Earth's Interior Flashcards
earth’s relatively thin rocky outer skin
Crust
How many percentage of Earth’s volume
a. Mantle
b. Core
a. 82%
b. 16%
a solid, rocky shell that extends to a depth of about 2900km.
Mantle
Composition of iron-nickel alloy with minor amounts of oxygen, silicon and sulfur
Core
the strong rigid outer layer consisting of the crust and a portion of the upper mantle
Lithosphere
has a temperature/pressure regime that results in a small amount of melting.
Asthenosphere
it is the movement of metallic core within this zone that generates Earth’s magnetic field
Outer Core
Natural geologic hazard caused by sudden and rapid movement o a large volume of rock
Earthquake
the result of rupture and slippage along fractures in Earth’s crust
Faults
Origin of an earthquake occurs at depths between 5 and 700 km
Focus
Point at the surface directly above the focus.
Epicenter
Form of elastic energy that causes vibrations in the material that transmits them.
Seismic Waves
produced by the rapid release of elastic energy stored in rock that has been deformed by differential stress. Once the strength of rock is exceeded, it suddenly ruptures, causing vibrations
Earthquakes
are smaller earthquakes that occur in the same general area during the days to years following a larger event or mainshock
Aftershocks
are earthquakes that precede larger earthquakes in the same location
Foreshock
Study of earthquake waves
Seismology
Instrument that record earthquake waves.
Seismograph
Records obtained from seismographs
Seismogram
motion is restricted to near Earth’s surface
Surface Wave
waves that travel through Earth’s interior.
Body Waves
push-pull waves, they push and pull rocks in the direction the wave is travelling.
P Wave
or
Primary Wave
“shake” the particles at right angles to their direction of travel.
S-wave
or
Secondary Wave
travel about 1.7 times faster than S waves in any solid matter
P-wave
is 10 percent slower than S waves
Surface Wave
is based on the amplitude of the largest seismic waves recorded on a seismogram.
Richter Scale
a measure of the degree of earthquake shaking at a given locale based on observed effects
Intensity
relies on data gleaned from seismic records to estimate the amount of energy released at an earthquake’s source
Magnitude
determines the strain energy released along the entire fault surface
Moment magnitude
where unconsolidated materials are saturated with water, earthquake vibrations can turn stable soil into mobile fluid
Liquefaction
large undersea earthquakes occasionally set in motion massive waves.
Tsunami