Second Geology Test Flashcards
Elastic rebound hypothesis
Displacement happens. Rocks accumulate energy. Rocks build up stress by plates moving past each other. One day the elastic will bounce back and there will be an earthquake
What is the main reason for earth quakes?
Plate boundaries and their moving. Fault boundaries to be exact ex: San Andreas, California
Transform boundary- earthquakes
Side swipe. Creates earth quakes. There is a seismic gap- friction is holding it back ex: San Andreas fault
Tension - divergent boundaries- earthquakes
Rocks don’t have much strain energy. Pulling apart. Low earth quake waves. Normal fault. People friendly boundary.
Subduction zone- earth quakes
Strike and slip- can be low, medium and high magnitude earthquakes. Earthquakes relates to volcanoes
Magnitude
Relies on the data attained from seismic records to estimate the amount of energy released at an earthquake’s source
Contour line
Lines contacting points of equal elevation
Volcanoes
Opening in the crust, spuing out magma which then is called lava.
P waves
Primary waves. Compressional waves, anything linear will snap. Ex: bridges and electric lines. “Push/pull” waves. They push (compress) and pull (stretch) rocks in the direction the wave is traveling. P waves travel through all materials! Solid, liquid and gas. First to be recorded on seismograph.
S wave
Secondary waves. Shake the particles at right angles to their direction of travel. Liquids and gases will not transmit S waves. Second wave to be recorded and is faster then surface waves.
L wave
Called a long wave and is a wave that reaches the surface. Makes the most damage. Is the surface wave. Last waves to be recorded. Slower then the p and S waves. (Body waves) greatest amplitudes. Cause greater ground shaking and hence greater property dance than either p or a waves
How do you measure and earthquake?
Need 3 different angles of the body waves ( p wave and S wave) the data goes into a seismograph and then prints out on a seismogram.
Intensity
A measure of the amount of ground shaking at a particular location, based on observed property damage.
What is the Richter Scale ?
Is calculated by measuring the amplitude of the largest seismic wave, usually surface (S wave) is used for this this measurement on seismograph pg 198
Seismograms
Provide useful information about the nature of seismic waves. They reveal two main types of waves generated by the slippage of a rock mass. Two types are surface waves and body waves
What are surface waves?
They travel in rock layers just below earths surface. Can be divided in two types of surface waves. 1. Causes earths surface and anything resting on it to move. 2 causes earths materials to move side to side.
What are body waves?
Travel through interior of earth. And can be further divided into two types of waves P waves and S waves.
What are the four factors of damage by an earthquake?
- The intensity
- The duration of the vibrations
- The nature of the material on which structures rest
- The nature of building materials and construction practices of the region
Volcanoes
Opening in the crust, spuing out magma, which is then called lava
Oceanic volcanoes
Are non explosive
Pacific Rim
Has the most volcanoes, is a subduction zone, explosive volcanoes.
Divergence boundary volcanoes
Adding new liquid to the sea floor= non explosive volcanoes
Hot spot
Magma stays at constant position. Ex: Hawaii and yellow stone. Can tell there are hot spots by earthquake waves. S waves don’t transmit through liquid.
Composite cone
Explosive volcanoes. Pacific rim. The greater the solid material the more explosive.
Viscosity
The primary factors that affect the behavior of magma and lava are it’s temperature and composition. Also the amount of dissolved gases it contains. The lack Magma mobility. As lava cools viscosity increases
Earthquakes can cause=
Liquefaction, landslides, fire, tsunami