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Lab 2: The Interior of the Earth
Lab 2: The Interior of the Earth

... earthquake waves moving through the Earth in the same way you can observe waves moving through water. They can, however, record and study the energy from the earthquake waves as the waves arrive at a recording station (seismograph station). They can use information they record about the waves to mak ...
Earth`s Interior 08
Earth`s Interior 08

... III. Theory of Continental Drift D. Evidence that supports theory = 1. Geologic (rock) 2. Biologic (life) 3. Climatological (past weather) 4. Continental Shelves fit together very well ...
M5.4-Gravity waves
M5.4-Gravity waves

... External Gravity Waves: Density ...
Study outline for Oceanography
Study outline for Oceanography

... Chapter 8 Waves and water dynamics Chapter at a glance: Most waves produced by storms Most move in circular motion In shallow water the physical characteristics of waves change. Tsunamis are high energy waves that can be very destructive. ...
Ch. 22.5 EQ study guide
Ch. 22.5 EQ study guide

... point called a FOCUS. •Vibrations travel from focus through the earth’s crust as waves. •Surface directly above the focus is called the epicenter. ...
Earth Science 12th Edition Vocabulary Chapter 15
Earth Science 12th Edition Vocabulary Chapter 15

... return to the ocean of water that has piled up on the shore by incoming waves. sea arch- an arch formed by wave erosion when caves on opposite sea stack- an isolated mass of rock standing just off shore produced by wave erosion of a head land. seawall- a barrier constructed to prevent waves from rea ...
Ever Changing Earth Test Study Guide Be able to define the
Ever Changing Earth Test Study Guide Be able to define the

... Rift zone Buckling zone Subduction zone Transform zone ...
QUAKE NOTES
QUAKE NOTES

... body waves- waves of energy that travel from the focus of an earthquake within the earth • p-waves- body waves that squeeze and stretch rock materials as they pass through earth, faster • s-waves- body waves that cause particles of ...
Document
Document

... How is an Earthquake’s Epicenter Located? Seismic wave behavior – 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 ...
Slide 1
Slide 1

... EQ Hazards 3. Landslides/ Mudflows – loose soil/rock moves downhill 4. Tsunamis:; caused by water displacement due to EQ at sea (usu. Subduction); ...
What Are Earthquakes?
What Are Earthquakes?

... lithosphere to break up into fault blocks. • These blocks thrust over one another as the plates move. • Two types of earthquakes may occur. • Between the two plates & • Inside the down going plate. ...
Lecture - Ann Arbor Earth Science
Lecture - Ann Arbor Earth Science

... distinct types of seismic waves: * Primary (P) waves * Secondary (S) waves * Surface waves Primary and Secondary waves (also called body waves) travel in all directions from the earthquakes point of origin (called the focus). Surface waves are confined to the upper few hundred miles of the crust. Th ...
Earthquake Waves - davis.k12.ut.us
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. ...
Earthquakes - Boone County Schools
Earthquakes - Boone County Schools

... 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 put them out. This earthquake caused the lengthiest rupture of a fault in U.S. history. People as far as western Nevada and sou ...
Sound - Garnet Valley School District
Sound - Garnet Valley School District

... Standing Wave • A standing wave is a wave that appears to stay in one place – it does not seem to move through the medium. • Node – a point on a standing wave that has no _______________from the rest position. • Antinode – a point where a crest or trough occurs _____________between two nodes. ...
File
File

... or P-waves, travel the fastest, so they are the first to arrive at some other point on Earth’s crust. Secondary waves, or Swaves, arrive next and these tend to cause more damage than P-waves. Although they do not travel as far as primary waves and move at relatively low speeds, surface waves tend to ...
Section 19.1 Forces Within Earth
Section 19.1 Forces Within Earth

... reach a critical point. • At these breaks rocks can move releasing the energy built up as a result of stress. • Earthquakes are the result of this movement and release of energy. ...
Lesson 3
Lesson 3

... 1.At different speeds and 2 In different ways ...
Vocabulary #3
Vocabulary #3

... When waves spread out to fill the space through which they are moving Refraction When a wave changes direction because it goes into a new medium Polarization The specific direction that a transverse wave is vibrating Electromagnetic waves A transverse wave of pure energy that can go through both a m ...
Earth Science – Quiz 2
Earth Science – Quiz 2

... A) P waves travel through solids; S waves do not. B) P and S waves travel through liquids, but P waves do not travel through solids. C) S waves travel through solids and P waves travel through liquids. D) P and S waves travel through liquids, but S waves do not travel through solids. 5. Major earthq ...
chapter 6 earthquakes
chapter 6 earthquakes

... ground when rock (plates) move suddenly and release energy. • aftershock – a release in energy after an earthquake ...
ES Chapter 11 Notes - Ridgefield School District
ES Chapter 11 Notes - Ridgefield School District

... An instrument used to measure the magnitude of an earthquake. A pen (attached to a pendulum) traces a record of Earth’s 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 a ...
Earthquakes
Earthquakes

... • This shaking is what causes most earthquake damage because it is so close to the focus. • As waves travel away from the focus they get weaker. ...
Earthquakes, Volcanoes, tsunamis
Earthquakes, Volcanoes, tsunamis

... weathering of lava. Tambora 1815- Indonesia, largest in recorded history. 71,000 people died from impact alone or starvation and disease afterwards. Ruined agriculture and livestocklead to worst famine in 19th century. ...
Earthquakes - Our Lady of Grace School / Homepage
Earthquakes - Our Lady of Grace School / Homepage

... seismic waves - carry the energy of an earthquake away from the focus, through Earth’s interior, and across the surface The energy is greatest at the epicenter. seismograph - instrument used to record ground movement caused by seismic waves as they move through the Earth ...
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Rogue wave



Rogue waves (also known as freak waves, monster waves, killer waves, extreme waves, and abnormal waves) are relatively large and spontaneous surface waves that occur far out in open water, and are a threat even to large ships and ocean liners.They present two kinds of danger: although rare, they are unpredictable, and may appear suddenly or without warning, and they can impact with tremendous force (a 12 meter wave in the usual ""linear"" model would have a breaking force of 6 million tons per square metre (MT/m2); modern ships are designed to tolerate a breaking wave of 15 MT/m2), but a rogue wave can dwarf both of these figures with a breaking force of 100 MT/m2.In oceanography, rogue waves are more precisely defined as waves whose height is more than twice the significant wave height (Hs or SWH), which is itself defined as the mean of the largest third of waves in a wave record. Therefore, rogue waves are not necessarily the biggest waves found on the water; they are, rather, unusually large waves for a given sea state. Rogue waves seem not to have a single distinct cause, but occur where physical factors such as high winds and strong currents cause waves to merge to create a single exceptionally large wave.Rogue waves can occur in other media than water. In particular, optical rogue waves allow study of the phenomenon in the laboratory. A 2015 paper studied the wave behavior around a rogue wave, including optical, and the Draupner wave, and concluded that ""rogue events do not necessarily appear without a warning, but are often preceded by a short phase of relative order"".
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