Volcanoes

Volcano:

an openingopening in the earth’s surface through which lava, hot gases, and rock fragments erupterupt

Magma 50-100 miles below the earth’s surface slowly begins to rise to the surface

As the magma rises it melts gaps in the surrounding rock

As more magma rises a large reservoir forms as close as 2 miles below the surface (magma chamber)

How do they form?

Pressure from the surrounding rock causes the magma to blast or melt a conduit (channel) to the surface where magma erupts onto the surface through a vent (opening)

How do they form?

The magma, now called lava, builds up at the vent forming a volcano

How do they form?

Often the volcano sides will be higher than the vent forming a depression called a crater

How do they Form?

Crater:

Caldera: an unusually large crater or the remains when the cone collapses into its own magma chamber

The Birth of a Volcano

Anatomy of a VolcanoCone:

the above ground structure built from lava and/or tephra

Conduit: the path that magma takes from the magma chamber to the vent

Magma Chamber: the reservoir located under the volcano where magma collects and becomes the supply of magma/lava to build the volcano

Lava: molten, liquidliquid rock on the surface of the earth

Parasitic Cone: a smaller secondary volcano

built on the side of or near the main volcano, but sharing the same conduit to the magma chamber

Fumarole: a secondary vent that emits only gases

Fissure: a long fissure (crackcrack) from which lava flows

Vent: opening of the volcano, through which lava, ash and gases flow

Take a minute to label the parts on the diagram (not all parts are shown)

Magma chamber

conduitmantle

Parasitic Cone

Ash Cloud/Gases Vent

Lava Flow

Crater

Two factors determine the type of eruption:

Amount of water vapor & other gases in the magma

The chemical composition of the magma

Types of Volcanic Eruptions

Trapped gases under high pressure will violently explode when the magma reaches the lower pressure of the surface.

Explosive EruptionsExplosive Eruptions

Has granitic magma is very thick and plugs the vent causing the pressure to build until it blows violently out the vent

Explosive EruptionsExplosive Eruptions

Mt. St. Helens

The high water content of the magma produces more water vapor which when mixed in granitic magma produces explosive eruptions

Explosive EruptionsExplosive Eruptions

Mont serrat

Explosive Eruptions-Examples

Mt. Pinatubo

Mt. St. Helens

Mt. Fuji

Eruption of Mt. St. Helens

Low pressure gas

Quiet EruptionsQuiet Eruptions

Has basaltic magma (is more fluid and will flow instead of explode)

Quiet EruptionsQuiet Eruptions

…and has low water content

Examples: Hawaii

Quiet EruptionsQuiet Eruptions

Typical Hawaiian Eruption

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Cinder conesCinder conesoSmall base, steep-sided, loosely consolidatedoUp to 1000 feet talloLife span of a few yearsoCommonly built from gravel size lava rock fragments called cindersoViolent eruptions, dangerous when close---High pressure gas bubbles causes thick lava to explode into the air, lava begins to cool as it rises and falls becoming very stickyoWhen lava hits the ground it sticks rather than flowsoThis builds a steep cone with a small base

Cinder Cones:

Shield volcanoesShield volcanoesoLarge baseLarge base, , gentle slopegentle slope, lava rock layers, lava rock layersoA few A few milesmiles high highoLife span of a Life span of a millionmillion years or more years or moreoThe lava is hot, thin, very The lava is hot, thin, very fluidfluid often often basalticbasaltic

oExample: Example: Hawaiian Islands, IcelandHawaiian Islands, Iceland

Shield volcano on Mars; Taken from space

Take a look at these examples:http://www.volcano.si.edu/world/tpgallery.cfm?category=Shield%20Volcanoes

The Mauna Loa volcano in Hawaii—the largest volcano on Earth—has the broad expanse characteristic of shield volcanoes. It spreads across half the island of Hawaii.

Shield Volcanoes

Mauna Kea

Composite or stratoComposite or stratoLarge mountain volcano often Large mountain volcano often snow snow cappedcapped, a few miles high, a few miles high

Life span of million years or moreLife span of million years or more

Composite or stratoComposite or stratooHave alternating eruptions of Have alternating eruptions of tephratephra (air- (air-borne) and borne) and lavalava. The tephra adds . The tephra adds heightheight to the volcano and the lava to the volcano and the lava cementscements the the tephra together and adds to the tephra together and adds to the basebase. .

oFound mostly in Found mostly in subductionsubduction zones and zones and have violent eruptions.have violent eruptions.

STrato/CompositeSTrato/CompositeLlaima Volcano, Chile.

Composite (strato) Volcanoes Composite (strato) Volcanoes examples: examples:

Mt. RainierMt. Fuji

Mt. Kilimanjaro

Types of Volcanoes Review

Where do Volcanoes Occur?

Where do Volcanoes Occur?location Examples

Divergent Boundaries: where plates move APARTAPART

IcelandIceland

Where do Volcanoes Occur?location Examples

convergent Boundaries: where plates come come togethertogether

Cascade range Cascade range volcanoes, Andesvolcanoes, Andes

Cascade Volcanoes

Where do Volcanoes Occur?location Examples

Hot Spots: plates riding over plates riding over an especially hot an especially hot place in the place in the mantlemantle

Hawaii, Yellowstone, Hawaii, Yellowstone, IcelandIceland

Hot SpotsHot Spots: Formation of the Hawaiian Islands

What comes out of volcanoes?What comes out of volcanoes?

•Lava•Tephra•Gases

Lava—3 kinds:

Pahoehoe lava:

Cooler, thicker, slow moving

harden with a relatively smooth surface

Often has a ropy or wrinkled appearance

Pahoehoe lava:

Aa lava: • Hot, thin, fast

flowing• Hardens with

a rough, jagged, sharp edge surface

Pillow Lava: Lava suddenly cooled

by water shows sack-like

segments (stuffed pillows)

Can you identify the kinds of lavalava from the pictures? Circle

your choice.

Tephra Basically, rockrock fragments• Also known as pyroclasticpyroclastic rock

fragments.• There are many different possible

sizes, from very small (volcanic ashash or dustdust to much larger rocks (called volcanic bombsbombs)

Ash & dust

Volcanic Bombs

This dacite breadcrust bomb (about 15 cm in diameter) was erupted from the lava dome at Mount St. Helens, Washington.

Lahar (mudflow): mixture of ash, eroded land,

and water flowing down river valleys

Lahar (mudflow):

GASESwater vapor, carbon dioxide, nitrogen, sulfur dioxide, hydrogen sulfide, chlorine

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Active (awake): Has erupted within recent time

and can erupt again at any time. Pre-eruption activities:

Increase in earthquake activity under the cone

increase in temperature of cone, melting of ice/snow in the crater swelling of the cone steam eruptions minor ash eruptions

Volcano Activity Levels (Stages)

Mt St. Helens

Dormant (sleeping):

No eruption within recent times, but there is record of past eruptions

Can become active and erupt again after a “wake up” period

ExampleExample: Mt. Rainier

Extinct: No eruption within recorded

history Not expected to ever erupt

againExample: Mount Mazama (Crater

Lake)

Crater Lake

Mount RainierMount Rainier• The most dangerousdangerous volcano in the US• The danger is mostly from laharslahars traveling

down river valleys at a speed of 25mph and destroying everything in its path

• 100,000 people live on the solidified mudflows of previous eruptions

Mount Rainier• The mountain is dangerously unstableunstable, a

tall, steep heap of loose rock held together by the force of gravity and a cubic mile of glacier ice that could be melted or shaken loose

• Lahar flows average every 500 years500 years and have gone as far as the Puget Sound lowlands

• Mount Rainier has erupted 4 times4 times in the last 4000 years with the last eruption 200 years ago

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