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Amplitude
Height of a wave
body waves
waves that travel through the interior of the earth
Cape Ann Earthquake
Happened in 1775, had a magnitude of 6.2, and its epicenter was right off Gloucester. Largest quake in colonized Boston history
divergent
type of boundary that produces shallow earthquakes, less pressure being released, causes more damage at the surface
DUCK, COVER, and HOLD ON
how do you survive an earthquake?
Earthquake
shaking of Earth's crust due to a release of energy
elastic rebound
states that as plates move past each other, friction causes them to stick together, strain builds up causing the plates to first bend, and then break. The earthquake occurs at the moment the plates break and slide past each other. ; idea created by H.F. Reid
epicenter
location along the surface directly above the focus of an earthquake
fault
a crack in the earth along which movement occurs
Fire
ground shaking can break gas lines causing _____. water lines can also break making it hard to stop the _____. Devastated the city in the 1906 San Francisco earthquake
focus
location of an earthquake, within the earth, where the waves originate
ground shaking
as plates move past one another, energy is release as waves causing
H. F. Reid
Proposed the elastic rebound theory
Inge Lehmann
Discovered the boundary between the outer and inner core of Earth.
intensity
amount of damage done to an area by an earthquake
landslides
caused when an earthquake destabilizes an already weak slope.
liquefaction
saturated material turns fluid, turning ground into a liquid like pudding, underground objects may float to the surface, soil needs to be saturated, water forces itself into rocks pushing them up. Causes Buildings sink and fall over
Love and Rayleigh
the two types of surface waves
magnitude
calculations that use data provided by seismic records to estimate the amount of energy released at the source of the earthquake concept introduced by Charles Richter in 1935 (not the scale but what does it measure)
Modified Mercalli
Earthquake scale that measure intensity, roman numeral
Mohorovicic discontinuity
aka Moho; boundary that separates the crust from the underlying mantle
Moment Magnitude
a more precise measure of earthquake magnitude than the richter scale derived from the displacement that happens along the fault line. can also be calculated from seismograms looking through long period of earthquakes.
P and S
Body waves
P wave shadow zones
exist due to the refraction of the waves band all the way around the world. refracted when they go from solid to liquid
primary (P) waves
known as a p wave or a compressional wave, it reaches the objects first because it moves the fastest and has a push pull motion. It moves things parallel to the focus and can travel through a solid, liquid, or gas.
Richter scale
1935 uses seismic records to find the approximate size of earthquakes. based on the amplitude (height) of the earthquake
S-P lag time
aka lapse time; difference in arrival time between the P and S waves
San Andreas fault
the fault between the North American and Pacific plates that causes major earthquakes in CA
secondary (S) waves
known as an s wave or shear wave, it arrives after the p wave because it moves slightly slower. It moves from side to side and is perpendicular to the focus. It can only travel through solids
seismic gap
An area along a fault where there has not been any earthquake activity for a long period of time
seismogram
the documented seismic data on paper (or digitally).
seismograph
the device used to detect the shaking of Earth's crust. records amplitude vs. time.
seismology
study of earthquake waves
Shadow Zone
Area where waves aren't received from earthquake; P waves get refracted through the core; S waves don't travel through outer or inner core
Subsidence
a geological phenomenon in which the ground in an area sinks
Surface waves
up and down motion, love and Rayleigh - types of surface wave, slowest of all waves, most dangerous
tsunami
"harbor wave" and is created when the seafloor quickly deforms and displaces overlying waves
aa
A lava flow of basaltic lava that forms rough, jagged blocks. It forms when the lava has cooled down, thus increasing the viscosity.
andesitic (intermediate)
Igneous rocks with a composition between granitic and basaltic rocks. Associated with volcanic activity.
ash
Tephra less than 2mm in diameter
assimilation
The process where magma incorporates some of the surrounding rock as it migrates upward.
basaltic (mafic)
Igneous rocks with a substantial amount of dark-colored minerals (basaltic composition)
block
Tephra that is bigger than 64mm, solid piece of side of volcano
Bombs
Ejected from a volcano while molten or semi-molten
Bowen's reaction series
The arrangement of minerals that shows at what temperatures they solidify at. Discovered at the beginning of the 12th century. Olivine is first to cool and quartz is last.
Caldera
a large crater caused by the violent explosion of a volcano that collapses into a depression
cinder cone
Volcanos built from ejected lava fragments (pyroclastic material). A product of relatively gas-rich mafic magma. They are very steep, have deep craters, and do not usually eject lava. 1000-1500 ft (small), mild eruptions, example : Paricutin, Mexico
Clinkers
broken lava blocks that fall down the from of an Aa flow
Composite (Strato) Volcano
classic volcanic shape, taller than wide, layers, Made from felsic magma, high in quartz, high in viscosity, high in gas content, violent eruptions, Example: Mt. St. Helens, Fuji, Tambora
crater
A steep-walled depression on the summit of many volcanoes. They are formed when ejected fragments of the volcano collect around the vent.
crystal settling
A process that occurs when the earlier-formed minerals are denser than the liquid portion and sink to the bottom of the magma chamber.
crystallization
The process by which magma cools and solidifies. This may occur beneath the surface or after a volcanic eruption. The slower the process, the larger the crystals.
decompression melting
melting due to a drop in confining pressure that occurs as rock rises closer to the surface
extrusive (volcanic) igneous rock
rocks that form when molten rock solidify at the surface,
felsic
light in color, high in quartz and feldspar, generated by partial melting at subduction boundaries
Fissure eruption
the eruption of magma out of a crack in the lithosphere, rather than from a single pipe or vent
Geothermal Gradient
the gradual increase in temperature with depth in the crust.
granitic composition
igneous rocks composed of light colored silicates, also known as felsic
Harry Truman
Man who refuses to leave before Mt. St. Helen's eruption. he dies in his home by Spirit Lake and a song is made for him.
hornito
A spatter cone that forms on the surface of a lava flow and looks like a big drip-castle. It develops when lava accumulates around a vent in the ground. They typically have steep sides and form pinnacles.
Hot Spot
an area where material from deep within the mantle rises and then melts, forming magma
igneous rock
the rock resulting from the cooling and crystallized magma or lava
inclusion
the other name for the xenolith, when a different type of rock is incorporated into another plutonic rock
intrusive
igneous rocks that form at depth that are only exposed through uplifting.
Kipuka
A small piece of land that is completely surrounded by lava flows
lahar
Large composite cones generate this type of mudflow, which is saturated volcanic debris that moves down the steep volcano slopes. They can form in hard rainfall or when the volcano erupts and melts snow
lapilli
Tephra between 2mm-64mm in diameter and is vesicular
lava
hot molten (or semi molten) rock that has reached the surface. Most of the gasses have escaped
lava bench
A platform created by more recent lava flows that extend over the old shoreline. They often conceal loose material and are hazardous.
lava trees
Lava surrounds the tree but does not destroy it (leaves a column of rock.)
Lava tubes
A natural conduit where lava travels under the surface of a lava flow. The tubes form by the crusting over of lava channels. (generally pahoehoe lava)
mafic
igneous rocks high in Mg and Fe, dark colored, prevalent in ocean crust
magma
hot , molten rock located under ground made of a liquid (melt), solid portion (minerals)
magmatic differentiation
The formation of one or more secondary magmas from a single parent magmas.
melt
The liquid portion of the magma body. As this hardens, it forms crystals.
mush
the crystallized rock that is on the verge of being solid
Nuee Ardente
french word for pyroclastic flow means glowing cloud
Pahoehoe
a hot, fast-moving type of lava that hardens to form smooth, ropelike coils
Partial melting
The process by which most igneous rocks melt. Since individual minerals have different melting points, most igneous rocks melt over a temperature range of a few hundred degrees. If the liquid is squeezed out after some melting has occurred, a melt with a higher silica content results.
Pele
Hawaiian goddess of the Volcanoes
Pele's Hair
A naturally spun volcanic glass thats blown away from lava formations, lava falls, or turbulent flows. Generally gold in color
pele's tears
molten lava spews up and as it falls down, it's elongated
pillow basalt
round blobs of basalt cooled in water
Pyroclastic flow
a ground- hugging avalanche of hot ash, pumice, rock fragments, and volcanic gas that rushes down the Mt. 100-400 mph, deadliest aspect of a volcanic eruption and can reach temperatures of 600-800 degrees
rift eruption
a divergent boundary on land
Ring of Fire
A narrow zone that rims the Pacific Ocean and contains most of the active continental volcanoes (composite cones.)
shield volcanoes
Broad, slightly domed volcanoes. They are formed by fluid basaltic lavas and are frown up from the ocean floor to form islands or seamounts. (An example is the Hawaiian chain.)
skylight
an opening in the roof of a lava tube
Strato Volcano
Another name fore Composite volcanoes
tephra
A general term for fragments of volcanic rock and lava that are blasted into the air (solid.)
Tree molds
Type of lava formation that is formed when lava surounds a tree, clings against it and drains away
Tsunami
Japanese word for "harbor wave", a volcanic eruptions abruptly displaces ocean water by either an explosion or landslide, Example : Krakatoa
vent
the surface opening at the top of a pipe
viscosity
a magmas resistance to flow, factors including temp and magmas chemical composition
Volatiles
gaseous components of magma dissolved in the melt. They will readily vaporize at surface pressures
Volcano
an opening in the earth's crust through which magma reaches the surface
xenolith
when a different type of rock is incorporated into another plutonic rock