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Welcome to the Segment One Final Review
Welcome to the Segment One Final Review

... All waves have these properties in common – but why they are important might be different Amplitude of a sound wave determines loudness or softness while amplitude of a light wave determines brightness ...
Weathering, Erosion and Deposition Presentation (PowerPoint)
Weathering, Erosion and Deposition Presentation (PowerPoint)

... ...
Weather and Climate Test Review Sheet (6th Grade)
Weather and Climate Test Review Sheet (6th Grade)

... A hurricane is a storm with winds over 120 km/h that can last several weeks. Earth’s oceans cover nearly ¾ (75%) of Earth’s surface. Water for Earth’s oceans originally came from water vapor from volcanoes. Photosynthesis is a process that needs sunlight as a source of energy to make food. The therm ...
Blank Jeopardy - Fort Thomas Independent Schools
Blank Jeopardy - Fort Thomas Independent Schools

... Mechanical waves such as sound waves travel fastest through this ...
Chapter 19
Chapter 19

... moving side-by-side by shear stress. ...
lecture * 2011 japanese tsunami and wave properties
lecture * 2011 japanese tsunami and wave properties

... this point the overriding plate springs back. When any vertical motions occur in the ocean, the water is disturbed vertically and tsunami waves are produced. ...
Types of Ocean waves
Types of Ocean waves

... of long wave length and low height approach a gently sloping beach, the ellipse becomes horizontal. When the waves break, the swash sweeps up the beach as a sheet of water often reaching the upper beach. Most of the swash soaks into the beach which means that there is very little backwash. Waves of ...
Waves
Waves

... Waves Earthquakes produce 3 types of waves with different behavior as they travel through materials ...
New Title - TeacherWeb
New Title - TeacherWeb

... travel through different kinds of materials at different rates. For example, a type of seismic wave called a P wave travels through crust material at an average speed of 6 km/sec. But through the uppermost mantle material, P waves travel at an average speed of 8 km/sec. Geologists use their knowledg ...
InAConchShell - some tryout study material
InAConchShell - some tryout study material

... seiche: standing wave; tsunami: seismic sea waves Wind-generated waves controlled by 4 factors: wind velocity, wind duration, fetch (area wind blows over), and original sea state. Fully developed sea: name says what it means; significant wave height: average of top 1/3. ...
Earthquake Quiz - cohort6science
Earthquake Quiz - cohort6science

... _______________11. The type of stress that pushes rock together causing a collision is tension. _______________12. The focus is the point on the Earth’s surface where an earthquake begins. _______________13. Compression is a type of stress that causes the Earth’s landforms to change shape. _________ ...
Chapter 8
Chapter 8

... of the asthenosphere ...
Chapter 12-1
Chapter 12-1

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practice exam
practice exam

... 29) A deep water wave is one that is moving through water that is deeper than: a) 200 m b) three times its height c) ½ its wavelength d) 3000 m e) 11,022 m 30) The horizontal distance between successive crests is the: a) wavelength b) wave height c) wave crest d) wave trough e) wave period 31) A wav ...
Ocean Waves
Ocean Waves

... As the wave passes, water particles move in a circular path They swing forward and down with the energy of the wave, then back up to their original position Winds affects the water at the surface more than it affects the deep water Below a certain depth, the water does not move at all ...
plate tectonics/earthquakes/volcanoes pangea—large
plate tectonics/earthquakes/volcanoes pangea—large

... ...
Wind Erosion
Wind Erosion

... wave, while more energy is given to the ‘top’ or crest. Water waves are primarily transverse waves, in which particles move up and down while the wave travels in a horizontal direction. ...
chapter 2 - HCC Learning Web
chapter 2 - HCC Learning Web

... F. 1968= Plate tectonics (Name change because the ocean crust moves as well as the continents)) G. Mechanism that moves the plates? Convection Currents occurring in the mantle- heat From the radioactive core rises II Seismic Waves A. Types 1. Primary or P Waves, Push and pull, fastest seismic wave, ...
Waves Fact Sheet Anything that causes water to move can produce
Waves Fact Sheet Anything that causes water to move can produce

... changes in atmospheric pressure, underwater volcanic eruptions, the movement of ships, or even fish jumping. The most common cause of surface waves in the ocean is the wind blowing across the water. Once set in motion by the wind, as long as the wave is in deep water, the energy of the waves is pass ...
Earthquake Definitions - Red Hook Central Schools
Earthquake Definitions - Red Hook Central Schools

... · Stress and pressure builds up and causes the plate to become deformed (bend) as it continues to try and move (the plates are elastic-they can change shape). · Eventually, the pressure is great enough to overcome the friction and the plates slip past one another. · The plate movement is the earthqu ...
WHERE DO EARTHQUAKES OCCUR? WHAT CAUSES
WHERE DO EARTHQUAKES OCCUR? WHAT CAUSES

... 15. Seismic waves that travel through Earth’s interior are _________________________. 16. Seismic waves that travel along Earth’s surface are ___________________________. 17. What is the name of the body wave that arrives second? _______________________. 18. Which seismic wave is the fastest and arr ...
Earth Quakes
Earth Quakes

... waves: the slowest type of waves which only travel along the Earth’s surface, not the interior like the S and P body waves.  Surface waves usually cause the most destruction because they move the ground and take the longest time to pass.  The point where the waves originate is where the rock fails ...
Earthquake Locations/Terminology Elastic Rebound Theory Seismic
Earthquake Locations/Terminology Elastic Rebound Theory Seismic

...  Faults: Breaks in ...
Seismic Waves
Seismic Waves

... ...
Waves and Tides
Waves and Tides

... When the trough of a wave gets close to land, it starts to drag while the crest moves on, getting higher and higher until it tumbles over. ...
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Wind wave



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.
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