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51 Cards in this Set

  • Front
  • Back
What Idea Did Alfred Wegener Propose in the year 1912?
All the continents were once together and diftied through the seafloor to their present locations
What Was The Name Of The SuperContinent?
Pangea
what Evidence Did Wegener Have About The Theroy Of Continental Drift
Puzzlelike Fit Of The COntinents
Fossil Clues
Rock Clues
Climate Clues
Why Was Wegeners Theory Not Accepted?
He Did Could Not Explain How Why Or When A Great Froce Cold Have Moved The Continents
What Proved Continents Where Drifting?
Seafloor Spreading
Explain Seafloor Spreading
Ocean Crust was Younger Than Continent Crust

The closer you are to the mid ocean ridge, the younger the crust

paleomagnetic clues=magentic fields
What are the four main layers of earth?
crust mantle outer core innner core
Crust
thinnest layer. mostly granite 35 miles
ocean crust=5miles basalt
mantle
thickest layer rigid upper mantlr called asthenosphere solid
Outer Core
liquid.. iron and nickel
Inner Core
solid.. iron and nickel
Convection currents
in the asthenopshere. plates move creating continental drift
Lithosphere
plates
The earths crust is broken into
9 major and 6 minor sections
plates
oceans and continents on top of them
convergent
2 plates come together
compression
Ring of fire
subduction
creates oceanic trench
volcanic islands
divergent
2 plates seperate
tension
landforms:
riftvalleys-africa ireland
linear sea: red sea
mid ocean ridges- atlantic
volcanic islands-iceland
transform
two plates slide past each otheerr
shearing
earthquakes
san andreas (cali)
continental to continantal convergent
fold and fault block mountains
hot spots-
mantle melts plates above it. (hawaii) geysers and hotsprings (old faithful)
earthquakes
realease a tremedeous amount of energy when rocks break
energy from moving plates is sent through earth in form of ____
vibrations
seiemic waves
vibrations from focus
___ ____ earthquakes per year
100,000
___% are in the ring of fire
80
earthquakes are cause by
tension
compression
shearing
earthquakes -divergent
tension makes normal faults were rock layers slip downward
earthquakes- convergent
reverse faults rocks above the fault line push forward
earthquakes-transform
slip strike rocks pushed sideways
focus
actual location wehre rock layers break
epicenter
earthes surface directly above the focus
3 types of seismic waves
p s and l waves
P waves
primary waves move the fastest stratches and compressies material go through any material
S Waves
secondary waves slower then p waves twists material it travels through goes throgh solids
L Waves
long surface waves
most destructive makes ground rise and fall on travels on surface
how do you locate an epicenter?
using the arrival time difference between p and s waves, seismologists know the distance to an earthquake (makes a cirlce) 3 stations nessecary to pinpoint the transmission
how do scientists know the interior of earth?
by the way p and s waves travel through earth, s go through mantle (solid) s waves dont go throught outer core (liquid) changes of speed and direction
magnitude
strength of an earthquake
seismogram
measures magnetude horizontal and vertical
richter scale
how magnitude is measure open ended. every number is 10x stronger then the previous
How many active volcanoes are there?
600 many in ring of fire
dormat
volcanoes that are not currently active but could still erupt
what are volcanoes a result of?
plate techtonics
mts st helen
convergent
most active volcano
mt. kilauea
three parts of a volcano
crater, vent and magma vent
basalt magma
flows easily and produces quiet erupstions of lava
graniite magma
thick and hard to flow. )explosive eruptions of tephra)
shield volcanoes
eruptions of lava broad sides lava layers
cincer cone
thephra steep sides tephra layers
composite
layers of both tephra and lava alternate eruption moderate slope