7: Volcanoes

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56 Terms

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Volcano

A vent, hill, or mountain from which molten rock, hot rock fragments, and gases are ejected onto the Earth's surface.

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Volcanism

The process of magma rising, erupting, and forming igneous rock; can be a geological hazard, a rock-forming process, or an energy source.

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Magma

Molten rock located beneath the Earth's surface, containing dissolved gases.

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Lava

Magma that has erupted onto the Earth's surface.

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Magma Chamber

A large underground reservoir of molten rock that feeds a volcano.

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Conduit

A pipe or channel that carries magma from the magma chamber to the Earth's surface.

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Vent

Any opening at the Earth's surface through which magma or volcanic gases are emitted; can be central or on the flank (side vent).

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Crater

A bowl-shaped depression at the summit of a volcano, often surrounding the main vent.

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Caldera

A large, basin-shaped volcanic depression formed by the collapse of a volcano's summit after a massive eruption or magma chamber evacuation.

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Divergent Boundary

A tectonic plate boundary where plates move apart, typically producing mafic magma and effusive (calm) eruptions (e.g., mid-ocean ridges, continental rifts).

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Convergent Boundary

A tectonic plate boundary where plates move toward each other, involving subduction and typically producing intermediate to felsic magma and explosive eruptions.

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Transform Boundary

A tectonic plate boundary where plates slide horizontally past each other; typically lacks volcanism due to absence of magma generation.

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Mantle Plume (Hot Spot)

A localized upwelling of hot mantle material that can produce volcanism, often forming shield volcanoes, independent of plate boundaries (e.g., Hawaii).

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Effusive Eruption

A relatively gentle volcanic eruption characterized by the passive outpouring of low-viscosity lava, allowing gases to escape easily.

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Explosive Eruption

A violent volcanic eruption characterized by the fragmentation and violent ejection of magma, ash, and gases due to high-viscosity magma trapping gases.

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Viscosity

The resistance of a fluid to flow; in magma, it is primarily controlled by silica content and temperature. High silica = high viscosity.

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Mafic Magma

Magma low in silica (45-52%) and high in iron and magnesium; has low viscosity, high temperature, and leads to effusive eruptions.

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Felsic Magma

Magma high in silica (>63%) and aluminum; has high viscosity, lower temperature, and leads to explosive eruptions.

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Partial Melting

The process where only a portion of a rock melts due to heat and/or pressure change, producing magma that is more silica-rich than the source rock.

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Decompression Melting

Partial melting triggered by a decrease in pressure as mantle rock rises, commonly at divergent boundaries and hot spots.

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Flux Melting

Partial melting triggered by the addition of water (a flux) from a subducting plate, which lowers the melting point of the overlying mantle rock at convergent boundaries.

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Magmatic Differentiation

The process by which magma evolves in composition, becoming more felsic, through mechanisms like assimilation and fractional crystallization.

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Assimilation

The process where hot magma melts and incorporates surrounding country rock as it rises, changing its composition.

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Fractional Crystallization

The process where early-forming minerals (mafic) crystallize and settle out of the magma, leaving the remaining melt more silica-rich.

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Shield Volcano

A broad, gently sloping volcano built by many layers of low-viscosity basaltic lava flows; typical of divergent boundaries and hot spots (e.g., Mauna Loa).

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Stratovolcano (Composite Volcano)

A steep-sided, conical volcano built by alternating layers of viscous lava flows, tephra, and pyroclastic deposits; typical of convergent boundaries (e.g., Mayon, Mt. St. Helens).

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Cinder Cone

A small, steep-sided volcano built from ejected lava fragments (scoria) that accumulate around the vent; often forms on the flanks of larger volcanoes.

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Large Igneous Province (LIP)

A massive accumulation of igneous rock, often from a brief, intense outpouring of mafic lava covering vast areas (e.g., Columbia River Basalts).

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Pyroclastic Material

Solid volcanic fragments ejected during an explosive eruption, including ash, lapilli, blocks, and bombs.

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Tephra

A general term for all pyroclastic material (solid fragments) ejected into the air during a volcanic eruption.

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Pyroclastic Density Current (PDC)

A fast-moving, ground-hugging flow of hot volcanic ash, rock fragments, and gases; includes pyroclastic flows and surges. It is the deadliest volcanic hazard.

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Lahar

A destructive volcanic mudflow or debris flow composed of a slurry of water and volcanic sediment; can occur during or long after an eruption.

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Debris Avalanche

A rapid, massive slope failure of a volcanic edifice, involving rock, soil, and volcanic debris; can trigger tsunamis if it enters water.

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Lateral Blast

A sideways-directed, low-angle explosive eruption from the flank of a volcano, often associated with dome collapse or flank failure.

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Volcanic Tsunami

A tsunami generated by volcanic activity, such as a submarine eruption, flank collapse into water, or pyroclastic flow entering the sea.

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Volcanic Gas

Gases released from magma, primarily water vapor, carbon dioxide, and sulfur dioxide, which can cause acid rain, climate effects, and health hazards.

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Vog (Volcanic Smog)

A hazy air pollutant mixture of sulfur dioxide gas and sulfate aerosols, formed by volcanic gas reacting with oxygen and moisture.

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Laze Plume

A corrosive steam plume produced when lava flows into seawater, generating hydrochloric acid gas and fine glass particles.

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Lava Dome

A steep-sided, often bulbous mound of viscous lava extruded from a volcanic vent; commonly associated with explosive eruptions.

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Fumarole

A vent that emits volcanic gases, such as steam and hydrogen sulfide, often from a persistent heat source.

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Holocene Volcano

A volcano that has been active at any time during the current Holocene Epoch (last ~11,700 years), considered potentially active.

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PHIVOLCS

The Philippine Institute of Volcanology and Seismology, the national agency responsible for monitoring volcanic and seismic activity in the Philippines.

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Permanent Danger Zone (PDZ)

A designated high-risk area around an active volcano where permanent habitation is prohibited due to constant volcanic hazards.

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Volcano Alert Level

A standardized scale used by monitoring agencies (like PHIVOLCS) to communicate the status of a volcano and recommend actions, ranging from normal to hazardous eruption.

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Pacific Ring of Fire

A major area in the basin of the Pacific Ocean where many earthquakes and volcanic eruptions occur due to the presence of numerous subduction zones.

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Island Arc

A curved chain of volcanic islands formed by subduction of one oceanic plate beneath another (ocean-ocean convergence).

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Continental Arc

A chain of volcanoes on a continental margin, formed by subduction of an oceanic plate beneath a continental plate (ocean-continent convergence).

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Basanite

A type of mafic volcanic rock; the specific composition is less critical than understanding it as a mafic, low-silica rock typical of divergent settings.

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Phreatomagmatic Eruption

An explosive eruption caused by the interaction of magma with external water (groundwater or surface water), producing fine ash and steam.

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Magmatic Eruption

An eruption driven primarily by the expansion of gases originally dissolved in the magma.

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Phreatic Eruption

A steam-driven explosion that occurs when groundwater is superheated by magma, ejecting old rock but no new magma.

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Pyroclastic Fall

The settling of tephra (ash, lapilli) from an eruption column under gravity, affecting downwind areas.

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Ballistic Projectile

Large, solid rock fragments (blocks and bombs) ejected on parabolic trajectories near the volcanic vent during an explosion.

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Ground Deformation

The swelling, subsidence, or cracking of the ground around a volcano due to magma movement, often a precursor to eruption.

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Secondary Explosion

An explosion caused by the interaction of hot volcanic deposits (like a recent lava flow) with water, generating new ash clouds or small PDCs.

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