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Aside from geologists, nobody really has anything good to say about volcanos… I know I certainly didn’t: They’re slow and kind of lame, fat and blobby… Or so i thought. As it turns out I just knew very little about the magma-makers. Volcanos can actually be pretty exciting… At least according to NOVA Beta. Here’s the anatomical breakdown by NOVA’s Lexi Krock:

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There are many different kinds of volcanoes, ranging from the Hawaiian type, which produces gentle, effusive eruptions that tourists can observe from mere steps away, to the andesitic variety, which can produce violent, life-threatening eruptions with little warning. Though volcanologists study all types of volcanoes, the latter kind is of greatest concern since it is capable of killing thousands of people, destroying entire cities and forests, and severely disrupting local economies.

Many volcanoes famous for their destructive power, including Mt. St. Helens, Galeras, Nevado del Ruiz, and Mt. Vesuvius, are andesitic volcanoes. Below, get to know the major features and products of an andesitic volcano, which forms when two tectonic plates rub against each other and generate enough friction and heat to create magma from melted rock. This magma surges through the surface of the earth, then solidifies, resulting over time in a classic volcano cone.

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1. ASH
Volcanic ash consists of rock, mineral, and volcanic glass fragments smaller than a tenth of an inch in diameter—or slightly larger than a pinhead. Volcanic ash is quite different from the soft, fluffy ash that results from burning wood, leaves, or paper. It is hard, does not dissolve in water, and can be extremely small—ash particles less than 1/1,000th of an inch in diameter are common. It is also extremely abrasive (similar to finely crushed window glass), mildly corrosive, and electrically conductive, especially when wet.

Volcanic ash is created during explosive eruptions by the shattering of solid rocks and the violent separation of magma into tiny pieces. Explosive eruptions result when groundwater heated by magma abruptly converts to steam and also when magma reaches the surface so that volcanic gases dissolved in the molten rock expand and escape into the air extremely rapidly. Hot ash and gas rise quickly to form a towering eruption column directly above the volcano.

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2. LAVA FLOW
Lava flows are masses of magma that pour onto the Earth’s surface during an effusive eruption; they include both moving lava and the resulting solidified deposits. Lava flows come in a great variety of shapes and sizes. This is due to the wide range in lava discharge during eruptions, characteristics of the erupting vent and topography over which lava travels, and viscosity of the different lava types.

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3. LAVA DOME
Lava domes are rounded, steep-sided mounds built by magma that is highly resistant to flow, usually either dacite or rhyolite. Such magmas are typically too viscous to move far from the vent before cooling and crystallizing. Domes may consist of one or more individual lava flows.

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An aerial view of the 600-foot lava dome in the crater of Washington’s Mt. St. Helens, as seen between the May and July eruptions in 1980. Enlarge
Photo credit: USGS

4. LAVA
Lava is the word for magma when it erupts onto the Earth’s surface. Geologists also use the term to describe the solidified deposits of lava flows and fragments hurled into the air by explosive eruptions (for example, lava bombs or blocks). Lava is from the Italian word for stream, which is derived from the verb lavare—to wash.

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A fast-moving lava flow from Mt. Etna in Sicily. Lava flows can also move slowly, especially as they begin to cool and develop a hard crust.
Photo credit: USGS

5. VENT
Vents are openings in the Earth’s crust from which magma and volcanic gases escape onto the ground or into the atmosphere. Vents may consist of a single, circular-shaped structure, a large elongated fissure and fracture, or a tiny ground crack. The release of volcanic gases and the eruption of molten rock result in a wide assortment of edifices, ranging from enormous shield volcanoes and calderas to fumaroles and small hornitos.

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Steam rises from a vent on Mount Asahidake, a volcano on Hokkaido, Japan.
Photo credit: USGS

6. TEPHRA
Tephra is a general term for fragments of volcanic rock and lava that are blasted into the air by explosions or carried upward by hot gases in eruption columns or lava fountains. Tephra includes large, dense blocks and bombs, and small, light rock debris such as scoria, pumice, reticulite, and ash.

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A fountain of hot lava and tephra erupts from a crater in Hawaii’s Kilauea East Rift in 1983. Enlarge
Photo credit: USGS

7. CALDERA
A caldera is a large, usually circular depression at the summit of a volcano formed when magma is withdrawn or erupted from a shallow underground magma reservoir. The removal of large volumes of magma may result in loss of structural support for the overlying rock, thereby leading to collapse of the ground and formation of a large depression. Calderas are different from craters, which are smaller, circular depressions created primarily by explosive excavation of rock during eruptions.

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Mount Aso vents a large cloud of steam at Japan’s Aso National Park. The mountain’s caldera is one of the world’s largest.
Photo credit: USGS

8. LAHAR
Lahar is an Indonesian word for a rapidly flowing mixture of rock debris and water that originates on the slopes of a volcano. Lahars are also referred to as volcanic mudflows or debris flows. They form in a variety of ways, chiefly from the rapid melting of snow and ice by pyroclastic flows, intense rainfall on loose volcanic rock deposits, the breakout of a lake dammed by volcanic deposits, and as a consequence of debris avalanches.

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A lahar from the Unzen Volcano eruption in Kyushu, Japan tore through this street in Shimabara, destroying cars and homes in the process.
Photo credit: © Corbis

9. FISSURE
On volcanoes, a fissure is an elongated fracture or crack at the surface from which lava erupts. Fissure eruptions typically dwindle to a central vent after a period of hours or days. Occasionally, lava will flow back into the ground by pouring into a crack or an open eruptive fissure, a process called drainback; sometimes lava will flow back into the same fissure from which it erupted.

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A close-up of a crack in the volcanic surface of a cooled lava flow from the crater of Mt. St. Helens.
Photo credit: © Corbis

10. DIKE
Dikes are tabular or sheet-like bodies of magma that cut through and across the layering of adjacent rocks and then solidify. They form when magma rises into a fracture or creates a new crack by forcing its way through rock. Hundreds of dikes can invade the cone and inner core of a volcano, often along zones of structural weakness.

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An exposed dike, approximately five feet wide, at the caldera of Mauna Loa Volcano in Hawaii.
Photo credit: USGS

11. MAGMA
Magma is molten or partially molten rock beneath the Earth’s surface. When magma erupts onto the surface, it is called lava. Magma typically consists of a liquid portion (often referred to as the melt); a solid portion made of minerals that crystallized directly from the melt; solid rocks incorporated into the magma from along the conduit or reservoir, called xenoliths or inclusions; and dissolved gases. Magma collects inside a volcano’s magma chamber before it erupts (see diagram).

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