MODULE 3: EARTHQUAKES & PLATE TECTONICS Flashcards
Rock Deformation
stress & strain
Stress
a force
the force acting on a surface may be greater in certain directions than in others
Strain/Deformation
change in volume or shape of rock in response to stress
Pressure
uniform stress in all directions
Not all plate boundaries have volcanoes.
All plate boundaries have earthquakes.
Earthquakes define plate bourndaries
Transform Fault
Strike-Slip Fault
Highest magnitute earthquake ever recorded
9.5 in Chile
Every time a fault slips (ruptures) an earthquake occurs
Earthquakes are caused by a fault rupturing and asudden release of energy through the Earth’s crust in the form of seismic waves
Province
area that has the same type of plate movement
Elastic Rebound Theory
how earthquakes occur
- a fault is locked but continuous & builing tensional stress
- causes temporary deformation along fault until it reaches it’s breaking point
- energy releases abruptly and earthquake occurs
potential energy is released in the form of elastic energy
Seismic waves
first two waves released (P-waves and S-waves) are called body waves
Focus/Hypocenter
where the rupture occurs & energy is initially released
Epicenter
surface expression of focus
P-waves - Primary wave (comPressional)
- a wave consisting of alternating pulses of compression and expansion
- rock movement is parallel to wave direction
- can pass through ANY medium
- faster (~3-5mi/s)
slinky, accordian
S-Waves - Secondary Waves (Shear)
- rock is subjected to side-to-side or up-and-down forces (perpendicular)
- not transmitted through liquid
- slower (~2mi/s)
Surface waves
travels parallel to earth’s surface, occurs when body waves hit the surface
Love waves
slither like a snake
more destructive than Rayleigh
Rayleigh waves
roll like the ocean
Seismograph
instrument that detects and measures vibrations (seismic waves
Seismogram
the paper record made by a seismograph
Reelfoot Rift
failed rift under the MIssissippi river
Highest elevation on earth
8848m, 29035ft, 5.5mi
Mount Everest, Himalayas, collision zone, convergent plate boundary
lowest elevation on Earth
11000m , 36080ft, 7mi
Marianas Trench, challenger deep, convergent plate boundary
continental shelf edge or break
where low-density, thick, felsic continental crust meets dense, thin, mafic ocean crust
geologic edge of a continent
continental slope and continental rise
Jacques Piccard and Donald Walsh
went down to the Marianas Trench in 1960, in the Trieste
James Cameron
solo travel to Marianas Trench
Alfred Wegener
Meterologist, German Polar researcher
studied weather patterns on Greenland served in German army WWI
Alfred Wegener
- noticed puzzle-piece like fit of continents
- proposed a supercontinent once existed Pangaea
- hypothesized the idea of continental drift
continental drift
the slow, lateral movement of continents across the earth
Drifters
continents have drifted slowly
over time to their modern positions
Fixists
positions of continents and oceans have always looked like they do today
Pangaea
Laurasia (north)
Gondwanaland (south)
Gondwanaland
Africa, South America, Madagascar, Sri Lanka, Antarctica, Australia
Laurasia
North America, Eurasia