earth science ch. 10

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Aussie10  on April 17, 2011

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earth science ch. 10

Volcano
an opening in the earth's crust through which molten lava and/ or gasses erupt
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Definitions

Volcano an opening in the earth's crust through which molten lava and/ or gasses erupt
Plate boundaries places where the Earth's crust is fractured apart into seperate plates
Ocean spreading center in the middle of the ocean, underwater where plates are splitting apart
an example of an ocean spreading center is mid-atlantic ridge
rift valleys On a continent where plates are splitting apart
ex of rift valley east african rift valley
continental margins subduction zones
ex. of continental margins western coast of S. america
pacific northwest
cascade mountains
japan
hot spots isolated areas with a magma plume, located in the middle of a tectonic plate
ex. of hot spots hawaii and yellowstone
Volcanos can be different because of variations in the magma
each magma has different____,______, and ______ minerals, gasses, and viscosity
viscosity a liquid's resistance to flow
low viscosity fluid
high viscosity very thick
what affects viscosity? temperature and silica content
When the temp. of magma is higher it flows faster
when there is more silica in magma the thicker the lava
Gases can make an eruption very explosive
Basaltic magma composition is iron-rich, and low in silica and gasses
Basaltic is explosivity is rare
Basaltic magma produces Shield volcanos
Shield volcanos they are low and broad and cover large areas
An ex. of a shield volcano hawaii
Basalt magma with a higher gas content makes cinder cones
cinder cone small steep-sided volcanoes where exploding debris cools mid-air, and builds the sides of the volcanos
cinder cone usually erupt once
Andesitic magma includes 60% silica and 3-4% gases
Andesitic magma produces composite cones
composite cones large steep-sided volcano with sides made of layer of lava and erupts debris
Composite cones aka strato volcano
composite cones erupt multiple times
composite cones are very ______ and _________ explosive and dangerous
many composite cones are located on the ring of fire
ex. of composite cones are mt. fuji, mt. rainer, mt st. helens
pluton unit of rock where the magma never erupts but cools underground
batholith massive rock unit (at least 100 mi2) that cooled underground
Many plutons come together to create a batholith
Intrusive rock texture is course- grained
granite is an example of intrusive rock
Extrusive rock cools the fastest
pumice light coolered air pockets
scoria darker color, air pockets
obsidian volcanic glass
pumice, scoria, and obsidian are made of adesitic and rhyditic lava
Basalt forms at shield volcanoes, mid- ocean ridges and cinder cones
A lava flow can cool to form aa or pahoehoe
aa blocky and sharp
pahoehoe ropey texture
Caldera a depression in a volcanic mountain, caused by collapse into the empty magma chamber after eruption
how does a caldera form? 1 2 3 4 5 1. eruption occurs with many vents and cracks in the area 2. 3. eruption continues 4. volcano collapses into empty magma chambers 5. crater may become a lake
Lava flows hot lava flows down a volcanoes side
tephra fragmented broken material ejected from a volcano its usually airborne then falls around the crater
ash it must be smaller the 2mm in diameter
lahar a mixture of water and debris that results from a volcanic eruption
lahar forms when 1. 2. 3. 4. 1. heat forms an eruption melts snow or ice on volcano 2. water rushes downhill with great velocity 3. the flood can pick up debris, dirt, ash, boulders, cars, etc. 4. begins with low viscosity ends with high viscosity ( cement like)
Pyroclastic flow a cloud of hot, toxic gas that rushes downhill from a volcano extremly hot 100-800 degrees celcius
hot spots are constant upwellings of magma in the same place. the plates of the lithosphere move over hot spots over long periods of time
Kauai 4,000,000
Oahu 3,000,000
maui 1,000,000
kohala 100,000
kilauea currently errupting
the hawaiian hotspots have been active for at least 100 million years
there is evidence there are hawaiian islands in parts of the pacific
seamount a mountain that rises from the sea floor, but does not break the surface of the water
why are seamounts no longer islands it was probably once but probs got eroded away the top
The emperor seamount extends to the northwest of hawaii
Mt. St. Helens is in the cascades

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