volcanic eruptions and other igneous activity viscosity – mobility of magma (resistance to flow)...

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Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: • temperature • composition • silica content • dissolved gases

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Page 1: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Volcanic eruptions and other igneous activity

Viscosity – mobility of magma (resistance to flow)

Factors affecting viscosity:

• temperature• composition

• silica content• dissolved gases

Page 2: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Factors affecting viscosity

Volcanic eruptions and other igneous activity

Low viscosity(high mobility)

High viscosity(low mobility)

High temp

Low temp

Low SiO2

High SiO2

Low gas content

High gas content

Page 3: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Importance of dissolved gases

Volcanic eruptions and other igneous activity

Low viscosity(high mobility)

High viscosity(low mobility)

Low violence eruption

High violence eruption

High pressure

Low gas content

High gas content

Low pressure

Page 4: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Materials extruded during an eruption

Volcanic eruptions and other igneous activity

• Lava flows• pahoehoe flows• aa flows• block lavas• pillow lavas

• Gases• Pyroclastic materials accdg to size

• ash and dust (welded tuff)• pea to walnut sized (lapilli, cinders)• blocks• bombs

• Pyroclastics accdg to texture• scoria (from basaltic magma)• pumice (from felsic magma)

Page 5: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Materials extruded during an eruption

Volcanic eruptions and other igneous activity

Lava flows – pahoehoe vs aa flows

Pahoehoe flows

Page 6: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Materials extruded during an eruption

Volcanic eruptions and other igneous activity

Lava flows – pahoehoe vs aa flows

aa flows

Page 7: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Materials extruded during an eruption

Volcanic eruptions and other igneous activity

Hardened pahoehoe flows = lava tubes

Page 8: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Materials extruded during an eruption

Volcanic eruptions and other igneous activity

Block lavas

Page 9: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Materials extruded during an eruption

Volcanic eruptions and other igneous activity

Pillow lavas

Page 10: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Materials extruded during an eruption

Volcanic eruptions and other igneous activity

Pillow lavas

The study of pillow lavas is important in reconstructing Earth’s geologic history. Can you tell why?

Page 11: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Materials extruded during an eruption

Volcanic eruptions and other igneous activity

Gases

Water vapor 70%CO2 15Nitrogen 5Sulfur dioxide 5

(low amounts of)ChlorineHydrogenArgon

Why is the study of volcanic gases very important?

Page 12: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Materials extruded during an eruption

Volcanic eruptions and other igneous activity

Gases

Page 13: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Materials extruded during an eruption

Volcanic eruptions and other igneous activity

Gases

Page 14: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Materials extruded during an eruption

Volcanic eruptions and other igneous activity

Pyroclastic materials – welded tuff

Page 15: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Materials extruded during an eruption

Volcanic eruptions and other igneous activity

Pyroclastic materials – welded tuff

Page 16: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Materials extruded during an eruption

Volcanic eruptions and other igneous activity

Pyroclastic materials – welded tuff

Page 17: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Materials extruded during an eruption

Volcanic eruptions and other igneous activity

Pyroclastic materials – welded tuff

Page 18: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Materials extruded during an eruption

Volcanic eruptions and other igneous activity

Pyroclastic materials – lapilli or cinders

From Vesuvius

Page 19: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Materials extruded during an eruption

Volcanic eruptions and other igneous activity

Pyroclastic materials – blocks

Page 20: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Materials extruded during an eruption

Volcanic eruptions and other igneous activity

Pyroclastic materials - bombs

Page 21: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Materials extruded during an eruption

Volcanic eruptions and other igneous activity

Pyroclastic materials (accdg to texture) - scoria

• Basaltic magma• Darker• Denser

Page 22: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Materials extruded during an eruption

Volcanic eruptions and other igneous activity

Pyroclastic materials (accdg to texture) - pumice

• Silica-rich magma• Lighter color• Less dense

Page 23: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Anatomy of a volcano

Volcanic eruptions and other igneous activity

Page 24: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Anatomy of a volcano - caldera

Volcanic eruptions and other igneous activity

Page 25: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Anatomy of a volcano - caldera

Volcanic eruptions and other igneous activity

Page 26: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Anatomy of a volcano - caldera

Volcanic eruptions and other igneous activity

Page 27: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Anatomy of a volcano – parasitic cones

Volcanic eruptions and other igneous activity

Page 28: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Anatomy of a volcano – fumaroles

Volcanic eruptions and other igneous activity

Page 29: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Volcano types – shield volcano

Volcanic eruptions and other igneous activity

• fluid basaltic lavas, often a few meters thick• broad, slightly domed structure• very few pyroclastic ejecta• lava tends to be more viscous as volcano matures

Page 30: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Volcano types – shield volcano

Volcanic eruptions and other igneous activity

Mauna Loa and Mauna Kea (upper white smudge) are 2 (of 5) overlapping shield volcanoes that make up Hawaii’s Big Island.

Page 31: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Volcano types – shield volcano

Volcanic eruptions and other igneous activity

Mauna Loa is over 9 km high (more than Everest’s 8.7km)

Page 32: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Volcano types – cinder cones

Volcanic eruptions and other igneous activity

• built from ejected lava fragments known as cinders or scoria• ash to walnut-sized ejecta

Page 33: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Volcano types – cinder cones

Volcanic eruptions and other igneous activity

• single eruptive episode = small cones• lava pipe is often immediately sealed with congealed lava• lava flows seldom happen; only at base, away from summit crater

Page 34: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Volcano types – composite cones

Volcanic eruptions and other igneous activity

• large, nearly symmetric structure of both lava and pyroclastic deposits• silica-rich magma travels only a short distance• gas-rich magma often produces violent eruptions

Page 35: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Volcano types – composite cones

Volcanic eruptions and other igneous activity

• steep summit with gently sloping flanks are due to lava flows• when young, lava tends to be more viscous, hence traveling farther to make a bigger base• mature volcanoes produce more viscous lava with increase the summit’s angle

Page 36: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Volcano types – hazards of composite cones

Volcanic eruptions and other igneous activity

sudden, often unexpected eruptions

Page 37: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Volcano types – hazards of composite cones

Volcanic eruptions and other igneous activity

Nuee ardente (glowing avalanches)

Page 38: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Volcano types – hazards of composite cones

Volcanic eruptions and other igneous activity

Lahar (mudflows of pyroclastic material)

Page 39: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Other volcanic landforms - Calderas

Volcanic eruptions and other igneous activity

Crater lake-type caldera

Page 40: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Other volcanic landforms - Calderas

Volcanic eruptions and other igneous activity

Hawaiian-type caldera

Page 41: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Other volcanic landforms - Calderas

Volcanic eruptions and other igneous activity

Yellowstone-type caldera

Page 42: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Other volcanic landforms – Fissure eruptions and basalt plateaus

Volcanic eruptions and other igneous activity

Fissure eruptions

Page 43: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Other volcanic landforms – Fissure eruptions and basalt plateaus

Volcanic eruptions and other igneous activity

Basalt plateaus

Page 44: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Other volcanic landforms – Lava dome

Volcanic eruptions and other igneous activity

Page 45: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Other volcanic landforms – Volcanic pipes

Volcanic eruptions and other igneous activity

Kimberlite diamond mines are volcanic pipes

Page 46: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Other volcanic landforms – Volcanic necks

Volcanic eruptions and other igneous activity

Volcanic necks are exposed pipes (erosion has long since removed the surrounding volcanic structure)

Page 47: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Intrusive igneous activity – plutons

Volcanic eruptions and other igneous activity

According to shape• Tabular• Massive

According to orientation• Discordant• Concordant

Dikes – tabular, discordantSills – tabular, concordantLaccoliths – tabular, concordantBatholiths

Page 48: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Other volcanic landforms – Dikes

Volcanic eruptions and other igneous activity

Page 49: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Other volcanic landforms – Sills

Volcanic eruptions and other igneous activity

Page 50: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Other volcanic landforms – Sills

Volcanic eruptions and other igneous activity

Page 51: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Other volcanic landforms – Sills

Volcanic eruptions and other igneous activity

Page 52: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Other volcanic landforms – Sills (columnar joints)

Volcanic eruptions and other igneous activity

Page 53: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Other volcanic landforms – Laccoliths

Volcanic eruptions and other igneous activity

Page 54: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Other volcanic landforms – Batholiths

Volcanic eruptions and other igneous activity

Page 55: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Other volcanic landforms – Batholiths (xenoliths)

Volcanic eruptions and other igneous activity

Page 56: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Other volcanic landforms – Stocks

Volcanic eruptions and other igneous activity

Stocks are smaller batholiths

Page 57: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Plate tectonics and igneous activity

Volcanic eruptions and other igneous activity

Page 58: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Igneous activity at convergent plate boundaries

Volcanic eruptions and other igneous activity

Volcanic island arcs

Page 59: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Igneous activity at convergent plate boundaries

Volcanic eruptions and other igneous activity

Page 60: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Igneous activity at convergent plate boundaries

Volcanic eruptions and other igneous activity

Continental volcanic arcs

Page 61: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Igneous activity at convergent plate boundaries

Volcanic eruptions and other igneous activity

Costa Rica coastal plains

Page 62: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Igneous activity at divergent plate boundaries

Volcanic eruptions and other igneous activity

Oceanic ridges

Page 63: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Igneous activity at divergent plate boundaries

Volcanic eruptions and other igneous activity

East African Rift

Page 64: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Intraplate igneous activity

Volcanic eruptions and other igneous activity

Mantle plume

Page 65: Volcanic eruptions and other igneous activity Viscosity – mobility of magma (resistance to flow) Factors affecting viscosity: temperature composition silica

Intraplate igneous activity

Volcanic eruptions and other igneous activity

Sahara desert volcanoes