![P waves](http://s1.studyres.com/store/data/006384533_1-2a4373e35af40283729cf8eda0ada612-300x300.png)
P waves
... Seismic waves that travel along Earth’s surface are called surface waves. Each wave travels through Earth’s layers in a different way and at different speeds. The speed of the seismic wave depends on the kind of material it travels through. Waves that travel through solids, liquids, and gases are ca ...
... Seismic waves that travel along Earth’s surface are called surface waves. Each wave travels through Earth’s layers in a different way and at different speeds. The speed of the seismic wave depends on the kind of material it travels through. Waves that travel through solids, liquids, and gases are ca ...
Chapter 8 - Earthquakes
... of the Earth’s crust are moving over plastic rock. Earthquakes occur at or near fault lines where the sliding action of these tectonic plates causes vibrations felt as earthquakes. Deformation – stress caused by the bending, tilting or folding of rock layers causing them to change shape. Plastic Def ...
... of the Earth’s crust are moving over plastic rock. Earthquakes occur at or near fault lines where the sliding action of these tectonic plates causes vibrations felt as earthquakes. Deformation – stress caused by the bending, tilting or folding of rock layers causing them to change shape. Plastic Def ...
Seismic Waves - Faculty Web Pages
... various paths and speeds depending on the material they are passing through. • Oceanic crust is composed mostly of basalt which is a sedimentary rock allowing waves to travel easily resulting more destruction on the surface. • Continental crust is mostly granite, a igneous rock type, which is of a m ...
... various paths and speeds depending on the material they are passing through. • Oceanic crust is composed mostly of basalt which is a sedimentary rock allowing waves to travel easily resulting more destruction on the surface. • Continental crust is mostly granite, a igneous rock type, which is of a m ...
blocks of crust slide past each other with no up or down motion
... blocks of crust slide past each other with no up or down motion ...
... blocks of crust slide past each other with no up or down motion ...
Ocean Web Quest Task Sheet PLEASE REMEMBER TO WRITE IN
... 14. Tides are created because the Earth and the moon are attracted to each other just like magnets are attracted to each other. The moon tries to pull at anything on the ______ to bring it __________. But, the Earth is able to hold onto everything ____________ ____ ___________. Since the water is al ...
... 14. Tides are created because the Earth and the moon are attracted to each other just like magnets are attracted to each other. The moon tries to pull at anything on the ______ to bring it __________. But, the Earth is able to hold onto everything ____________ ____ ___________. Since the water is al ...
Geology of the Hawaiian Islands
... Measuring the force of earthquakes 3. Duration of shaking Up to tens of seconds 4. Intensity scales Based on damage and human perception 5. Magnitude scales Based on amount of energy released ...
... Measuring the force of earthquakes 3. Duration of shaking Up to tens of seconds 4. Intensity scales Based on damage and human perception 5. Magnitude scales Based on amount of energy released ...
CGF 3MO - TeacherWeb
... what is denudation: weathering/erosion, transportation, deposition. what is mass wasting gradational process: driven by solar energy; gravity and kinetic energy weathering: chemical (decomposition) and mechanical (disintegration) mechanical weathering processes chemical weathering processes karst to ...
... what is denudation: weathering/erosion, transportation, deposition. what is mass wasting gradational process: driven by solar energy; gravity and kinetic energy weathering: chemical (decomposition) and mechanical (disintegration) mechanical weathering processes chemical weathering processes karst to ...
Powerpoint Format ()
... Knight is: Chapter 23, Sections 23.1-23.7 Test 2 will cover up to and including Section 23.7, Thin Lenses and Refraction Theory, plus lab materials from this semester. A masteringphysics Problem Set is due Friday by 5:00 PM. It is the last problem set of 2007. Suggested Chapter 23 Exercises and Prob ...
... Knight is: Chapter 23, Sections 23.1-23.7 Test 2 will cover up to and including Section 23.7, Thin Lenses and Refraction Theory, plus lab materials from this semester. A masteringphysics Problem Set is due Friday by 5:00 PM. It is the last problem set of 2007. Suggested Chapter 23 Exercises and Prob ...
6.7 Earthquake Waves Wave Notes
... 11. Select a student to read aloud the introduction, and as a class follow along. 12. Teacher models for the students by: a. Line up the paperclips so all are facing the same direction b. Let the rubberband and clips come to a rest c. Gently pluck the rubberband so the clips gently rotate as the “S” ...
... 11. Select a student to read aloud the introduction, and as a class follow along. 12. Teacher models for the students by: a. Line up the paperclips so all are facing the same direction b. Let the rubberband and clips come to a rest c. Gently pluck the rubberband so the clips gently rotate as the “S” ...
here
... Information carried by these waves is used to: -Locate the focus of the earthquake. -Calculate the earthquake magnitude. - “See” into the Earth’s interior. ...
... Information carried by these waves is used to: -Locate the focus of the earthquake. -Calculate the earthquake magnitude. - “See” into the Earth’s interior. ...
Study guide - Earthquakes, volcanoes, fault types
... ... the 3 types of faults and the stress that produces each; know direction of each stress type ... the plate boundary that is associated with each fault type and example of each type of boundary ... difference between hanging wall and foot wall and be able to identify each in a fault diagram ... wh ...
... ... the 3 types of faults and the stress that produces each; know direction of each stress type ... the plate boundary that is associated with each fault type and example of each type of boundary ... difference between hanging wall and foot wall and be able to identify each in a fault diagram ... wh ...
Seismology A shaky science
... Studying Earthquake Waves Seismologist study seismograms and can tell a great deal about earthquakes. It can indicate how far way the epicenter is from the seismic station and the energy released by the earthquake. Magnitude- the amount of energy released by an earthquake. Arrival time- the time it ...
... Studying Earthquake Waves Seismologist study seismograms and can tell a great deal about earthquakes. It can indicate how far way the epicenter is from the seismic station and the energy released by the earthquake. Magnitude- the amount of energy released by an earthquake. Arrival time- the time it ...
How and Where Do Earthquakes Occur? Causes of Earthquakes
... • The place underground where the break first occurs is the focus of the earthquake. • The epicenter is the location at Earth’s surface just above the focus. • When the vibrations reach the surface , we feel them as an earthquake, first at the epicenter and then at greater distances from the epicent ...
... • The place underground where the break first occurs is the focus of the earthquake. • The epicenter is the location at Earth’s surface just above the focus. • When the vibrations reach the surface , we feel them as an earthquake, first at the epicenter and then at greater distances from the epicent ...
Short-Hand Notes
... B) The importance of Subduction and ocean trenches 1) Different land formations are formed as a result of an oceanic trench 2) What type of land formations form depends on what types of rock meet ...
... B) The importance of Subduction and ocean trenches 1) Different land formations are formed as a result of an oceanic trench 2) What type of land formations form depends on what types of rock meet ...
Oceanography
... features of sea water a)Define salinity b)Measure salinity c)Define Halocline -Temperature -Density -Describe the causes for ocean circulation a)Interactions between atmosphere and the ocean *Coriolis force b)Thermo Haline circulation c)Define Antarctic intermediate water North Atlantic deep water A ...
... features of sea water a)Define salinity b)Measure salinity c)Define Halocline -Temperature -Density -Describe the causes for ocean circulation a)Interactions between atmosphere and the ocean *Coriolis force b)Thermo Haline circulation c)Define Antarctic intermediate water North Atlantic deep water A ...
ppt. - Science with Ms. Braget
... vibrations that travel through Earth carrying the energy released during an earthquake – They move like ripples on a pond – They carry the energy of an earthquake away from the focus, through Earth’s interior, and across the surface – The energy is greatest the the ...
... vibrations that travel through Earth carrying the energy released during an earthquake – They move like ripples on a pond – They carry the energy of an earthquake away from the focus, through Earth’s interior, and across the surface – The energy is greatest the the ...
PPT
... Compression waves (Pwaves): travel by squeezing and expanding medium they travel through. They can travel through both solids and liquids (e.g., sound waves). Shear waves (S-waves): travel by shearing medium they pass through. S-waves can travel only through solids since particles need to be bonded ...
... Compression waves (Pwaves): travel by squeezing and expanding medium they travel through. They can travel through both solids and liquids (e.g., sound waves). Shear waves (S-waves): travel by shearing medium they pass through. S-waves can travel only through solids since particles need to be bonded ...
Hint: Convert miles into nautical miles
... numbers in a short form by expressing them as powers of ten. To do this, we write the number as the product of a number between one and ten and a power of ten. For example, the total surface area of the world’s oceans is approximately 143,000,000 square miles. To write this in scientific notation, f ...
... numbers in a short form by expressing them as powers of ten. To do this, we write the number as the product of a number between one and ten and a power of ten. For example, the total surface area of the world’s oceans is approximately 143,000,000 square miles. To write this in scientific notation, f ...
Interior of the Earth
... When molten lava solidifies at mid-ocean ridges, iron-containing minerals in the lava align themselves with Earth’s active magnetic field. These minerals record the orientation of the magnetic field at the time they solidified. Click here to see a demonstration of Earth’s alternating magnetic polari ...
... When molten lava solidifies at mid-ocean ridges, iron-containing minerals in the lava align themselves with Earth’s active magnetic field. These minerals record the orientation of the magnetic field at the time they solidified. Click here to see a demonstration of Earth’s alternating magnetic polari ...
Name: ___________________________ Chapter 6 Notes: Earthquakes Stress
... Seismic Waves: vibrations that travel through Earth carrying the energy released during an earthquake Types of Seismic waves P waves: the first wave to arrive ...
... Seismic Waves: vibrations that travel through Earth carrying the energy released during an earthquake Types of Seismic waves P waves: the first wave to arrive ...
File
... Long hill of sand that is deposited a short distance from the shore •Forms parallel to the beach and acts like a dam. •If pressure is great enough – ma break and create a rush of water seaward = called rip currents = fast narrow currents of water ...
... Long hill of sand that is deposited a short distance from the shore •Forms parallel to the beach and acts like a dam. •If pressure is great enough – ma break and create a rush of water seaward = called rip currents = fast narrow currents of water ...
Chapter 11 -2 Study Guide
... Seismic waves that do not travel through the Earth as fast as P waves are called Secondary Waves or S – Waves. S waves travel through solids. -Not liquids or gases Surface Waves or L waves L waves originate (start) on the Earth’s surface at the epicenter. They move along the surface the way wa ...
... Seismic waves that do not travel through the Earth as fast as P waves are called Secondary Waves or S – Waves. S waves travel through solids. -Not liquids or gases Surface Waves or L waves L waves originate (start) on the Earth’s surface at the epicenter. They move along the surface the way wa ...
sinusoidal wave
... string element, the element cannot go any higher, so its velocity must be zero. Because of the downward curvature of the string at that instant, the net force is downward and so the element will move downward immediately after the crest passes. The element continues to move down, speeding up initial ...
... string element, the element cannot go any higher, so its velocity must be zero. Because of the downward curvature of the string at that instant, the net force is downward and so the element will move downward immediately after the crest passes. The element continues to move down, speeding up initial ...
Table of Contents - Mr. Tobin`s Earth Science Class
... push rocks in direction in which wave is traveling. Secondary Wave: S-Waves. Slower than p-waves. Rocks move at right angles in relation to direction of waves. Both P and S waves pass through Earth’s interior. ...
... push rocks in direction in which wave is traveling. Secondary Wave: S-Waves. Slower than p-waves. Rocks move at right angles in relation to direction of waves. Both P and S waves pass through Earth’s interior. ...
Wind wave
![](https://commons.wikimedia.org/wiki/Special:FilePath/Wedge_Newport_Hurricane_Marie_photo_D_Ramey_Logan.jpg?width=300)
In fluid dynamics, wind waves, or wind-generated waves, are surface waves that occur on the free surface of oceans, seas, lakes, rivers, and canals or even on small puddles and ponds. They result from the wind blowing over an area of fluid surface. Waves in the oceans can travel thousands of miles before reaching land. Wind waves range in size from small ripples, to waves over 100 ft (30 m) high.When directly generated and affected by local winds, a wind wave system is called a wind sea. After the wind ceases to blow, wind waves are called swells. More generally, a swell consists of wind-generated waves that are not significantly affected by the local wind at that time. They have been generated elsewhere or some time ago. Wind waves in the ocean are called ocean surface waves.Wind waves have a certain amount of randomness: subsequent waves differ in height, duration, and shape with limited predictability. They can be described as a stochastic process, in combination with the physics governing their generation, growth, propagation and decay—as well as governing the interdependence between flow quantities such as: the water surface movements, flow velocities and water pressure. The key statistics of wind waves (both seas and swells) in evolving sea states can be predicted with wind wave models.Although waves are usually considered in the water seas of Earth, the hydrocarbon seas of Titan may also have wind-driven waves.