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53 Cards in this Set

  • Front
  • Back

anticline

an arch-shaped fold

aquifer

Layer or zone in subsurface capable of producing water to a well

artesian wells

well from which water flows under natural pressure without pumping.

compression

Stress that causes contraction (push together)

cone of depression

As water flows, pressure around a well decreses. This creates a cone-shaped depression that is similar to when the plug is pulled in a bathtub

creep

Slowest of all types of flow


Most significant damage and difficult to control

debris flow

Slower than mudflow with larger particles



More viscous

delta

Landform that forms at the mouth of a river where it flows

dip-slip faults

When the footwall goes one way and the hanging wall goes the other.



Come in the form of "normal" or "reverse"

drainage basin

Area drained by main stream

earthflow

Slower than debris and mud flows


Tongue-shaped masses of wet regolith

earthquake intensity

What you "feel"


Based on DAMAGE


Used for historical earthquakes


earthquake magnitude

Roughly based on energy


More modern and accurate

elastic limit

The lowest possible stress that something with move

epicenter

Point on surface above focus

erosion

Removal and transport of rock, sediment, soil

floodplain

An area of land adjacent to a stream or river

focus

Where rupture on fault plane starts

gravity

Reason for which groundwater flows

hot spring

A spring that is formed by geothermally heated groundwater from the earth's crust

hydrologic cycle

The continuous movement of water on, above and below the surface of the Earth.

impermeable rocks

Rocks that don't pass fluid through their pores

infiltration

The process by which groundwater enters the soil

liquefaction

Near-surface layer of water-saturated sand changes rapidly from a solid to a liquid



Causes buildings to "float"

L-waves

Surface waves


Only horizontal particle motion

mass movements

process by which soil, sand, regolith, and rock move downslope typically as a mass, largely under the force of gravity

meanders

A bend in a river

mudflow

Most rapid of all flows



triggered by rainstorms

normal faults

A slide DOWN

permeable rocks

Rocks that do pass water through their pores

point bars

Deposits at the inside of the bend of a meandering river

porosity

Percent of the total volume that is open space

P-waves

Fastest type of wave, arrives first


LONGITUDINAL (left to right)

reverse faults

A slide UP

rockslide

When rocks move downslope

runoff

The flow of water that occurs when excess water from rain, meltwater, or other sources flows over the earth's surface

shadow zone

An area of the Earth's surface where seismographs cannot detect an earthquake

shear

Stress that causes movement in two different directions (think strike-slip)

slump

Material moves downward along the curved surface of a rupture

spring

Natural flow of water from the ground surface



Intersection of water table - ground surface

stalactites

Precipitated calcite from above



"The TIGHTS come down"

stalagmites

Precipitated calcite from below



"The MITES come up"

strain

Change in size and/or shape due to the application of stress

stress

Force exerted over some area that causes rocks to undergo strain

strike-slip faults

A slide BACKWARD or FORWARD

S-waves

Slower than P-Wave (Secondary)


Move perpendicular to wave (up and down)

syncline

A trough-shaped fold

tension

Stress that causes extension

thrust faults

A reverse fault at a very small angle



Build large mountain belts

water table

The boundary below which all pore spaces are filled

where earthquakes occur

Plate Boundaries and Intra-Plate (Interior of a Plate)



How to determine: S (minus) P arrival time

zone of aeration

Unsaturated zone, little to no water

zone of saturation

Below zone of aeration, pores are filled and saturated with water