Units 26-27 Flashcards
What are the five categories of evidence that teach us about earth’s interior?
- Direct observation of rocks from interior
- Relationships to rocks or meteorites from space
- Inferences from Earth’s density
- Evidence from seismic (earthquake) waves
- Requirements for producing Earth’s magnetic field
What brings deep rocks to the surface that can’t be reached by drilling or other ways?
Volcano blasts and ascending magmas.
Crust
The uppermost compositional layer of Earth.
Characteristics of the crust:
Very thin
Composed of two parts: Granitic continental crust and basaltic oceanic crust
True or False: Rocks brought to the surface by volcanoes are denser than the basalts on the ocean floor.
True
Mantle
The middle compositional layer of earth.
Characteristics of Mantle:
Thick layer
Made of peridotite in the upper part
and higher density rocks of peridotite composition in the lower part.
Peridotite
Rock made up of mostly silicon, oxygen, iron, and magnesium.
True or False: Peridotite is denser than the basalt and granite of the earth’s crust
True
Meteorites
A rock from space that HITS earth’s surface
Stony chondrites
Meteorites thought to be composed of unprocessed material from the original solar nebula
The same materials that our planet and solar system were originally made.
What percentage of meteorites are stony chondrites?
86%
Stony achondrites
Meteorites thought to represent material from small planetary bodies that had differentiated into layers and then were broken up.
What percentage of meteorites are stony achondrites?
8%
Iron meteorites
Meteorites thought to represent the type of material found in Earth’s core
What percentage of meteorites are iron?
6%
Core
The deepest or central compositional layer of Earth. It is composed mostly of iron
What is the equation for Earth’s mass?
M = gR^2 / G
M = mass of earth
g = acceleration of gravity
R = radius of earth
Why do we care what Earth’s density is?
Because that tells us about the rocks that compose it.
Why do we care about Earth’s mass?
Because having the mass lets us calculate density
True or False: Earth’s surface is elastic
True
It rebounds back into shape when pressure is released
Elastic rebound
The point at which stress in Earth’s lithosphere is strained to a point where it can bend no further. When this happens, the lithosphere ruptures and rebounds somewhat like a rubber band that has just been pulled apart.
Fault
A break in earth’s lithosphere where rocks on one side of the break have slipped past the rocks on the other side
What causes faults exclusively?
Earthquakes
What characteristic of earth are faults a result of (not earthquakes)?
Elastic rebound
Tectonic plates
The brittle, rigid but thin outer part of Earth is divided into sections called tectonic plates
Seismic waves
Waves produced by earthquakes (caused by tectonic plates rubbing against each other, smashing into each other, and slipping.
Seismos translation?
Earthquake in Greek
True or False: Earthquakes simultaneously produce compression, shear, and surface waves.
True
Which type of waves travel fastest, compression, shear, or surface?
Compression
P waves
Primary waves.
These are compression waves produced by an earthquake. They travel the fastest so they reach the measuring detectors first (primary).
S waves
Secondary waves.
Shear waves. They are second to arrive at seismic detectors
What is the slowest type of wave?
Surface
Focus
Point of origin in an earthquake.
The place inside the earth where an earthquake originates
Epicenter
The point on Earth’s SURFACE directly above the focus of an earthquake
True or False: The speeds of P and S waves change depending on the type of rocks/materials they are passing through.
True
True or False: The stiffer the rocks, the slower the wave speed.
FALSE
The faster the wave speed
Why do wave speeds and directions REFRACT inside the earth’s surface?
Because of the properties and elasticity of the rocks they are travelling through, which vary by density.
Seismographs
The detectors in the grid of earthquake recording stations.
Seismometers
Device that measures ground motion
Seismic discontinuity
A place where the velocities of seismic waves change abruptly.
Moho
Short for Mohorovicic discontinuity. It is the location of the boundary between densities. At the base of the earth’s crust.
Shadow zone
A region of earth where seismic waves cannot be detected by seismometers.
Look at 26.7 figure. Easy.
Outer core
The upper part of the core that is made of liquid iron
How did we figure out that the outer core (or any part of the earth’s interior) was liquid?
Because of the shadow zones. Shear waves can only travel through a solid.
Inner core
The lower part of the core that is made of solid iron
What happens to the density as you move in through the core of the earth?
It increases
Curie temperature
The temp at which a material loses its magnetism (not a permanent magnet anymore)
True or False: Earth’s magnetic field is produced by a giant, iron core that is magnetized.
FALSE
The core is not magnetized (too hot, curie temperature explanation)
What causes earth’s magnetic fields?
Electrical currents in the earth
What causes the electrical currents in the earth?
The difference in temperature between the inner and outer core (solid and liquid) creates convection that move iron atoms in great cylindrical cells that rotate equatorially (earth’s rotation).
Relies on the Sun’s magnetic field.
True or False: There are many types of rock in the earth’s crust, including igneous, sedimentary, and metamorphic.
True
It averages granite
Silicates
Minerals that contain silicon and oxygen bonded together
True or False: The oceanic crust is virtually all basalt
True
Which is more dense, the oceanic or continental crust?
Oceanic
Dense oxides
Minerals that form deep in earth’s mantle due to the enormous pressures