20150511082695
... 1) _______________ - vibrations carrying energy released during an Earthquake away from the point where the break in the crust occurred. a) seismograph b) tsunami c) seismic waves d) compass ...
... 1) _______________ - vibrations carrying energy released during an Earthquake away from the point where the break in the crust occurred. a) seismograph b) tsunami c) seismic waves d) compass ...
Week 10c_2015
... below a depth of about ~5100km, but it was not before the early 1960's that the actual size of the inner core was accurately calculated after underground nuclear tests were conducted in Nevada. ...
... below a depth of about ~5100km, but it was not before the early 1960's that the actual size of the inner core was accurately calculated after underground nuclear tests were conducted in Nevada. ...
CLASSICAL MECHANICS II - Makerere University Courses
... At the end of the course the student should be able to: Derive equations of motion for various systems Identify types of motion such as wave motion or linear or rotation motion. Solve problems involving motion of bodies. Characterise bodies in terms of their position, momentum and energy. ...
... At the end of the course the student should be able to: Derive equations of motion for various systems Identify types of motion such as wave motion or linear or rotation motion. Solve problems involving motion of bodies. Characterise bodies in terms of their position, momentum and energy. ...
Chapter 9: Earthquakes
... a) causes rocks on either side of a fault to move past each other C. Types of Faults 1. Normal Fault a) Tension pulls the rocks apart b) Rock above the fault surface moves downward in relation to rock below the fault surface c) Dia. 2. Reverse Fault a) Compression Pushes on Rocks from opposite direc ...
... a) causes rocks on either side of a fault to move past each other C. Types of Faults 1. Normal Fault a) Tension pulls the rocks apart b) Rock above the fault surface moves downward in relation to rock below the fault surface c) Dia. 2. Reverse Fault a) Compression Pushes on Rocks from opposite direc ...
Objectives - cloudfront.net
... • Remember that tectonic plates move very_______________. Sometimes rocks move along easily with the plates, but they can also jam up against a plate or between two_______________. Over time, stress builds up within the rock at the plates_______________ against each other. ...
... • Remember that tectonic plates move very_______________. Sometimes rocks move along easily with the plates, but they can also jam up against a plate or between two_______________. Over time, stress builds up within the rock at the plates_______________ against each other. ...
lecture11_2012
... The moon is a lot less attenuative, thus producing many high frequency signals. Problem: Can’t find P, S and Surface waves 5 ...
... The moon is a lot less attenuative, thus producing many high frequency signals. Problem: Can’t find P, S and Surface waves 5 ...
Earthquake Waves - davis.k12.ut.us
... The further away an earthquake is the more separation between the arrival time of the P-waves and S-waves. Think of it like timing the distance of lightning by counting the difference between the arrival of light and sound. ...
... The further away an earthquake is the more separation between the arrival time of the P-waves and S-waves. Think of it like timing the distance of lightning by counting the difference between the arrival of light and sound. ...
Wearing Down Earth`s Surface
... • Remember that tectonic plates move very_______________. Sometimes rocks move along easily with the plates, but they can also jam up against a plate or between two_______________. Over time, stress builds up within the rock at the plates_______________ against each other. ...
... • Remember that tectonic plates move very_______________. Sometimes rocks move along easily with the plates, but they can also jam up against a plate or between two_______________. Over time, stress builds up within the rock at the plates_______________ against each other. ...
Earth Science Part 2 Presentation
... Destructive to about 100 km from epicenter Major earthquake. Can cause serious damage Large earthquake. Serious damage for hundreds of km ...
... Destructive to about 100 km from epicenter Major earthquake. Can cause serious damage Large earthquake. Serious damage for hundreds of km ...
Seismic Waves Webquest - Dublin City Schools Dashboard
... 1. Go to http://aspire.cosmic-‐ray.org/Labs/SeismicWaves/ you can also access this website in the resources section of this lesson. 2. Spend 1-‐2 minutes playing with the Mighty Wave Make ...
... 1. Go to http://aspire.cosmic-‐ray.org/Labs/SeismicWaves/ you can also access this website in the resources section of this lesson. 2. Spend 1-‐2 minutes playing with the Mighty Wave Make ...
Document
... Wavelength: The distance between identical points on the wave. Amplitude: The maximum displacement A of a point on the wave. Angular Frequency w: w = 2 f Wave Number k: k = 2 / Recall: f = v / y ...
... Wavelength: The distance between identical points on the wave. Amplitude: The maximum displacement A of a point on the wave. Angular Frequency w: w = 2 f Wave Number k: k = 2 / Recall: f = v / y ...
earthquakes… - White Plains Public Schools
... A seismogram is a record written by a seismograph in response to ground motions produced by an earthquake, explosion, or other ground-motion sources ...
... A seismogram is a record written by a seismograph in response to ground motions produced by an earthquake, explosion, or other ground-motion sources ...
Final Revision
... each of them is called……… 3- The type of pollination in the same flower is…………and the pollination between two flowers is ………… 4- The first law of sound reflection, the angle ……………….. = the angle of……………………… 5- Sound waves are ……… waves which can not travel through…….. 6- The colored whorl of the flo ...
... each of them is called……… 3- The type of pollination in the same flower is…………and the pollination between two flowers is ………… 4- The first law of sound reflection, the angle ……………….. = the angle of……………………… 5- Sound waves are ……… waves which can not travel through…….. 6- The colored whorl of the flo ...
Earthquakes and Seismic Waves
... forming faults. Stress increases along a fault until the rock breaks. An earthquake begins. In seconds, the large amount of stored energy is released. ...
... forming faults. Stress increases along a fault until the rock breaks. An earthquake begins. In seconds, the large amount of stored energy is released. ...
How are seismic waves generated-Elastic rebound theory Describe
... What can seismic waves tell us? Studies of the different types of seismic waves can tell us much about the nature of the Earth’s structure. For example, seismologists can use the direction and the difference in the arrival times between P-waves and S-waves to determine the distance to the source o ...
... What can seismic waves tell us? Studies of the different types of seismic waves can tell us much about the nature of the Earth’s structure. For example, seismologists can use the direction and the difference in the arrival times between P-waves and S-waves to determine the distance to the source o ...
stressed out vocab answer key
... Wave Direction: Side to side, or shear Particle Motion: Sideways or perpendicular ...
... Wave Direction: Side to side, or shear Particle Motion: Sideways or perpendicular ...
AIM: Introduce you to scientific study of the world's
... • Longitudinal or compressional component –Travels through rock as regions of compressed and dilated rock –Atoms/molecules move back & forth along lines parallel to direction in which wave travels –Travels through solids and liquids –Travels at higher speeds, & so arrives at distant recording statio ...
... • Longitudinal or compressional component –Travels through rock as regions of compressed and dilated rock –Atoms/molecules move back & forth along lines parallel to direction in which wave travels –Travels through solids and liquids –Travels at higher speeds, & so arrives at distant recording statio ...
Physics - WordPress.com
... 4.7 Investigate the unpredictability of earthquakes, through sliding blocks and weights 4.8 Explain why scientists find it difficult to predict earthquakes and tsunami waves even with available ...
... 4.7 Investigate the unpredictability of earthquakes, through sliding blocks and weights 4.8 Explain why scientists find it difficult to predict earthquakes and tsunami waves even with available ...
velocity structure of the near
... beneath the surface, however due to field methodology, these do not show up in the data record. A reflected P-wave travels down into the earth reflecting back toward the surface equidistantly off of the underlying medium boundaries between the source and receiver. That is, the angle at which the wa ...
... beneath the surface, however due to field methodology, these do not show up in the data record. A reflected P-wave travels down into the earth reflecting back toward the surface equidistantly off of the underlying medium boundaries between the source and receiver. That is, the angle at which the wa ...
Lecture 11 Review
... modulus measures the stiffness of the material lattice, i.e. ∆p change in pressure stress applied β= ...
... modulus measures the stiffness of the material lattice, i.e. ∆p change in pressure stress applied β= ...
Earthquakes2010
... • Reverse: caused by compression (convergence), one block moves up relative to the other • Strike-slip: caused by shear stress (transform), no vertical movement. Blocks slide past each other ...
... • Reverse: caused by compression (convergence), one block moves up relative to the other • Strike-slip: caused by shear stress (transform), no vertical movement. Blocks slide past each other ...
Waves I - Galileo and Einstein
... • Sound waves in air are pressure waves. The obvious variables for dimensional analysis are the pressure [P] = [force/area] = MLT-2/L2 = ML-1T-2 and density [] = [mass/vol] = ML-3. • Clearly P / has the right dimensions, but detailed analysis proves v ...
... • Sound waves in air are pressure waves. The obvious variables for dimensional analysis are the pressure [P] = [force/area] = MLT-2/L2 = ML-1T-2 and density [] = [mass/vol] = ML-3. • Clearly P / has the right dimensions, but detailed analysis proves v ...
File
... and always arrive after P waves. Side to side. (body) • Surface Waves – Cause motion mostly in the upper few KM of earth’s crust. Travel more slowly and are more destructive than body waves. Can move up and down or side to side. ...
... and always arrive after P waves. Side to side. (body) • Surface Waves – Cause motion mostly in the upper few KM of earth’s crust. Travel more slowly and are more destructive than body waves. Can move up and down or side to side. ...
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.