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volcanoes
mountain that opens downward to a reservoir of molten rock
temperature
is directly
proportional
to pressure
Hotspot
is the area where there is active volcanism
Volcanism
releases magma through earth surface
Near
tectonic plates
are where volcanoes can be found
volcanoes
are formed through the
collision of plate boundaries
Volcano life cycle
magma invasion
building pressure
eruption
John Tuzo Wilson
he discovered
3 linear chains
of volcanoes and
submarine volcanoes
that are thousand miles apart
Hawai Emperor Seamount
most well known of the three and the youngest
Volcanic chains
are the result of the slow movement of a tectonic plate across a fixed hotspot
William Jason Morgan
proposed the existence of roughly cylindrical convective upwelling on Earth's manner
Areas with Hotspots
Hawaii
Iceland
Reunion
Galapagos
Yellowstone
Mantle plumes
columns where heat or rocks in the mantle rises
connector
Hotspot
caused by the convection of hot mantle at the mantle plume
Convection
occurs when matter such as magma circulates within Earth
Magma
is
heated
->
expands
, less dense
Active volcano signs
crater widens > magma chamber is active
frequent earthquakes
450 volcanoes
can be found in the Pacific Ring of fire
Earthquake
abrupt and violent shifting of tectonic plates
Earthquake
types of wave energy that ravel through bedrock
Hypocenter
/
Focus
origin of earthquake
Epicenter
point on the earth's surface directly above the
focus
seismic waves
surface
body
Surface waves
only travels on the surface
love
- parallel , most damaging
Rayleigh (ground roll)
- elliptical
body waves
interior of the earth, faster than surface
P waves
- travels through all types of matter , faster than
S wave
S wave
- travels only through solid
Interior
of the earth mostly made up of
liquid
and has
high
temperature
High temperature
one of the causes fir speed
Seismology
study of earthquakes
Robert Mallet
postulated that earthquakes consisted mainly of longitude motion
Pendulum
generates the movement of the frame which generates record of the vibration
Richter
determines magnitude,
8 units
Mercalli
intensity of the earthquake,
12 units
Guiseppe Mercalli
invented Mercalli in
1902
Charles F. Richter
developed Richter in 1934
Thomas C. Hanks
and
Hiroo Kanamori
developed
Moment Magnitude Scale
(
MMS
) in
1979
Types of Earthquake
Tectonic
- common
volcanic
- warning for volcanic eruptions
collapse
- caused by mining
explosion
- caused by Chemical uses
Foreshocks
small earthquakes that commonly precede a major one
Aftershocks
small earthquakes after the major one
Seiche
large water wave that moves up and down instead of forward \
fault
crack across the rocks that have been offset
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