Earthquakes
... marks you made. 3) Once they are matched, as close as you can, read down from this intersection to find the equivalent distance. ...
... marks you made. 3) Once they are matched, as close as you can, read down from this intersection to find the equivalent distance. ...
Document
... in the same direction as wave movement – S or secondary waves • slower than P waves • travel through solids only • shear waves - move material perpendicular to wave movement ...
... in the same direction as wave movement – S or secondary waves • slower than P waves • travel through solids only • shear waves - move material perpendicular to wave movement ...
Physics Final Review Sheet Name
... 50. What type of material conducts heat and electricity well? ...
... 50. What type of material conducts heat and electricity well? ...
Earthquakes
... The San Andreas fault zone separates two great sections of the crust of earth, the North American plate and the Pacific plate ...
... The San Andreas fault zone separates two great sections of the crust of earth, the North American plate and the Pacific plate ...
DP Physics 4.1 Oscillations Name: 1. A wave can be described as
... entire bulk of the medium move in a parallel and a perpendicular direction (respectively) relative to the direction of energy transport. In a surface wave, it is only the particles at the surface of the medium that undergo the circular motion. The motion of particles tends to decrease as one proceed ...
... entire bulk of the medium move in a parallel and a perpendicular direction (respectively) relative to the direction of energy transport. In a surface wave, it is only the particles at the surface of the medium that undergo the circular motion. The motion of particles tends to decrease as one proceed ...
The Wave Equation & Velocity
... Rock properties that affect seismic Crustal Rocks velocity include: • Porosity • Rock composition • Pressure • Temperature • Fluid saturation = Vp, = Vs are much more sensitive to and than to ...
... Rock properties that affect seismic Crustal Rocks velocity include: • Porosity • Rock composition • Pressure • Temperature • Fluid saturation = Vp, = Vs are much more sensitive to and than to ...
Dynamic_Planet_CyFalls_
... travel fastest when they move along the land surface are amplified most when moving through solid bedrock cause more damage to buildings when they travel faster are “dampered” when they move through soft, wet sediments none of the above is true ...
... travel fastest when they move along the land surface are amplified most when moving through solid bedrock cause more damage to buildings when they travel faster are “dampered” when they move through soft, wet sediments none of the above is true ...
EARTHQUAKES
... to 140 degrees that, for a given earthquake, does not receive any direct P waves. The shadow zone results from S waves being stopped entirely by the liquid core and P waves being bent (refracted) by the liquid core. ...
... to 140 degrees that, for a given earthquake, does not receive any direct P waves. The shadow zone results from S waves being stopped entirely by the liquid core and P waves being bent (refracted) by the liquid core. ...
- Google Sites
... • SEISMIC WAVES produced by the release of energy – move out in circles from the point of rupture (focus) 2 types of Seismic Waves: surface & body (travel inside & through earth’s layers) ...
... • SEISMIC WAVES produced by the release of energy – move out in circles from the point of rupture (focus) 2 types of Seismic Waves: surface & body (travel inside & through earth’s layers) ...
5 - PowerPoint - Earthquakes
... the same direction as wave movement S or secondary waves slower than P waves travel through solids only shear waves - move material perpendicular to wave movement ...
... the same direction as wave movement S or secondary waves slower than P waves travel through solids only shear waves - move material perpendicular to wave movement ...
Section 19.2 and 19.3 – Seismometer, Seismograms, and Scales
... • Seismic waves change their paths and speed as they encounter boundaries between zones of different materials. • Using this information scientists have discovered the thickness and composition of the Earth’s regions: – Upper mantle is perdotite – Outer core mostly liquid iron and nickel – Inner cor ...
... • Seismic waves change their paths and speed as they encounter boundaries between zones of different materials. • Using this information scientists have discovered the thickness and composition of the Earth’s regions: – Upper mantle is perdotite – Outer core mostly liquid iron and nickel – Inner cor ...
Conceptual Physics- Final Examination Review Practice
... _______19. The force of attraction between two particles due to their mass is called gravity. _______20. An example of a lever is a hammer. _______21. Any change is speed or velocity is called acceleration. _______22. An object with more mass would be more difficult to stop. _______23. Energy is mea ...
... _______19. The force of attraction between two particles due to their mass is called gravity. _______20. An example of a lever is a hammer. _______21. Any change is speed or velocity is called acceleration. _______22. An object with more mass would be more difficult to stop. _______23. Energy is mea ...
McGill University Faculty of Science Department of Earth and
... PcS, the ScS, the PKiKP, etc.. etc. (all body waves travelling through the volume of the Earth) and the Rayleigh, the Love, the Stonely, the tsunami, etc. (all surface or boundary waves travelling along some 2-dimensional surface within or on the Earth). All such wavetypes conspire through construc ...
... PcS, the ScS, the PKiKP, etc.. etc. (all body waves travelling through the volume of the Earth) and the Rayleigh, the Love, the Stonely, the tsunami, etc. (all surface or boundary waves travelling along some 2-dimensional surface within or on the Earth). All such wavetypes conspire through construc ...
Introduction to Waves Classification of Waves
... very quickly, even though not a single individual who takes part in spreading it travels between these two cities. There are two quite different motions involved, that of the rumor, Washington to New York, and that of the persons who spread the rumor. The wind, passing over a field of grain, sets up ...
... very quickly, even though not a single individual who takes part in spreading it travels between these two cities. There are two quite different motions involved, that of the rumor, Washington to New York, and that of the persons who spread the rumor. The wind, passing over a field of grain, sets up ...
Shear wave velocity prediction from petrophysical logs
... network structures for the dataset. Due to the fact that Leveneberg-Marquardt (LM) algorithm is one of the most effective training algorithm in speeding up the convergence rate of the MLP neural network, it has been widely used in practical estimation and classification problems. The LM suffers from ...
... network structures for the dataset. Due to the fact that Leveneberg-Marquardt (LM) algorithm is one of the most effective training algorithm in speeding up the convergence rate of the MLP neural network, it has been widely used in practical estimation and classification problems. The LM suffers from ...
File - Physical Science
... B) ocean floor drilling D) paleomagnetism 7. Cooler, older, oceanic lithosphere SINKS into the mantle at ________. A) subduction zones along convergent plate boundaries B) transform fault zones along divergent plate boundaries C) rift zones along mid-ocean ridges D) sites of long-lived, hot spot vol ...
... B) ocean floor drilling D) paleomagnetism 7. Cooler, older, oceanic lithosphere SINKS into the mantle at ________. A) subduction zones along convergent plate boundaries B) transform fault zones along divergent plate boundaries C) rift zones along mid-ocean ridges D) sites of long-lived, hot spot vol ...
Earthquakes - Chapter 10
... In reality, copper wire coils move around magnets, generating current which is recorded. ...
... In reality, copper wire coils move around magnets, generating current which is recorded. ...
what are earthquakes
... in the same direction as wave movement – S or secondary waves • slower than P waves • travel through solids only • shear waves - move material perpendicular to wave movement ...
... in the same direction as wave movement – S or secondary waves • slower than P waves • travel through solids only • shear waves - move material perpendicular to wave movement ...
Lec8 - nptel
... wavelength (high frequency). Therefore, in the real world of heterogeneous materials. Rayleigh waves are also dispersive. The dispersion of Rayleigh waves can be used to evaluate subsurface stiffness profiles by field testing techniques. Since the velocities of both Rayleigh waves and Love waves dec ...
... wavelength (high frequency). Therefore, in the real world of heterogeneous materials. Rayleigh waves are also dispersive. The dispersion of Rayleigh waves can be used to evaluate subsurface stiffness profiles by field testing techniques. Since the velocities of both Rayleigh waves and Love waves dec ...
What are Earthquakes - University of Canterbury
... in the same direction as wave movement – S or secondary waves • slower than P waves • travel through solids only • shear waves - move material perpendicular to wave movement ...
... in the same direction as wave movement – S or secondary waves • slower than P waves • travel through solids only • shear waves - move material perpendicular to wave movement ...
What are Earthquakes?
... in the same direction as wave movement – S or secondary waves • slower than P waves • travel through solids only • shear waves - move material perpendicular to wave movement ...
... in the same direction as wave movement – S or secondary waves • slower than P waves • travel through solids only • shear waves - move material perpendicular to wave movement ...
tsunami - Tull13
... the coast and monitor changes in sea level . Unfortunately , since tsunamis are not very tall in height when they are out at sea. Dentation is not easy and there are many false alarms , sirens at affected beaches my be activated – do not ignore ...
... the coast and monitor changes in sea level . Unfortunately , since tsunamis are not very tall in height when they are out at sea. Dentation is not easy and there are many false alarms , sirens at affected beaches my be activated – do not ignore ...
Electromagnetic Waves Mechanical Waves All W aves
... • Waves are vibrations created by an energy source (such as the Sun); waves move from one place to another • Waves have specific shapes -- tops (crests) and bottoms (troughs), length (wavelength) and height (amplitude) • The number of waves that pass a particular point can be counted; the number of ...
... • Waves are vibrations created by an energy source (such as the Sun); waves move from one place to another • Waves have specific shapes -- tops (crests) and bottoms (troughs), length (wavelength) and height (amplitude) • The number of waves that pass a particular point can be counted; the number of ...
Exam #: Printed Name: Signature: PHYSICS DEPARTMENT
... An electromagnetic wave with angular frequency ω is normally incident on a metal with conductivity σ, permittivity ǫ0 , and magnetic permeability µ0 . This problem can be analyzed by treating the metal as a dielectric with an effective permittivity ǫeff = ǫ0 (1 + iσ/(ǫ0 ω)). a) Assuming that the con ...
... An electromagnetic wave with angular frequency ω is normally incident on a metal with conductivity σ, permittivity ǫ0 , and magnetic permeability µ0 . This problem can be analyzed by treating the metal as a dielectric with an effective permittivity ǫeff = ǫ0 (1 + iσ/(ǫ0 ω)). a) Assuming that the con ...
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.