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SALT

SALT 9th Science - Chp 8

QuestionAnswer
geology study of the earth
crust the earth’s outer layer of rock; thinnest beneath the oceans
oxygen the most abundant element in the earth’s crust
granite composes the portion of the earth’s crust underlying the continents
basalt composes the portion of the earth’s crust underlying the oceans
sediments deposits of sand and mineral fragments, usually laid down by water
Mohorovičić discontinuity (Moho) boundary between the crust and the mantle
mantle the middle layer of earth between the crust and the core (upper and lower mantle); like the crust, the mantle is solid rock
transition zone zone in between, where the upper mantle merges into the lower mantle
plastic rock rock in the mantle with some properties of a solid and some properties of a liquid
Gutenberg discontinuity boundary between the bottom of the mantle and the core
core the central portion of the earth’s interior (outer core seems to be liquid, and the inner core of the earth inner core is thought to be solidthought to be solid due to pressure)
plate tectonics the theory that states that the earth’s crust and upper mantle consist of huge plates that slowly drift as a result of convection currents in the mantle
theory of plate tectonics states earthquakes and volcanoes are far more likely to occur at the edges of plates
Pangaea According to the continental drift hypothesis, all the present-day continents were at one time connected into this huge land mass
fault a fracture in a rock that occurs when the rock breaks under the strain of the forces upon it
normal fault type of fault that results when rocks along one side of a fault sink vertically
strike-slip fault type of fault that results when rocks along one side of a fault move horizontally along the fault
thrust fault type of fault that results when rocks on one side of a fault move on top of the rocks on the other side
fold is formed by the bending of buckling of rocks under great force
syncline troughlike structure formed when rocks are folded downward
anticline archlike structure formed when rocks are folded upward
volcanic mountains type of mountains apparently formed when molten rock erupts from a hole in the earth’s crust
domed mountains type of mountains apparently formed when molten rock collects beneath an overlying rock layer, forcing the layer upward into a blisterlike structure
folded mountains type of mountains apparently formed when the edges of two adjacent rock layers are pushed violently together, causing the layers to buckle like a wrinkled rug
fault-block mountains type of mountains apparently formed when rocks on one side of a fault are forced upward and the rocks on the other side are forced downward
earthquake a trembling or shaking of the earth’s crust
tremor a weak earthquake (with a magnitude of less than about 3)
aftershocks small earthquakes that often follow a larger earthquake at frequent intervals for days or even months
seismology study of earthquakes
faulting the sudden movement of rock masses along a fault
elastic rebound theory states that rocks spring back to a position of little or no strain at the moment of an earthquake, causing vibrations in the earth’s crust
San Andreas fault a large, well-known strike-slip fault in western California
focus the point deep in the earth at which an earth quake begins
epicenter the point on the earth’s surface directly above the point at which an earthquake begins
P-waves (primary waves) earthquake waves consisting of a rhythmic push-pull motion in the direction of wave travel; fastest type of earthquake waves
S-waves (secondary waves) earthquake waves consisting of a rhythmic side-to-side motion that occurs at right angles to the direction of wave travel; they can produce a lot of damage to buildings
surface waves earthquake waves that travel along the earth’s surface
seismograph an instrument used to record the vibrations caused by earthquakes
Circum-Pacific belt area where about 80% of the world’s earthquakes occur
Mercalli scale a scale with 12 degrees of intensity describing and measuring the effect of an earthquake on man, man’s structures, and the earth’s surface
Richter scale the most famous scale used to measure earthquake strength, which rates earthquakes on a scale of 1 to 10
volcano an opening in the earth’s surface through which hot gases, ash, and molten rock are ejected from the earth’s interior
vent the channel in a volcano through which gases, ash, and molten rock are ejected from the earth’s interior
magma molten rock beneath the surface of the earth
volcanology the study of volcanoes and volcanic phenomena
cinder-cone volcano type of volcano consisting primarily of erupted volcanic ash and rock fragments held loosely together
shield volcano broad, gently sloping volcano built up of large quantities of highly fluid lava that harden into rock
composite volcano volcano formed partly by explosive eruptions of ash and rock fragments and partly by mild lava flows
active volcano has erupted in the last 50 years
dormant volcano has not erupted in the last 50 years, but may erupt again
extinct volcano will probably not erupt again
Ring of Fire the most important volcanic belt, a narrow zone of active volcanoes that nearly encircles the Pacific basin
ejecta any substance emitted by an active volcano
lava molten rock that flows from volcanoes
pahoehoe lava lava that hardens into a smooth-textured rock with a “ropy” appearance
aa lava lava that hardens into rough, jagged rocks with a crumbly texture
pyroclasts particles or blocks of solid volcanic ejecta
pyroclasts range in size volcanic ash, volcanic cinders, volcanic blocks, and volcanic bombs.
volcanic bomb large almond- or teardrop-shaped pyroclasts formed when lava solidifies while hurtling through the air
nuée ardent a superheated, incandescent cloud of gas and volcanic ash that flows swiftly down a volcanic slope as an avalanche
caldera a huge bowl-shaped crater in the ground more than 2 miles wide, formed by the collapse of an underground magma chamber
lava tunnel an underground tunnel formed when the surface of a large lava flow hardens before the lava beneath
igneous intrusions a mass of igneous rock beneath the earth’s surface
dike vertical, sheetlike igneous intrusion formed when magma hardens in a vertical crack or fissure
sill horizontal, sheetlike igneous intrusion formed when magma hardens in a horizontal crack or fissure
laccolith domelike igneous intrusion formed when magma bulges overlying rocks upward
batholiths an igneous intrusion similar to a loccolith but much larger; commonly forms the base of great mountain ranges
Created by: kbtarheelgirl
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