Java Games: Flashcards, matching, concentration, and word search.

Chapter 22: Earth's Interior

AB
geologistsscientists who study Earth and the processes that have shaped Earth over time
uniformitarianismthe principle that geologic processes operating today also operated in the past
crustthe rocky outer layer of Earth
silicatesa rock made of compounds of silicon and oxygen generally containing metals such as alluminum, iron, or calcium
mantlea thick layer of hot but solid rock beneath Earth's crust
lithospherea layer of relatively cool, rigid rock that includes the uppermost part of the manlte as well as Earth's crust
asethenoshperea layer of softer, weaker rock beneath Earth's lithosphere, which can flow slowly
mesospherethe lower portion of Earth's mantle
corethe dense sphere at Earth's center, made mostly of iron and nickel
rocka solid combination of minerals or other materials
inorganica desription of a material that is not organic
streakthe color of a mineral's powder
hardnessteh resistance of a mineral to scratching
lusterthe way a mineral's surface reflects light
fractureteh way a mineral breaks, determined by the mineral's crystal structure
cleavagea mineral's tendency to split along regular, well-defined planes
igneous rockrock that forms from magma or lava
magmaa mixture of molten rock and gases, insluding water vapor,which forms underground
lavamagma that flows over Earth's surface
intrusive rockan igneous rock that forms inderground from hardened magma
extrusive rockan igneous rock that forms at Earth's surface
sedimentsmall, solid pieces of material that come from rocks or living things
sedimentary rockrock that forms over time as sediment sqeezed and cemented together
clastic rockssedimentary rocks that form from the borken fragments of other rocks
metamorphice rockrock that has been changed by temperature, pressure, or reactions with hot water.
foliated rocksa metamorphic rock with crystaks arranged in parallel bands
rock cyclea series of processes in which rocks continuously change from one type to another
plate tectonicsthe theory that pieces of Earth's lithosphere, called plates, move about slowly on top of the asthenosphere
Pangeaan acient supercontinent formed about 300 million years ago, which later gave rise to today's continents
continental driftthe process in which the continents mvoe slowly across Earth's surface
mid-ocean ridgea chain of underwater mountains
sea-floor spreadingthe process by which new oceanic crust is created at mid-ocean ridges, as older crust moves away
subductionthe process by which oceanic crust sinks into the mantle through a trench
trencha long, deep depression in the ocean floor where old oceanic crust sinks in the mantle
divergent boundarya boundary at which tectonic playes move away from each other
convergent boundarya boundary at which tectonic plates collide
transform boundarya boundary at which tectonic plates slide past each other, moving in opposit directions
earthquakea movement of Earth's crust that occurs when rocks in the crust suddenly shift, realeasing stored energy
seismic wavesvibrations that carry the energy released during an earthquake
tsunamia large sea wave generated by an underwater earthquake, volcano, or landslide
stressthe forces of deformation acting on the rocks of Earth's crust
faulta break in Earth's crust
folda bend in layers of rock
focusthe location beneath Earth's surface where an earthquake begins
epicenterthe point on Earth's surface directly above the focus of an earthquake
P wavesprimary waves; longitudinal waves caused by earthquakes
S wavessecondary waves; transverse waves caused by earthquakes
surface wavesa transverse wave that develops when a seismic wave reaches Earth's surface
seismographa device that can detect and record seismic waves
volcanoa mountain that forms when magma reaches the surface
magma chamberpocket in which magma collects before a volcanic eruption
pipea narrow vertical channel through which magma rises to Earth's surface
ventan opening in the ground where amgma escapes to Earth's surface
cratera bowl-shaped pit at the top of the central vent in a volcano



This activity was created by a Quia Web subscriber.
Learn more about Quia
Create your own activities