
Document
... Earthquakes: Vibrations (seismic waves) within Earth materials are produced by the rapid release of energy Earth’s crust is in constant motion because of tectonic forces Earth’s crust can store elastic energy When forces exceed the elastic limits and structural strength of the rocks, the rocks ...
... Earthquakes: Vibrations (seismic waves) within Earth materials are produced by the rapid release of energy Earth’s crust is in constant motion because of tectonic forces Earth’s crust can store elastic energy When forces exceed the elastic limits and structural strength of the rocks, the rocks ...
Document
... Earthquakes: Vibrations (seismic waves) within Earth materials are produced by the rapid release of energy Earth’s crust is in constant motion because of tectonic forces Earth’s crust can store elastic energy When forces exceed the elastic limits and structural strength of the rocks, the rocks ...
... Earthquakes: Vibrations (seismic waves) within Earth materials are produced by the rapid release of energy Earth’s crust is in constant motion because of tectonic forces Earth’s crust can store elastic energy When forces exceed the elastic limits and structural strength of the rocks, the rocks ...
Activity 1 quiz File
... a) S-waves b) P-waves c) Surface waves 11) _____ Which type of seismic wave causes the most damage to buildings? a) S-waves b) P-waves c) Surface waves 12) _____ Which type of seismic wave can travel through both solid and liquid material? a) S-waves b) P-waves c) Surface waves 13) _____ The places ...
... a) S-waves b) P-waves c) Surface waves 11) _____ Which type of seismic wave causes the most damage to buildings? a) S-waves b) P-waves c) Surface waves 12) _____ Which type of seismic wave can travel through both solid and liquid material? a) S-waves b) P-waves c) Surface waves 13) _____ The places ...
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 ...
Document
... Off the west coast of northern Sumatra there was an earthquake on December 26, 2004 at 7:58 a.m. It killed 277,898 people. The magnitude was ...
... Off the west coast of northern Sumatra there was an earthquake on December 26, 2004 at 7:58 a.m. It killed 277,898 people. The magnitude was ...
Quiz 5
... C) volcanic bombs D) tsunamis E) xenoliths 3. _______ are the first waves to leave the focus after an earthquake. A) P-waves B) S-waves C) surface waves D) body waves E) shear waves 4. The _______ is the part of the Earth's interior where rocks start to melt. A) lithosphere ...
... C) volcanic bombs D) tsunamis E) xenoliths 3. _______ are the first waves to leave the focus after an earthquake. A) P-waves B) S-waves C) surface waves D) body waves E) shear waves 4. The _______ is the part of the Earth's interior where rocks start to melt. A) lithosphere ...
NAME - Thomas C. Cario Middle School
... 10.) What is the name of the spot on the Earth’s surface directly above where the earthquake takes place? Epicenter 11.) How many seismograph stations are needed to locate an epicenter? 3 12.) What information is needed in order to use a graph to find out how far away an earthquake is from a seismo ...
... 10.) What is the name of the spot on the Earth’s surface directly above where the earthquake takes place? Epicenter 11.) How many seismograph stations are needed to locate an epicenter? 3 12.) What information is needed in order to use a graph to find out how far away an earthquake is from a seismo ...
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 ...
Solid Earth
... There are approximately 12 lithospheric plates on Earth’s surface. Most scientists believe that convection within Earth’s lower and upper Mantle is the major driving force linked to plate motion. Convection is driven my temperature differences/density differences and gravity. ...
... There are approximately 12 lithospheric plates on Earth’s surface. Most scientists believe that convection within Earth’s lower and upper Mantle is the major driving force linked to plate motion. Convection is driven my temperature differences/density differences and gravity. ...
The Stillinger-Weber Potential
... Non-uniform Temperature Profile at Large Shear Rate Time needed to dissipate heat created by applied shear across the whole system ...
... Non-uniform Temperature Profile at Large Shear Rate Time needed to dissipate heat created by applied shear across the whole system ...
Chapter 7 Study Guide
... 13. If an earthquake begins while you are in a building, the safest thing to do is ...
... 13. If an earthquake begins while you are in a building, the safest thing to do is ...
Notes on Earthquakes
... Readings from 3 seismograph stations are needed to locate the epicenter P-waves travel the fastest ...
... Readings from 3 seismograph stations are needed to locate the epicenter P-waves travel the fastest ...
Earthquakes
... - Seismographs are machines attached to the bedrock that measure earthquake waves (seismic waves) - A seismogram is the printed report of the waves. - Richter Scale: a scale from 1-10 that measures the magnitude of an earthquake - Aftershocks are mini earthquakes that occur after an earthquake - Pri ...
... - Seismographs are machines attached to the bedrock that measure earthquake waves (seismic waves) - A seismogram is the printed report of the waves. - Richter Scale: a scale from 1-10 that measures the magnitude of an earthquake - Aftershocks are mini earthquakes that occur after an earthquake - Pri ...
Shear wave splitting

Shear wave splitting, also called seismic birefringence, is the phenomenon that occurs when a polarized shear wave enters an anisotropic medium (Fig. 1). The incident shear wave splits into two polarized shear waves (Fig. 2). Shear wave splitting is typically used as a tool for testing the anisotropy of an area of interest. These measurements reflect the degree of anisotropy and lead to a better understanding of the area’s crack density and orientation or crystal alignment.We can think of the anisotropy of a particular area as a black box and the shear wave splitting measurements as a way of looking at what is in the box.