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Mapping the Inner Earth
seismograph
- device used to measure earthquakes
seismometer
- modern seismographs
seismogram
- data recorded by seismometers
seismologist
- a person who studies seismology
Seismic Waves
Body
Waves- P -Waves and S -Waves
Surface
Waves - Love Waves and Rayleigh Waves
P Waves
Primary seismic waves, fastest, detected in both solids and liquids
S waves
Secondary seismic waves, slower than P-Waves, detected only in solids
Love Waves
Dispersive surface waves with horizontal motion, perpendicular to the direction of wave propagation
Rayleigh Waves
Motion is a combination of longitudinal compression and dilation that results in an elliptical motion of points on the surface
Plate Tectonics
All-Earth-a single landmass or supercontinent from which Earth began
Continental Drift
Theory-proposed by
Alfred Wegener
and proposed the Pangaea
Gondwana
and
Laurasia
-two major supercontinents after the breaking of Pangaea
Seafloor Spreading Theory -proposed by Harry Hess that seafloors and not the continents are moving and carrying continents along
Plate Tectonics
Theory -the lithosphere is made of independent slabs of solid rocks called plates which float on the plastic mantle
Plate Boundaries and Interactions
Convergent
Plate Boundary-continental-continental, continental-oceanic, oceanic-oceanic
Divergent
Plate Boundary-plates are moving apart and new crust is being produced
Transform
Plate Boundary-plates are moving horizontally past each other
Triangulation
Process of locating the epicenter of an earthquake using data from multiple seismograph stations
Types of Mountains and Mountain Ranges
Fold
Mountains-formed through plate convergence
Volcanic
Mountains-formed by volcanic activity
Erosion
Formed Mountains-shaped by erosion
Dome
Mountain Ranges-made by upwarping of tectonic plates
Fault-Block
Mountain Ranges-made by movement of normal faults causing tensional forces
Electromagnetic Induction
A changing magnetic field produces an electric current
Faraday's
Law
A change in the strength of a magnetic field (magnetic flux) induces a current
Lenz's
Law
The induced current creates a magnetic field that opposes the change in the magnetic flux
Magnetic Flux
The quantity of magnetism passing through a surface
Generators
Devices
that can convert mechanical energy to electrical energy
Armature
-consists of coils of insulated wire wound around a soft iron core
Field
-either an electromagnet or permanent magnet used as a source of magnetic field
Slip
Rings
-made of either brass or copper
Brushes
-stationary part sliding with the slip rings that collects the current and transmits to the external circuit
DC Generators
Generators that induce a direct current (DC) but no slip rings
Motors
Devices that can convert electrical energy to mechanical energy
(
Rotor)
consists of coils of insulated wire wound around a soft iron core
(
Stator)
either an electromagnet or permanent magnet used as a source of magnetic field
(
Commutator)
rotary electrical switch that periodically reverses the current direction
AC Motors
Electric motors that are driven by alternating current (AC)
Synchronous AC motors and induction motors have no commutators and brushes
DC Motors
Rotary electric motors that convert Direct Current (DC) energy into mechanical energy
Brushed DC motor and brushless DC motor
Light
An electromagnetic (EM) wave
Light
A
transverse
wave
Produced by accelerating charges
Can travel in vacuum
Has a speed of 290,792,458 m/s
Wave Equation
Quantity: speed of propagation, wavelength, frequency
EM Spectrum Regions
Radio Waves
Microwaves
Infrared Waves
Visible Light Waves
Ultraviolet Rays
X-Rays
Gamma Rays
EM Spectrum Region
Designation, Unit, Applications/Uses
Ionizing
radiation includes X-rays and Gamma rays
Nonionizing
radiation, those that include the other regions of the EM spectrum, though less dangerous, pose a health threat
Radio waves
Can interfere with a pacemaker
Overexposure to EM radiation
Can cause blindness, burns, or delayed effects like cancer
Plane Mirrors
Image formed is virtual, upright, and same size as the object
Concave Mirrors
Location of image depends on location of object
Image can be real, inverted, and smaller/larger than object
Convex Mirrors
Image is always virtual, upright, and smaller than the object
Mirror Equation
Quantity: focal length, object distance, image distance, magnification
Magnification
Ratio of image size to object size
CONTINENTAL CRUST -
made up of light granitic rocks
OCEANIC CRUST
- the part that underlies the ocean and is composed of dense basaltic rocks
MOHOROVICIC
DISCONTINUITY - marks the boundary between the crust and the upper mantle
UPPER MANTLE
- both solid and plastic
LOWER MANTLE
- more solid than the upper mantle due to more pressure
GUTENBERG
DISCONTINUITY - boundary between the
mantle
and core
CORE
- most of Earth's volume, the greatest density
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