Geological Terms
- aftershocks
- smaller earthquakes following a large earthquake in the same area
- compressed/ compression
- crust is pushed together and folded
by great forces in the earth's crust
- continental shelf
- land under water at the edge of a continent
- depressed
- an area of land is pushed
downward from its original position
- displacement
- movement of the Earth's crust in relation to
where it was originally,
can be sideways or up and down
- duration
- the amount of time between first feeling the ground shake
and the time it stops shaking during an earthquake
- epicenter
- the point on the Earth's surface directly above where the earthquake occured
- fault
- a crack in the ground along which one or both of the sides have moved
either up, down, or sideways past each other
- fiord (fjord)
- U-shaped valley is carved to the sea during ice ages,
and later flooded with water to form huge canals.
- focus
- place in the earth where the earthquake started
- glacial deposits
- soil, rocks and clays that were left
behind by a glaciar
- hinge line
- a line of that does not move up or down which
separates the areas of an
earthquake that subsided from those that were uplifted
- intensity (of earthquakes)
- a way to measure earthquakes by the
amount of ground shaking felt, damage done to buildings,
and changes seen in the earth's surface
- isoseismal intensity lines
- lines drawn on a map telling where the edges of areas
that
had the same amount of shaking during an earthquake are
- island arc
- a chain of islands formed above the place where two
of the Earth's plates meet
- liquefaction (of soil)
- when sand and soil act like a
thick liquid during an earthquake
- magnitude (of earthquakes)
- a measure of the size of an earthquake on a
scale of 1 to 10.
Each number means the earthquake was ten times worse
than an
earthquake with the next lowest number.
- normal fault
- a fault in which one side of the rock
has moved downward
- paleosiesmology
- study of earthquakes that happened before
people started to record them
- plate (tectonic)
- a huge section of the Earth's surface which slowly
moves. The edges of plates scraping
together causes earthquakes
- quick clay
- a type of clay formed by glaciers
that loses its shape when shaken
- reverse fault
- a fault in which one side of the rock moves
up and over the other side
- runup height
- the height of the water level greater than normal
when a tsunami runs up on land along a coast
- rupture
- the Earth's crust breaks
- seiche
- a sloshing of water back and forth in a
small body of water, like in a bathtub
- slump
- a large area of land slides off a hillside
- subducted
- one plate is pulled under another at a
plate boundary,
causing earthquakes, melting, volcanoes, and mountains
- subsidence
- an area of land sinks
- surge
- a great rush of large volumes of water
- tension
- the earth's crust is stretched in opposite directions
- topography
- shape of land, under water or above it
- tsunami
- an open ocean wave generated
by large scale motion of the sea floor
- tsunami runup
- the height above sea level to which the
tsunami wave rises above land
- uplift
- an area is pushed upward
from its original position
- vertical displacement
- land is pushed up or lowered from original position
- zone of subsidence
- the area of land that dropped lower
than its original level
Learn more about the
1964 Good Friday Great Alaskan Earthquake
Other sites of interest:
Windows to Arizona Geology
United States Geological Survey Report on
the
Alaskan quake.
Credits
With many thanks to the following sources:
Macklin, T. for
photos by his brother.
1) Bolt, B., 1993, Earthquakes. W.H.Freeman and Company.
2) Christensen, D.
http://www.aeic.alaska.edu/Seis/64quake/quake_description.html
3) Lutgens, F. and Tarbeck, E., 1995, Essentials in Geology. Prentice Hall.
4) Pipkin, B. and Trent, D., 1997, Geology and the Environment. West/Wadsworth.
5) Sokolowski, T.
http://wcatwc.gov/64quake.htm
6) United States Geological Survey.
http://wwwneic.cr.usgs.gov/neis/eqlists/USA/1964_03_28.html
Page by Nievita Bueno Hartness
Last Updated 12/06/2001
E-mail me at:
nhartnes@geo.arizona.edu