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Natural Disasters
Natural Disasters

Chapter 5
Chapter 5

... Focus: (aka hypocenter) the point underground where the release of stress is located Epicenter: the point on the earth’s surface directly above the focus Aftershock: an earthquake that occurs after a larger earthquake in the same area. Liquefaction: earthquake's violent shaking suddenly turns loose, ...
Essentials of Geology Earthquakes and Earth`s
Essentials of Geology Earthquakes and Earth`s

... • P waves arrive first, then S waves, then L and R • Average speeds for all these waves is known • After an earthquake, the difference in arrival times at a seismograph station can be used to calculate the distance from the seismograph to the epicenter. ...
ES Chapter 11 Notes - Ridgefield School District
ES Chapter 11 Notes - Ridgefield School District

... vibrations onto a sheet of paper. It records all 3 types of waves. **DRAW & LABEL A DIAGRAM OF A SEISMOGRAPH** * if S + P waves are close together  EQ is nearby * if S + P waves are far apart  EQ is far away **DRAW SEISMOGRAPH RESULTS & LABEL AS “NEAR” OR “FAR”** ...
Earthquakes - Boone County Schools
Earthquakes - Boone County Schools

... earthquake killed over 3,000 people and caused $524 million in property loss. The damage in San Francisco alone was over $20 million. Due to broken pipelines, water was shut off to the entire city. Many fires soon broke out throughout the city and caused major devastation as there was no water to pu ...
Oceanography
Oceanography

... 1. crest – highest point of a wave 2. trough – lowest point of a wave 3. wavelength – distance between 2 adjacent wave crests or wave troughs 4. wave frequency – the number of waves that pass a point in a certain amount of time 5. wave period – time between the passage of two wave crests(or troughs) ...
Seismic Wave
Seismic Wave

... for the damage and destruction associated with earthquakes. There are two types of surface waves: Love waves and rayleigh waves. A Love seismic wave is the fastest surface wave and moves the ground from sideto-side. Confined to the surface of the crust, Love waves produce entirely horizontal motion. ...
EARTHQUAKES & VOLCANOES
EARTHQUAKES & VOLCANOES

... Seismology is the study of earthquakes and seismic waves that move through and around the earth. A seismologist is a scientist who studies earthquakes and seismic waves. What Are Seismic Waves? • Seismic waves are the waves of energy caused by the sudden breaking of rock within the earth or an explo ...
M5.4-Gravity waves
M5.4-Gravity waves

... External Gravity Waves: Density ...
Earthquakes
Earthquakes

... B. Epicenter – the location on the surface directly above the focus. ...
Tsunami - BrainPOP
Tsunami - BrainPOP

... b. Tsunamis are caused by the natural cycle of tides c. Tsunamis occur in seas and lakes, not oceans d. Boats usually float on large waves 5. How do tsunami waves compare to regular ocean waves? a. They're generally much flatter b. They're generally much wider c. They extend deeper underneath the wa ...
Study Guide for Oceanography Test 2016
Study Guide for Oceanography Test 2016

... Study Guide for Oceanography Test ...
Earthquakes
Earthquakes

...  Focus  The location in the Earth’s crust where the earthquake occurs.  It can occur anywhere between the surface and a depth of 700 km. The closer to the surface it occurs, the more powerful the earthquake is.  Epicenter  The location on the Earth’s surface above the focus. ...
Earthquake Summary Sheet
Earthquake Summary Sheet

... 1. earthquake: the release of tension (energy) built up from the movement of plates along plate boundaries 2. fault: a break along the rocks where earthquakes occur 3. focus: place inside the Earth where the earthquake starts 4. epicenter: place on the Earth’s surface directly above the focus 5. sei ...
Seismic Waves and Earth`s Interior PPT Name
Seismic Waves and Earth`s Interior PPT Name

... the San Andreas Fault in California. The energy of earthquakes moves away from the focus in all directions. While some of the waves occur on the surface, other waves of energy move through the planet at very deep levels. The large earthquake that triggered the tsunami of 2004 sent waves of energy th ...
Oceanography Review! Told you it was short!
Oceanography Review! Told you it was short!

... world’s oceans called what? 10. The oceans contain approximately _____________% of all the Earth’s water. ...
Class2atxt
Class2atxt

... – More calm and constant – Along divergent boundaries or at hot spots – Relatively less dangerous ...
- Google Sites
- 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) ...
Principles of Geology
Principles of Geology

... The major branches of the travel-time curves carry the same descriptions as for shallow-focus events. Waves leaving the focus in an upward direction, and reflected at the surface are described by the letters p, s, as follows: ...
Tsunami - BrainPOP
Tsunami - BrainPOP

... b. Tsunamis are caused by the natural cycle of tides c. Tsunamis occur in seas and lakes, not oceans d. Boats usually float on large waves 5. How do tsunami waves compare to regular ocean waves? a. They're generally much flatter b. They're generally much wider c. They extend deeper underneath the wa ...
Ch. 5 - Power Point Review
Ch. 5 - Power Point Review

... 2. Place seismograms on a time distance chart 3. Line up seismogram (P & S waves on time ...
Ch. 1 Layers of the Earth
Ch. 1 Layers of the Earth

... Seismic Waves: There are 2 types of seismic waves. These waves are called Primary Waves and Secondary Waves. 1. P- Waves travel through solids, liquids, & gases. And also travel at a faster rate than S-waves. ...
Earthquakes and Volcanoes
Earthquakes and Volcanoes

... immediately above the focus ◦ Damage from earthquakes are usually greatest at the epicenter ...
P wave - LSMS Ms. Benson GT
P wave - LSMS Ms. Benson GT

... layers of different material. Scientists use the difference in arrival times of reflected and refracted waves from distant earthquakes to construct a picture of what the Earth’s interior looks like. P waves and S waves have allowed scientists to determine indirectly the internal structure of the Ear ...
Earthquakes - staffordscience
Earthquakes - staffordscience

... year, more than 30,000 earthquakes occur worldwide that are strong enough to be felt.  Only about 75 major earthquakes take place each year and often occur in remote regions  Essential Question: How do we locate an earthquake’s epicenter? ...
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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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