• Shuffle
    Toggle On
    Toggle Off
  • Alphabetize
    Toggle On
    Toggle Off
  • Front First
    Toggle On
    Toggle Off
  • Both Sides
    Toggle On
    Toggle Off
  • Read
    Toggle On
    Toggle Off
Reading...
Front

Card Range To Study

through

image

Play button

image

Play button

image

Progress

1/40

Click to flip

Use LEFT and RIGHT arrow keys to navigate between flashcards;

Use UP and DOWN arrow keys to flip the card;

H to show hint;

A reads text to speech;

40 Cards in this Set

  • Front
  • Back
Theory of Plate Tectonics
idea that the earth's crust is made up of moving plates, the earth's crust floats on a layer of semiliquid rock or magna
Lithosphere
The crust and upper area of the mantle that consists of large pieces called plates.
plate boundaries
places where the plates meet
Causes of Earthquakes
1. The build up of energy when two surfaces push and scrape each other
2. Faults
3. Adding or removing large amounts of earth
4. Molten rock under a volcano moves
Faults
breaks in the earth's surface along which rocks can move
3 types of Faults:
1. thrust or reverse - rocks push together until they force a secton of rock upward
2. normal fault-rocks move apart, a section of rock may fall between the separating rocks
3. strike-slip fault - rocks move horizontally past each other
a famous strike-slip fault
San Andreas Fault in California
Earth waves (seismic waves)
vibrations sent out from the beginning point of an earthquake
epicenter
point on the surface of the earth directly above the focus
body waves
seismic waves that occur beneath the surface of the earth
2 types of body waves
P waves - fastest moving body wave: straight path
S waves - move more slowly than the P wave, up and down, zigzag pattern
land waves (L waves)
when P and S waves reach the surface of the earth
L waves
slowest moving and most destructive waves
2 types of L waves
1. Love waves - fastest moving land waves, move back and forth
2. Rayleigh waves - move along ground in a rolling motion
Seismograph
a machine used to detect, time, and measure the movements of the earth
Richter Scale
measures the magnitude (strength)
Tsunamis
a giant wave
Causes of volcanoes
* crack in the earth's crust allows for magma and gases to surface
1. Magma chambers - deep pockets of molten rock
2. Hot magma rises and pushes through the earth's crust
3. When magma breaks through it is called lava
4. Lava comes out through vents (may have more than 1 vent)
* minerals and gases determine how much the volcano will explode
* some volcanoes produce clouds filled with jagged bits of crushed rocks - ash
2/3 of active volcanoes are found in an area of the Pacific Ocean called:
Ring of Fire
Hot spots
pools of intensely hot magma
Move volcanic eruptions occur where?
under the ocean
Another location of volcanoes
Mediterranean Sea
Cinder cone shape volcano
more like a hill
bowl-like crater
1 vent
showers bits of ash and lava
Shield volcano
gradually sloping sides
looks like upside down saucer
generally largest in the world
not usually explosive
Composite cone volcano
steep sides and very tall
explosive eruptions
Active volcano
one that has erupted at some point during recorded time and is expected to erupt again
Dormant volcano
have erupted in distant past,
currently inactive,
not expected to erupt again
Extinct volcano
does not have a recorded eruption
not expected to erupt in the future
effects of volcanoes
vog
acid rain
debri flow
product of volcanoes
pumice
obsidian jewelry
granite for building
vog
volcanic fog, a pollution that can aggravate respiratory problems
acid rain is from ?
gases
debri flow
falling mud and rocks
Other Thermal Eruptions
Hot springs
Geyser
Mud pot
Hot spring
heat from magma warms water, water rises to the earth's surface
Geyser
hot spring that periodically blows steam and hot water into the air
Mud pot
hot spring that contains more mud than water
crater
bowl shape at the top of main vent of a volcano
seismologist
scientist who study the movement of the earth
volcanologist
scientist who study volcanoes