Module 12 Volcanoes VOLCANOES q A volcano is

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Module 12 Volcanoes

Module 12 Volcanoes

VOLCANOES q A volcano is a vent or fissure in the Earth’s crust through

VOLCANOES q A volcano is a vent or fissure in the Earth’s crust through which molten magma, hot gases, and other fluids escape to the surface of the land or to the bottom of the sea q Eruption: Ø The escape of magmatic products from the chamber through the vent to the surface. Ø Due to gas pressure of the magma, eruption can be classified: Ø Effusive Ø Explosive Ø Combination (Composite)

Based on the vent position, volcanic eruption can be classified into: • • Central

Based on the vent position, volcanic eruption can be classified into: • • Central Eruption Fissure Eruption Side Eruption Excentric Eruption

Vent positions Central Eruption Fissure Eruption Side Eruption

Vent positions Central Eruption Fissure Eruption Side Eruption

Parts of a volcano

Parts of a volcano

Earth’s Geothermal q GEOTHERM: increase in temperature with depth in the earth q GEOTHERMAL

Earth’s Geothermal q GEOTHERM: increase in temperature with depth in the earth q GEOTHERMAL GRADIENT is the rate of change of T with depth q In upper 100 km, average geothermal gradient = 300 C km-1 q Heat source is decay of radioactive elements q This heat causes melting of rocks to form Magma

Composition of Magma q Variation in magma properties include: Ø SILICA CONTENT varies from

Composition of Magma q Variation in magma properties include: Ø SILICA CONTENT varies from 45% to 75% Ø VOLATILES (GAS CONTENT) most common gases: H 2 O vapor, CO 2, SO 2, H 2 S Ø TEMPERATURE OF ERUPTED MAGMA varies from 12000 C to about 8000 C q Variation in magma properties affect VISCOSITY of the magma

Viscosity of Magma q VISCOSITY refers to the thickness or fluidity of a liquid

Viscosity of Magma q VISCOSITY refers to the thickness or fluidity of a liquid Ø Liquid with HIGH viscosity are very thick, sticky Ø Liquid with LOW viscosity are very fluid q Effect of various properties on magma viscosity: Ø Temperature: HIGH temperature = LOW viscosity (i. e. very fluid) Ø Silica Content: HIGH silica = HIGH viscosity Ø Volatile Content: HIGH volatiles = LOW viscosity (However, high gas contents contribute to explosive eruptions)

Classification of Volcanoes

Classification of Volcanoes

Classification of Volcanoes

Classification of Volcanoes

Eruption Types due to gas pressure

Eruption Types due to gas pressure

Eruption Types HAWAIIAN-HAWAI

Eruption Types HAWAIIAN-HAWAI

Eruption Types VULCANIAN DOME - MERAPI

Eruption Types VULCANIAN DOME - MERAPI

Eruption Types VULCANIAN - SURTSEYAN

Eruption Types VULCANIAN - SURTSEYAN

Eruption Types VULCANIAN - PAPANDAYAN GAMALAMA

Eruption Types VULCANIAN - PAPANDAYAN GAMALAMA

Eruption Types PELEEAN - ST HELLENS

Eruption Types PELEEAN - ST HELLENS

Eruption Types PLINIAN PINATUBO

Eruption Types PLINIAN PINATUBO

Eruption Types PLINIAN - TAMBORA

Eruption Types PLINIAN - TAMBORA

Where do the igneous rocks form? Volcanic (extrusive) Igneous Rocks Pyroclastic Eruption, Pelean Eruption

Where do the igneous rocks form? Volcanic (extrusive) Igneous Rocks Pyroclastic Eruption, Pelean Eruption of Mount St. Helens, Washington, 1980

Where do the igneous rocks form? Volcanic (extrusive) Igneous Rocks Other Notable Pyroclastic Volcanic

Where do the igneous rocks form? Volcanic (extrusive) Igneous Rocks Other Notable Pyroclastic Volcanic Eruptions

Eruption Types STROMBOLIAN - ANAK KRAKATAU

Eruption Types STROMBOLIAN - ANAK KRAKATAU

Shield Volcanoes

Shield Volcanoes

Shield Volcanoes

Shield Volcanoes

Shield Volcanoes

Shield Volcanoes

Shield Volcanoes

Shield Volcanoes

Shield Volcanoes

Shield Volcanoes

Shield Volcanoes HOT SPOT

Shield Volcanoes HOT SPOT

Cinder Cone Volcanoes

Cinder Cone Volcanoes

Strato Volcanoes

Strato Volcanoes

Strato Volcanoes

Strato Volcanoes

Strato Volcanoes

Strato Volcanoes

Lava Dome Volcanoes

Lava Dome Volcanoes

Dome Volcanoes

Dome Volcanoes

Caldera Volcanoes The formation of Caldera

Caldera Volcanoes The formation of Caldera

Caldera Volcanoes

Caldera Volcanoes

Global Distribution of Volcanoes

Global Distribution of Volcanoes

from: http: //www. geo. lsa. umich. edu/~crlb/COURSES/270 Distribution of Volcanoes Most subduction zones are

from: http: //www. geo. lsa. umich. edu/~crlb/COURSES/270 Distribution of Volcanoes Most subduction zones are in the “Ring of Fire” (so-called because of volcanism of the Pacific)

Volcanism & Plate Tectonics Volcanism in continental Volcanism in islands arc

Volcanism & Plate Tectonics Volcanism in continental Volcanism in islands arc

Volcanism & Plate Tectonics Volcanism in Mid Oceanic Ridge Pacific Ocean

Volcanism & Plate Tectonics Volcanism in Mid Oceanic Ridge Pacific Ocean

Volcanism & Plate Tectonics Hot Spot Volcanism

Volcanism & Plate Tectonics Hot Spot Volcanism

Classification of Volcanic Environment

Classification of Volcanic Environment

Types and Zones of Volcanism

Types and Zones of Volcanism

Finally. . . Rest in Peace COLUMNAR JOINT VOLCANIC NECK

Finally. . . Rest in Peace COLUMNAR JOINT VOLCANIC NECK