Volcanoes Volcano Definition A vent at which lava

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Volcanoes

Volcanoes

Volcano Definition - A vent at which lava, pyroclastic debris (ash and fragments of

Volcano Definition - A vent at which lava, pyroclastic debris (ash and fragments of previously solidified rock), and gas erupt. - Eruption may build a mountain around the vent. (Mountain is also called a volcano). - Anatomy of a volcano: - magma chamber at depth - a vent to the surface

Word bank: conduit, vent, crater, side vent, ash cloud, crust, magma chamber, lava

Word bank: conduit, vent, crater, side vent, ash cloud, crust, magma chamber, lava

Where do Volcanoes Occur? Divergent volcanism: 1. Mid-ocean ridges • Where plates separate under

Where do Volcanoes Occur? Divergent volcanism: 1. Mid-ocean ridges • Where plates separate under water • Creates new sea floor 2) Rifts Where plates separate on land • • e. g. , East African rift (next slide) Iceland (this slide)

Great African Rift Valley • Bbb

Great African Rift Valley • Bbb

Mid Ocean Ridge It is thought that the Great Rift Valley will eventually become

Mid Ocean Ridge It is thought that the Great Rift Valley will eventually become an ocean.

Where do Volcanoes Occur? Convergent Boundaries - the majority of major volcanoes - e.

Where do Volcanoes Occur? Convergent Boundaries - the majority of major volcanoes - e. g. , the Andes, Japan, Aleutians (ring of fire)

Where do Volcanoes Occur? Hot spots - e. g. , Hawaii; Yellowstone Park

Where do Volcanoes Occur? Hot spots - e. g. , Hawaii; Yellowstone Park

Nature of lava • Characteristics of lava depend on its temperature and viscosity. –

Nature of lava • Characteristics of lava depend on its temperature and viscosity. – viscosity is a measure of the ability of a fluid to resist flow • high viscosity means thick • low viscosity means watery and fast • The higher the temperature of a lava, the lower its viscosity (i. e. , the easier it flows) • The greater the gas content, the lower the viscosity. Frothy lava flows more easily.

Types of Eruptions • Lava dominated eruptions: – Characteristic of low viscosity eruptions. –

Types of Eruptions • Lava dominated eruptions: – Characteristic of low viscosity eruptions. – If lava has low viscosity, it fountains out easily. You will see lava fountains, lakes and rivers, that flow long distances.

Low Viscosity flow fountains, lakes & rivers of lav

Low Viscosity flow fountains, lakes & rivers of lav

Types of Eruptions • Explosive eruptions: – Sticky, very viscous lava clogs up the

Types of Eruptions • Explosive eruptions: – Sticky, very viscous lava clogs up the vent. Gas (CO 2 and H 2 O) that come out of solution and make bubbles. Gas pressure builds up and the volcano explodes. – Result is a cloud of ash that blankets countryside or an ash flow that rushes down the volcano side at speeds up to 100 km/h, incinerating everything in its path. • Explosions can also occur when water gets into magma chamber and turns to steam or when part of the mountain slips away and pressure is released.

Lava Vocab • Tephra – materials that explode along with lava – Cooled chunks

Lava Vocab • Tephra – materials that explode along with lava – Cooled chunks of lava – Rocks, ash, parts of crust, etc. • Pyroclastic flow – Rapidly moving clouds of tephra mixed with hot, suffocating gases – http: //www. youtube. com/watch? v=Wbk. Po 0 Hws 0 M

Types of Volcanoes • The fissure volcano: is a long crack in the earth's

Types of Volcanoes • The fissure volcano: is a long crack in the earth's surface through which magma erupts. These cracks may form as two tectonic plates pull apart. • The shield volcano: is a broad, shallow volcanic cone, which arises because the running lava, which is fluid and hot, cools slowly.

Types of Volcanoes • The dome volcano: has a steep, convex slope from thick,

Types of Volcanoes • The dome volcano: has a steep, convex slope from thick, fastcooling lava. • The ash-cinder volcano: throws out (in addition to lava) much ash into the air. Through this the volcanic cone is built up from alternate layers of ash and cinder.

Types of Volcanoes • The composite volcano: are also built up from alternate layers

Types of Volcanoes • The composite volcano: are also built up from alternate layers of lava and ash but, besides its main crater, it has many little craters on its slope. • The caldera volcano: is an older volcano with a large crater which can be 62 miles (100 km) wide. In this crater many little new craters are formed.

Intrusive Activity • Plutons – – Intrusive igneous rock bodies formed by cooled magma

Intrusive Activity • Plutons – – Intrusive igneous rock bodies formed by cooled magma that forced its way into the crust and cooled before hitting the surface • 4 types – Batholiths and stocks – Laccoliths – Sills – Dikes

Batholiths • Large, irregularly shaped • Coarse-grained igneous rock • Common in interior of

Batholiths • Large, irregularly shaped • Coarse-grained igneous rock • Common in interior of many mountain chains

Laccoliths • Lens-shaped • Smaller than batholith • Stone Mountain, GA

Laccoliths • Lens-shaped • Smaller than batholith • Stone Mountain, GA

Sills • Magma intrudes parallel to layers of rock

Sills • Magma intrudes parallel to layers of rock

Dike • Cuts across preexisting rocks

Dike • Cuts across preexisting rocks

Pluton Review

Pluton Review