Somma volcano

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Aerial view of Fogo Island, Cape Verde, an example of a somma volcano. The volcanic cone Pico do Fogo rises 100 m above the walls of the caldera. Ilha do Fogo aerial shot 1.jpg
Aerial view of Fogo Island, Cape Verde, an example of a somma volcano. The volcanic cone Pico do Fogo rises 100 m above the walls of the caldera.

A somma volcano, also known as a sommian, is a volcanic caldera that has been partially filled by a new central cone. The type is named after Mount Somma ("Summit"), a stratovolcano in southern Italy [1] with a summit caldera in which the upper cone of Mount Vesuvius has grown. Other examples of somma volcanoes can be found on Russia's Kamchatka Peninsula and the Kuril Islands, stretching south from Kamchatka to Hokkaidō, Japan.[ citation needed ]

Some examples of somma volcanoes are the following:

See also

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A caldera is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcanic eruption. An eruption that ejects large volumes of magma over a short period of time can cause significant detriment to the structural integrity of such a chamber, greatly diminishing its capacity to support its own roof, and any substrate or rock resting above. 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 over the course of a century, the formation of a caldera is a rare event, occurring only a few times within a given window of 100 years. Only eight caldera-forming collapses are known to have occurred between 1911 and 2018, with a caldera collapse at Kīlauea, Hawaii in 2018. Volcanoes that have formed a caldera are sometimes described as "caldera volcanoes".

<span class="mw-page-title-main">Mount Vesuvius</span> Active stratovolcano in the Gulf of Naples, Italy

Mount Vesuvius is a somma–stratovolcano located on the Gulf of Naples in Campania, Italy, about 9 km (5.6 mi) east of Naples and a short distance from the shore. It is one of several volcanoes forming the Campanian volcanic arc. Vesuvius consists of a large cone partially encircled by the steep rim of a summit caldera, resulting from the collapse of an earlier, much higher structure.

<span class="mw-page-title-main">Ring of Fire</span> Region around the rim of the Pacific Ocean where many volcanic eruptions and earthquakes occur

The Ring of Fire is a tectonic belt of volcanoes and earthquakes.

<span class="mw-page-title-main">Atlasov Island</span> Northernmost island of the Kuril islands

Atlasov Island, known in Russian as Ostrov Atlasova (Остров Атласова), or in Japanese as Araido (阿頼度島), is the northernmost island and volcano and also the highest volcano of the Kuril islands, part of the Sakhalin Oblast in Russia. The Russian name is sometimes rendered in English as Atlasova Island. Other names for the island include Uyakhuzhach, Oyakoba (Ainu) and Alaid, the name of the volcano on the island.

<span class="mw-page-title-main">Active volcano</span> Geological feature

An active volcano is a volcano that has erupted during the Holocene, is currently erupting, or has the potential to erupt in the future. A volcano that is not currently erupting but could erupt in the future is known as a dormant volcano. Volcanoes that will not erupt again are known as extinct volcanoes.

<span class="mw-page-title-main">Anak Krakatoa</span> Volcanic island in the Sunda Strait

Anak Krakatoa is a volcanic island in Indonesia. On 29 December 1927, Anak Krakatoa first emerged from the caldera formed in 1883 by the explosive volcanic eruption that destroyed the island of Krakatoa. There has been sporadic eruptive activity at the site since the late 20th century, culminating in a large underwater collapse of the volcano, which caused a deadly tsunami in December 2018. There has been subsequent activity since. Owing to its young age the island is one of several in the area that are of interest to, and the subject of extensive study by, volcanologists.

<span class="mw-page-title-main">Mount Somma</span> Summit caldera surrounding Mount Vesuvius

Mount Somma is a mountain located in the Province of Naples, in the Campania region of southern Italy. It is 1,132 metres (3,714 ft) high. It is an integral part of the Somma–Vesuvius volcanic complex and of the larger Campanian volcanic arc, which is known for its high levels of seismic and volcanic activity.

<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">Simushir</span> Island in the Kuril Islands

Simushir, meaning Large Island in Ainu, is an uninhabited volcanic island near the center of the Kuril Islands chain in the Sea of Okhotsk in the northwest Pacific Ocean. It was formerly known as Marikan.

<span class="mw-page-title-main">Kambalny</span> Stratovolcano in southern Kamchatka

Kambalny is a stratovolcano located in the southern part of the Kamchatka Peninsula, Russia. It is the southernmost active volcano of Kamchatka. It has erupted mafic rocks. It has a summit crater as well as five cinder cones on its flanks which are the source of lava flows.

<span class="mw-page-title-main">Taunshits</span> Stratovolcano in the eastern portion of the Kamchatka peninsula

Taunshits is a stratovolcano located in the eastern part of the Kamchatka Peninsula, Russia.

<span class="mw-page-title-main">Nemo Peak</span> Mountain in Russia

Nemo Peak is a stratovolcano located at the northern end of Onekotan Island, Kuril Islands, Russia. It is truncated by two nested calderas, with the cone of Nemo Peak itself rising in the southwest end of the youngest caldera and a crater lake partially filling the northeast part, named Ozero Chernoye.

<span class="mw-page-title-main">Tao-Rusyr Caldera</span> Stratovolcano with a caldera on the island of Onekotan

Tao-Rusyr Caldera is a stratovolcano located at the southern end of Onekotan Island, Kuril Islands, Russia. It has 7.5 km wide caldera formed during a catastrophic eruption less than 10,000 years ago. The waters of Kol'tsevoe Lake fill the caldera, along with a large symmetrical andesitic cone, Krenitsyn Peak, that rises as an island within the lake. This volcano was named after Captain Pyotr Krenitsyn of the Imperial Russian Navy.

Uratman is a somma volcano located at the northern end of Simushir Island, Kuril Islands, Russia. It overlooks the Brouton Bay which is contained within the crater. The volcano consists of a Pleistocene caldera which contains an andesite cone of Holocene age.

<span class="mw-page-title-main">Tyatya</span> Volcano in the Kuril Islands, Russia.

Tyatya is a volcano located in the northeastern part of Kunashir Island, Kuril Islands, Russia. It is the highest peak on the island with an elevation of 1,819 metres (5,968 ft). Tyatya is one of the finest examples anywhere in the world of a somma volcano, a stratovolcano whose summit has collapsed to form a caldera which has then been mostly refilled by a new, younger volcanic cone which rises above the caldera rim.

<span class="mw-page-title-main">Kurils Nature Reserve</span> Russian strict nature reserve in the Kuril Islands

Kurils Nature Reserve is a Russian 'zapovednik' covering the north and south portions of Kunashir Island, the largest and most southernmost of the Kuril Islands, which stretch between Hokkaido Island in Japan to the Kamchatka peninsula in the Russia Far East. It also covers two smaller islands nearby to the southeast. The area is one of the largest wintering sites for coastal seabirds. The reserve sits on a tectonically unstable location, and is one of two Russian national reserves that protects territory of active volcanoes. The reserve is situated in the Yuzhno-Kurilsky District of Sakhalin Oblast. The reserve was created in 1984, and covers an area of 65,364 ha (252.37 sq mi).

<span class="mw-page-title-main">Kamchatka Volcanic Eruption Response Team</span> Volcano research center in Russia

The Kamchatka Volcanic Eruption Response Team (KVERT) is a Russian national institution dedicated to provide information of any volcanic activity taking place on the Kamchatka Peninsula and the Kuril Islands of Russia that could become a threat to local communities and aviation. It was established in 1993 by the Far Eastern Branch of the Russian Academy of Sciences, Institute of Volcanic Geology and Seismology under cooperation with the Kamchatkan Branch of Geophysical Survey. The Alaska Volcano Observatory (AVO), United States Geological Survey (USGS) and its affiliates also provide joint efforts to the program. The KVERT website, posted in both Russian and English, allows users to view information on volcanoes in the region and monitor reports of active volcanoes. A section also provides webcameras at select locations that update regularly. Currently, around 66 active volcanoes are routinely monitored. The majority of the volcanoes on the Kuril Islands are monitored by the Sakhalin Volcanic Eruption Response Team (SVERT), which is located in Yuzhno-Sakhalinsk, but all reports of volcanic activity in the island chain are posted in joint effort on the KVERT website.

References

  1. De Simone, Girolamo Ferdinando (2014). "On the shape of Vesuvius before AD 79 (and why it should matter to modern archaeologists)". Rivista di Studi Pompeiani. 25: 201–204. ISSN   1120-3579.