the magma chamber is the place where molten rock collects
Volcanoes are ruptures, vents, or fissures on the crust of a planetarymassobject that allow lava, ash, and gases to escape from a magma chamber below the surface
Volcanology, also known as vulcanology, is the studyofvolcanoes
Vulcano is a volcanic island in the Aeolian Islands of Hawaii
Vulcan is the god of fire in Roman mythology
The Earth's crust is broken into 17 major tectonic plates
Cryovolcanoes are ice volcanoes found particularly on some moons of Jupiter, Saturn, and Neptune
MudVolcanoes are formations not often associated with magmatic activity
Types of Boundaries in Plate Tectonics:
TransformBoundary: plates slide past each other, e.g., San Andreas Fault
ConvergentBoundary: two plates move toward each other, e.g., Pacific Ring of Fire or Mount Etna
DivergentBoundary: region where crustal plates move apart, e.g., Mid-Ocean Bridge, Black Smokers, or Iceland
Oceanic Plate Boundary: one plate is pushed or subducted under the other
Plate tectonics involve pieces of the Earth's crust and uppermost mantle, together referred to as the lithosphere
Adiabatic Expansion is the release of pressure due to the pull of tectonicplates
Blacksmokers are deep-sea vents
Subduction or Convergent Zones are places where two plates collide
Flux Melting occurs when water lowers the melting temperature of the overlying mantle wedge, creating magma
Hotspots are volcanic areas formed by mantle plumes
Mantle Plumes are columns of hot material rising from the core-mantle boundary in a fixed space, causing large-volume melting, e.g., Hawaiian Islands, Snake River Plain with the Yellowstone Caldera
Oceanic Plates are plates located under the ocean
Spreading occurs when two plates move away from each other and new crust is created
Subduction happens when two plates collide, and one plate dives beneath the other, ending up being destroyed in the mantle
Intrusion: magma that cools beneath the surface of a volcano without erupting
Volcanism: transportation mechanism of heat extrusion through the surface
Asthenosphere: top part of the Earth's mantle containing elements such as uranium and thorium
Extrusion: magma that cools at the surface of a volcano causing it to grow on the outside
Magma: molten rocks under the lithosphere
Lava: when magma reaches the Earth's surface, it becomes liquid rock
Tephra: boulders or dust belched forth by cinder cones
Volcanologists: people who study volcanoes
PHIVOLCS: Philippine Institute of Volcanology and Seismology
Magma Chamber or Magma Reservoir: cavity in the lower layers of the crust
Parasitic Cone: small cone-shaped volcano formed by an accumulation of volcanic debris
Sill: flat piece of rock formed when magma hardens in a crack in a volcano
Vent: opening in Earth's surface through which volcanic materials escape
Flank: the side of a volcano
Crater: mouth of the volcano that surrounds a volcanic vent
Conduit: underground passage where magma travels through
Summit: highest point of a volcano; apex
Throat: entrance of a volcano that ejects lava and volcanic ash
Ash: fragments of lava or rock blasted into the air by volcanic explosions
Ash cloud: cloud of ash formed by volcanic explosions