| Term | Definition |
|
crust |
Earth's outermost layer, which varies in thickness from about 5km to 60km and is separated from the mantle by the Moho Discontinuity |
|
epicenter |
point of Earth's surface directely above an earthquake's focus |
|
focus |
in an earthquake, the point beneath Earth's surface where energy release occurs |
|
inner core |
very dense, solid center od the Earth that is made of mostly iron with smaller amounts of oxygen, silicon, sulfur, or nickel |
|
magnitude |
measure of the energy released by an earthquake |
|
mantle |
largest layer inside Earth, lying directly above the outer core and that is made mostly of silicon, oxygen, magnesium, and iron |
|
normal fault |
break in rock due to tension forces, where rock above the fault surface moves downward in relation to rock below the fault surface |
|
outer core |
liquid core that surrounds Earth's solid inner core, and that is made mostly of iron |
|
primary waves |
waves that travel outward from an Earthquake's focus and cause particles in rocks to move back and forth in the same direction the wave is moving |
|
reverse fault |
break in rock due to compression forces, where rocks above the fault surface move upward and over the rocks below the fault surface |
|
secondary waves |
waves that travel outward from an earthquke's focus and move through Earth by causing particles in rocks to vibrate at right angles to the direction of the wave |
|
seismic waves |
energy waves that are produced at and travel outward from the earthquake's focus |
|
seismograph |
device used by seimologists to record primary, secondary, suface waves from earthquakes |
|
seismologist |
scientist who studiesearthquakes and seismic waves |
|
strike-slip fault |
break in rock due to shearing forces, where rocks on either side of the fault suface move past each other with little upward or downward movement |
|
athenosphere |
plastic-like layer below the lithosphere |
|
continental drift |
hypothesis proposed by Alfred Wegener that the states that continents have moved slowly to their current locations on Earth |
|
convection current |
cycle of heating, rising, cooling, and sinking that is thought to be the force behind plate tectioncs |
|
lithosphere |
rigid, outermost layer of Earth that is about 100km thick, and is composed of the crust and part of the upper mantle |
|
pangaea |
single large landmass made up of all the continents connected together that broke apart 200 million years ago |
|
plate |
surface along which rocks break and move |
|
plate tectonics |
theory that Earth's crust and upper mantle are broken into sections that move around on a plastic-like layer of the mantle |
|
seafloor spreading |
theory that magma from below Earth's crust is forced upward toward the surface at a mid-ocean ridge, flows from the cracks as the seafloor spreads apart and bcomes solid as it cools, forming new seafloor |
|
surface waves |
waves of energy that reach Earth's surface during an earthquake, travel outward from the epicenter, and move rock particles up and down, and side to side |
|
tsunami |
powerful seismic sea wave that can travel thousands of kilometers in all directions and that begins over an earthquake focus |
|
batholith |
largest intrusive igneous rock bodies that form when magma cools underground before reaching Earth's surface |
|
caldera |
large opening formed when the top of a volcano collapes |
|
cinder cone volcano |
steep-sided volcano made of loosely packed tephra |
|
composite volcano |
a volacano formed by alternating layers of tephra and lava and that is found mostly where Earth's plates come together |
|
crater |
steep-walled depression around a volcano's vent |
|
dike |
intrusive igneous rock body formed when magma is squeezed into a vertical crack that cuts across rock layers and hardens |
|
hot spot |
location in the mantle that is hotter than any other areas and that melts rock, which is forced up toward the crust as magma |
|
shield volcano |
a broad volcano with gently sloping sides |
|
sill |
intrusive igneous rock body formed when magma is squeezed into a horizontal crack that cuts across rock layers and hardens |
|
volcanic neck |
solid, igneous core of a volcano left behind when a volacno stops erupting |
|
vent |
an opening on Earth's surface where magma is forced up and flows out as lava |
|
volcano |
opening in Earth's surface that often forms a mountain when layers of lava and volcanic ash erupt and build up |
|
earthquake |
vibrations caused by breaking rocks along faults |
|
fault |
surface along which rocks break and move |
|
tephra |
bits of rock or solified lava dropped from the air |
|
fossils |
remains or traces of a once living organism reserved by rock |
|
pertified remains |
fossils that form when some or all of the original materials that made up the organisms are replaced with minerals |
|
carbonaceous film |
fossil formed when the remains of a once living organism are subjected to heat and pressure, leaving only a thin film of carbon behind |
|
mold |
fossil formed when an organism is buried, decays, and leaves behind a hollow place in rock |
|
cast |
fossil formed when sediments fill in a mold and harden into rock |
|
index fossil |
fossil of a species that existed on Earth for only a short time, were abundant, and were widespread geographically |
|
principle of superposition |
states that for undisturbed layers of rock, older rocks lie underneath younger and younger rocks |
|
relative dating |
method to determine the order of events and relative age of rocks by examining the position of rocks in a sequence |
|
unconformity |
gaps in the rock layers due to erosion, nondeposition, or both |
|
absolute dating |
process that uses the properties of atoms in rocks and other objects to determine their exact ages, in years |
|
radioactive decay |
release of nuclear particles and energy from unstable atomic nuclei |
|
half-life |
time needed for one half-life the mass of a sample of a radioactive isotope to decay |
|
uniformitarianism |
states that Earth processes happening today are similar to those that happened in the past |
|
radioactive dating |
process to determine the absolute ages of rocks by measuring the amounts of parent and daughter materials in a rock |
| Add or remove terms from this set |