Midterm 5 Flashcards
Earths 3 basic layers
Crust
Mantle
Core
Earths crust
Thin and cool
Divided into basaltic oceanic crust and granitic continental crust
Earths mantle
Thick
Hot rock rich in silicon and oxygen (like the crust)
Mantle contains more magnesium, iron, and calcium
Earths core
Composed of scorching hot metal
Mostly iron/some nickel
Earth consists of layers that differ by properties rather than….
Chemical composition
Properties that determine Earth’s layers
Temperature
Pressure
Strength
Ability to flow
Earth’s structural layers
Lithosphere Asthenosphere Lower mantle Outer core Inner core
Seismology is..
The study of earthquakes and seismic waves
Earthquakes release stored
Elastic energy
Energy radiates outward in all directions
Energy travels in the form of
Seismic waves
Which cause the ground to shake and vibrate
What does the analysis of seismic waves provide?
A detailed view of Earth’s layered interior
Two types of seismic waves
- Body waves: travel through earth’s interior (primary waves: p-waves; secondary waves: s-waves)
- Surface waves: travel on earth’s surface (Rayleigh waves; love waves) MOST DESTRUCTIVE
Wegener’s evidence to support continental drift hypothesis
- Jigsaw fit of the continents
- Fossil evidence
- Matching rock types
- Structural similarities in mountain chains on different continents
- Paleoclimatic evidence
Plate Tectonics - earths division
Earth divided into a dozen or so major lithospheric plates as well as a few smaller ones
Plates
In motion and continually changing in shape and size
Largest plate
Pacific Plate
Do several plates include an entire continent plus a large area of sea floor?
Yes
Oceanic-oceanic convergence
- When 2 oceanic plates converge, the older and denser plate descends beneath the other plate
- As the denser plate descends, partial melting of mantle rock generates magma and volcanoes
- If the volcanos emerge as islands, a volcanic island arc is formed (ex: Japan)
Oceanic-continental convergence
- the denser oceanic slab sinks into the asthenosphere
- As the denser plate descends, partial melting of mantle rock generates magma
- The mountains produced by volcanic activity from subduction of oceanic lithosphere are called continental volcanic arcs or island arcs
Continental-continental convergence
- continued subduction can bring two continents together
- the less dense, buoyant continental lithosphere does not subduct
- the result is a collision btwn two continental blocks
- the process produces mountains
Transform-Fault boundaries
- most located within ocean basins
- a few of these cut through continental crust
Extremophiles
Organisms adapted to the extreme conditions found at great depth in ocean trenches