
Unit: Dynamic Earth - Science Teacher Tom
... Do Now: Draw diagrams representing the movement along the 3 types of plate boundaries along with the associated features seen on Earth’s crust. Make sure to include continental-continental, oceanic-oceanic, and continental-oceanic interactions for all 3 types of plate boundaries. AIM: What are the c ...
... Do Now: Draw diagrams representing the movement along the 3 types of plate boundaries along with the associated features seen on Earth’s crust. Make sure to include continental-continental, oceanic-oceanic, and continental-oceanic interactions for all 3 types of plate boundaries. AIM: What are the c ...
Birth of the Universe
... P waves: - primary waves - compressional wave - movement is in the same direction that the wave is traveling - highest velocity seismic wave (4mi/s) - travel through solids, liquids, and gases ...
... P waves: - primary waves - compressional wave - movement is in the same direction that the wave is traveling - highest velocity seismic wave (4mi/s) - travel through solids, liquids, and gases ...
File
... different speeds, the difference in their arrival times can be used to determine the DISTANCE away an earthquake occurred. ...
... different speeds, the difference in their arrival times can be used to determine the DISTANCE away an earthquake occurred. ...
Earthquake Lesson
... different speeds, the difference in their arrival times can be used to determine the DISTANCE away an earthquake occurred. ...
... different speeds, the difference in their arrival times can be used to determine the DISTANCE away an earthquake occurred. ...
Topics covered in PH112 - Rose
... Torque, moment arm, line of action of F Newton’s second law in angular form Work and rotational kinetic energy Rolling bodies, KE in terms of center of mass Angular momentum of a system of particles, and of a rigid body Conservation of angular momentum Simple harmonic motion: frequency, period, ampl ...
... Torque, moment arm, line of action of F Newton’s second law in angular form Work and rotational kinetic energy Rolling bodies, KE in terms of center of mass Angular momentum of a system of particles, and of a rigid body Conservation of angular momentum Simple harmonic motion: frequency, period, ampl ...
Plate Tectonics - twpunionschools.org
... • The energy from an earthquake is released as seismic waves, that travel through Earth’s crust from the focus causing the ground to shake. • P waves – come first, compress and expand • S waves – come second, side to side • Surface waves- move along the surface, causes severe ground movements ...
... • The energy from an earthquake is released as seismic waves, that travel through Earth’s crust from the focus causing the ground to shake. • P waves – come first, compress and expand • S waves – come second, side to side • Surface waves- move along the surface, causes severe ground movements ...
Document
... With these waves, the particle motion is PERPENDICULAR to the direction of energy transfer ...
... With these waves, the particle motion is PERPENDICULAR to the direction of energy transfer ...
Structure of the Earth`s Deep Interior
... (plumes arise from a thin, compositionally distinct layer near CMB) modulated by slabs which may enter PPv phase nearby ...
... (plumes arise from a thin, compositionally distinct layer near CMB) modulated by slabs which may enter PPv phase nearby ...
Earthquakes & Volcanoes
... Types of Seismic Waves: 1. PRIMARY Waves: P-WAVES travel the fastest FIRST to be recorded travel through solid AND liquid compressional waves that push and pull ...
... Types of Seismic Waves: 1. PRIMARY Waves: P-WAVES travel the fastest FIRST to be recorded travel through solid AND liquid compressional waves that push and pull ...
earthquakes - Cloudfront.net
... ground when rock (plates) move suddenly and release energy. • aftershock – a release in energy after an earthquake ...
... ground when rock (plates) move suddenly and release energy. • aftershock – a release in energy after an earthquake ...
Earthquakes, Aftershocks and Seismic Waves
... • The aftershocks occur during a period of readjustment, in which small localized strains on the fault are released. • Deep focus earthquakes usually do not have aftershocks. • Earthquakes cause Seismic Waves! • Use to study composition of earth’s interior. ...
... • The aftershocks occur during a period of readjustment, in which small localized strains on the fault are released. • Deep focus earthquakes usually do not have aftershocks. • Earthquakes cause Seismic Waves! • Use to study composition of earth’s interior. ...
The Northridge Earthquake
... HOMEWORK: DETERMINE THE EPICENTER OF THE 1994 NORTHRIDGE EARTHQUAKE Seismic waves, felt as the shaking motion when an earthquake occurs, are generated when energy is released during an earthquake. The difference in time is takes for the two primary types of seismic body waves—P waves and S waves—to ...
... HOMEWORK: DETERMINE THE EPICENTER OF THE 1994 NORTHRIDGE EARTHQUAKE Seismic waves, felt as the shaking motion when an earthquake occurs, are generated when energy is released during an earthquake. The difference in time is takes for the two primary types of seismic body waves—P waves and S waves—to ...
Surface Waves
... raypaths refracted by the varying density and modulus (stiffness) of the Earth's interior. The density and modulus, in turn, vary according to temperature, composition, and phase. This effect resembles the refraction of light waves. ...
... raypaths refracted by the varying density and modulus (stiffness) of the Earth's interior. The density and modulus, in turn, vary according to temperature, composition, and phase. This effect resembles the refraction of light waves. ...
a. Transverse or Shear wave
... Secondary Waves AKA S-Wave; With these waves, the particle motion is PERPENDICULAR to the direction of energy transfer a. ...
... Secondary Waves AKA S-Wave; With these waves, the particle motion is PERPENDICULAR to the direction of energy transfer a. ...
Vibrations and Waves. So much fun, you can’t stand it!
... Longitudinal (compressional) waves displace matter parallel or inline with the direction of the wave. ( Think slinky, earthquake) ...
... Longitudinal (compressional) waves displace matter parallel or inline with the direction of the wave. ( Think slinky, earthquake) ...
Standard EPS Shell Presentation
... moves the ground up & down and side-toside rolling the ground like waves on water. ...
... moves the ground up & down and side-toside rolling the ground like waves on water. ...
More Earth Science Cloze Notes
... •As the rock layers are shaking back and forth they send out waves of vibration called Seismic Waves •“Seismic” always has to do with earthquake activity ...
... •As the rock layers are shaking back and forth they send out waves of vibration called Seismic Waves •“Seismic” always has to do with earthquake activity ...
Earthquake Terms
... 3. Seismograph- An instrument that detects, records, and measures the vibrations produced by an earthquake. 4. Seismogram- The record made by a seismograph, the paper on which the earthquake waves are recorded. 5. Epicenter- The point on the surface of the earth directly above the focus of an earthq ...
... 3. Seismograph- An instrument that detects, records, and measures the vibrations produced by an earthquake. 4. Seismogram- The record made by a seismograph, the paper on which the earthquake waves are recorded. 5. Epicenter- The point on the surface of the earth directly above the focus of an earthq ...
Document
... 28. What does the speed of a seismic wave depend on? _______________________________________________________________ _______________________________________________________________ 29. Which are always the first waves of an earthquake to be detected? _________________________________________________ ...
... 28. What does the speed of a seismic wave depend on? _______________________________________________________________ _______________________________________________________________ 29. Which are always the first waves of an earthquake to be detected? _________________________________________________ ...
01 - Mayfield City Schools
... 28. What does the speed of a seismic wave depend on? _______________________________________________________________ _______________________________________________________________ 29. Which are always the first waves of an earthquake to be detected? _________________________________________________ ...
... 28. What does the speed of a seismic wave depend on? _______________________________________________________________ _______________________________________________________________ 29. Which are always the first waves of an earthquake to be detected? _________________________________________________ ...
Chapter 8 Section 1 Guided Reading
... 28. What does the speed of a seismic wave depend on? _______________________________________________________________ _______________________________________________________________ 29. Which are always the first waves of an earthquake to be detected? _________________________________________________ ...
... 28. What does the speed of a seismic wave depend on? _______________________________________________________________ _______________________________________________________________ 29. Which are always the first waves of an earthquake to be detected? _________________________________________________ ...
Surface wave inversion

Inversion is the set of methods used to infer properties through physical measurements. Surface wave inversion is the method by which elastic properties, density, and thickness of layers in the subsurface are attained through analysis of surface wavedispersion. The entire inversion process requires the gathering of seismic data, the creation of dispersion curves, and finally the inference of subsurface properties.