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72 Cards in this Set

  • Front
  • Back
Earthquake
shaking motions and vibrations of the earth caused by large releases of energy that accompany volcanoes, explosions, and movements of Earth's bedrock along fault lines
Focus
the origin of an earthquake at depth in the earth
epicenter
the point on Earth's surface directly above the focus
Seismic Waves
elastic waves of vibration and shaking that originates at the focus of the earthquake and travel in all directions through, on, and below the surface of the Earth
Seismograph
record of seismic waves that is produced by a seismograph
Body Waves
seismic waves that travel through the earth's interior,

-P-waves: called primary waves because they travel fast and arrive at seismographs first; compression or "push-pull" waves
-S-waves: called secondary waves because they travel slower and arrive at seismographs second; perpendicular or "side-to-side" waves
L-waves
surface seismic waves that arrive at seismographs last because they travel along on earth's surface
active faults
faults that can move and generate earthquakes at the present time
first motion
the way the pen on a seismograph moves when the p-waves arrive can tell you about the relative motion of the fault zone
-compression: the pen moves up when the P-waves arrive
-dilation: the pen moves down when the P-waves arrive
-compression and dilation are relative motions
topographic map
two-dimensional model represent a three-dimensional landscape
latitude
measured from 0 at equator to 90 degrees N (at north pole) and 90 degrees S (at south pole)
longitude
measured east to west from 0 degrees at the prime meridian
GPS (global positioning system)
constellation of 28 satellites in 12 hour orbits about 12,000 miles above earth; based on the universal transverse mercator system.
UTM (Universal Transverse Mercator System)
global military navigation grid and coordinate system; grid is rectangular and measured in decimal-based metric units
zones
sixty north-south strips of longitude of a 6 degree width, numbered Zone 01 to Zone 60; location within a zone is defined by its easting and northing coordinate
easting
distance in meters within a zone measured from west to east
northing
distance in meters from the equator
topographic profile
cross section that shows the elevations, ruggedness, and slopes along a given line between two points

vertical exaggeration = vertical/horizontal scale
relief
difference in elevation between 2 points
regional relief: difference between the highest and lowest points on a topographic map
gradient
steepness of a slope; typically determined by dividing the relief between two points by the distance between them (including curves of streams)
slope
typically calculated as the change in elevation between to points divided by the straight-line distance between them (rise/run)
declination
difference in degrees of compass north and true north on a topographic map
benchmark
permanent marker placed by the U.S. geological survey or Bureau of Land management
perennial streams
flow continuously throughout the year and are represented by blue lines on topographic maps
intermittent streams
flow only at certain times a year, such as rainy seasons or during snow melt; they are represented by dotted line segments on a topographic map
flood
occurs when a stream overflows its banks
alluvium
sediment transported and deposited by streams
stream drainage system
drainage network including upland tributaries and main stream
stream drainage patterns
stream drainage systems form characteristic patterns of drainage depending on relief and geology. page 214 and fig 11.2 for specific patterns
drainage basin
entire area of land drained by one stream
floodplain
relatively flat areas on either side of a river prone to flooding
cutbanks
form at the outer edge of meanders and experience erosion
point bars
form at the inner edge of meanders and experience deposition
oxbow lake
forms as the result of a meander being cut off from main stream channel (due to flooding)
stream terraces
remnants of older floodplains
submergent coastline
created by a rising sea level; sea level rise can be caused by water level rising (transgression) or land level getting lower (subsidence)
emergent coastline
created by falling sea level; sea level can fall by water level falling (regression) or by rising of the land surface (uplift)
barrier island
long, narrow island that parallels the mainland coastline and is separated from the mainland by a lagoon, tidal flat, or salt marsh
beach
gently sloping deposit of sand or gravel along the edge of a shoreline
estuary
river valley flooded by a rise in level of an ocean or lake
longshore current
water current in the surf zone that flows slowly parallel to the shoreline, driven by waves; moves sediment in direction of current
delta
sediment deposit at the mouth of a river where it enters an ocean or lake
spit
sand bar extending from the end of a beach into the mouth of an adjacent bay
wave-cut cliff
seaward facing cliff along a steep shoreline, produced by wave erosion
wave-cut platform
bench or shelf at sea level along a steep shore, formed by wave erosion
marine terrace
eleveated platform that is bounded on its seaword side by a cliff or steep slope; formed when a wave-cut platform is elevated by uplift or regression
stack
isolated rocky island near a headland cliff
sea wall
an embankment of boulders, reinforced concrete, or other material constructed against a shoreline to prevent erosion by waves and currents
groin
short wall constructed perpendicular to shoreline in order to trap sand and make or build up a beach
jetties
long walls extending from the shore at the mouths of harbors and used to protect the harbor entrance from filling with sand or being eroded by waves and currents
strike
the compass bearing (direction) of a line formed by the intersection of a horizontal plane (such as the surface of a lake) and an inclined layer (bed, stratum) of rock,fault, fracture, or other surface.
dip
the angle between a horizontal plane and the inclined (tilted) stratum, fault, or fracture.
faults
breaks along which movement has occured. caused by tension compression and shear forces
hanging wall
top surface of a fault
footwall
the bottom surface of a fault
normal fault
tension fault, walls move away from one another
reverse fault
compression fault, walls move toward one another
strike skip fault
shearing fault, left lateral vs. right lateral means that from one side of the fault the other side appears to move in a certain direction, right for right lateral and vice versa
anticlines
oldest rocks in the middle
synclines
youngest rocks in the middle
domes
strata sloped upward, anticline
basin
strata slope downward like a bowl, syncline
water table
upper surface of the water logged zone called the zone of saturation
groundwater
water in the saturated zone
well
can withdraw groundwater
aquifers
rock strata that conduct water
hydraulic gradient
slope of the water table surface
water table contour lines
contour lines for water
cone of depression
change in the regional flow of groundwater around a well
karst
distinctive topography that indicates dissolution of underlying soluble rock, generally limestone
sinkhole
surface depression formed by the collapse of caves or other large underground void spaces
artesian well
water that wells out of the surface due to its own pressure somehow...a well that comes out at the surface of the earth on its own