice volcano) is a type of volcano that erupts volatiles such as water, ammonia or methane into an extremely cold environment that is at or below their freezing point.

Olivine in a peridotite weathering to iddingsite within a mantle xenolith

Ultramafic rock

3 links

Ultramafic rocks (also referred to as ultrabasic rocks, although the terms are not wholly equivalent) are igneous and meta-igneous rocks with a very low silica content (less than 45%), generally >18% MgO, high FeO, low potassium, and are composed of usually greater than 90% mafic minerals (dark colored, high magnesium and iron content).

Ultramafic rocks (also referred to as ultrabasic rocks, although the terms are not wholly equivalent) are igneous and meta-igneous rocks with a very low silica content (less than 45%), generally >18% MgO, high FeO, low potassium, and are composed of usually greater than 90% mafic minerals (dark colored, high magnesium and iron content).

Olivine in a peridotite weathering to iddingsite within a mantle xenolith
IUGS Classification diagram for intrusive ultramafic rocks based on modal percentages of mafic minerals. Green area represents typical mantle peridotite.

Volcanic ultramafic rocks are rare outside of the Archaean and are essentially restricted to the Neoproterozoic or earlier, although some boninite lavas currently erupted within back-arc basins (Manus Trough, New Guinea) verge on being ultramafic.

Satellite image of the Tibetan Plateau between the Himalyan mountains to the south and the Taklamakan Desert to the north

Plateau

0 links

Area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side.

Area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side.

Satellite image of the Tibetan Plateau between the Himalyan mountains to the south and the Taklamakan Desert to the north
The Pajarito Plateau in New Mexico is an example of a volcanic plateau.
Road to the ALMA’s Operations Support Facility and then on further to the Chajnantor Plateau at 5000 meters above sea level.

Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers.

This conical hill in Salar de Arizaro, Salta, Argentina called Cono de Arita constitutes a landform.

Landform

1 links

Natural or artificial land feature on the solid surface of the Earth or other planetary body.

Natural or artificial land feature on the solid surface of the Earth or other planetary body.

This conical hill in Salar de Arizaro, Salta, Argentina called Cono de Arita constitutes a landform.
Karst towers landforms along Lijiang River, Guilin, China

Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins.