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. ...
... 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. ...
Earthquakes and Volcanoes
... Why do Earthquakes Occur? • Stress builds up at a fault • Stress is a force that adds potential energy to the rock • As soon as the rock slips, energy is released ...
... Why do Earthquakes Occur? • Stress builds up at a fault • Stress is a force that adds potential energy to the rock • As soon as the rock slips, energy is released ...
Seismic Waves
... Scientist study earthquakes to know more about the earth. To study earthquakes scientist use seismographs. Seismographs measures the the movement and vibration of earthquakes. It also tells what kind of seismic wave it is. Seismic waves are vibrations caused by rocks moving or breaking along faults ...
... Scientist study earthquakes to know more about the earth. To study earthquakes scientist use seismographs. Seismographs measures the the movement and vibration of earthquakes. It also tells what kind of seismic wave it is. Seismic waves are vibrations caused by rocks moving or breaking along faults ...
Document
... 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. ...
HERE
... • They cannot travel through liquids, so they cannot travel through the outer core. • The wave is called a shear wave. Matter is moved perpendicular to motion of energy. (*** Your chem teacher would call this a transverse wave). ...
... • They cannot travel through liquids, so they cannot travel through the outer core. • The wave is called a shear wave. Matter is moved perpendicular to motion of energy. (*** Your chem teacher would call this a transverse wave). ...
Study Guide Chapter 4 – Earthquakes GPS: S6E5. Students will
... from side to side as well as up and down, shake structures violently, and can only move through solids – not through liquids. 12. __________________________ move more slowly than P waves and S waves, but they can produce severe ground movements making the ground roll like ocean waves or shake buildi ...
... from side to side as well as up and down, shake structures violently, and can only move through solids – not through liquids. 12. __________________________ move more slowly than P waves and S waves, but they can produce severe ground movements making the ground roll like ocean waves or shake buildi ...
Magma Supply Vs Magma Plumbing
... What is an Earthquake • “An earthquake is a sudden and sometimes catastrophic movement of a part of the Earth's surface. Earthquakes result from the dynamic release of elastic strain energy that radiates seismic waves. Earthquakes typically result from the movement of faults, planar zones of deform ...
... What is an Earthquake • “An earthquake is a sudden and sometimes catastrophic movement of a part of the Earth's surface. Earthquakes result from the dynamic release of elastic strain energy that radiates seismic waves. Earthquakes typically result from the movement of faults, planar zones of deform ...
name________________________
... A. BLAMING SOMEONE ELSE FOR WHAT YOU DID B. THE MOVEMENTS OF ROCK ALONG A FAULT C. THE VIBRATION OF CRUST D. NONE OF THESE 15. IN REGARD TO WAVES, HERTZ IS THE SAME AS A. VELOCITY B. FREQUENCY 16. DRAW IN AND LABEL ALL FOUR BASIC LAYERS OF THE EARTH ...
... A. BLAMING SOMEONE ELSE FOR WHAT YOU DID B. THE MOVEMENTS OF ROCK ALONG A FAULT C. THE VIBRATION OF CRUST D. NONE OF THESE 15. IN REGARD TO WAVES, HERTZ IS THE SAME AS A. VELOCITY B. FREQUENCY 16. DRAW IN AND LABEL ALL FOUR BASIC LAYERS OF THE EARTH ...
Inside the Earth
... A earthquake is a movement or vibration of the earth. They are caused by the release of stored energy in earths outer layer.This release of energy causes sudden shifts of rocks along faults ...
... A earthquake is a movement or vibration of the earth. They are caused by the release of stored energy in earths outer layer.This release of energy causes sudden shifts of rocks along faults ...
Topic 5
... - faster than surface but slower than primary - can pass only through solids - medium amount of damage ...
... - faster than surface but slower than primary - can pass only through solids - medium amount of damage ...
Earthquakes
... other and collide; as the plates move, the overriding plate scrapes across the top of the subducting plate. Divergent Oceanic environments – Make up the midocean ridges, plates are moving away from each other. Spreading causes earthquakes. ...
... other and collide; as the plates move, the overriding plate scrapes across the top of the subducting plate. Divergent Oceanic environments – Make up the midocean ridges, plates are moving away from each other. Spreading causes earthquakes. ...
Vocab-Chapter 8
... ____________________________ 1. The study of earthquakes. ____________________________ 2. An area on the Earth’s surface where no direct seismic waves from a particular earthquake can be detected. ____________________________ 3. The point inside the Earth where an earthquake begins. ________________ ...
... ____________________________ 1. The study of earthquakes. ____________________________ 2. An area on the Earth’s surface where no direct seismic waves from a particular earthquake can be detected. ____________________________ 3. The point inside the Earth where an earthquake begins. ________________ ...
earthquakes - Archway Chandler
... 1. normal – caused by tension 2. reverse (thrust) – caused by compression 3. strike-slip – caused by shearing ...
... 1. normal – caused by tension 2. reverse (thrust) – caused by compression 3. strike-slip – caused by shearing ...
Physics - WordPress.com
... earthquakes and tsunami waves even with available data © Pearson Education Ltd 2011. Copying permitted for purchasing institution only. This material is not copyright free. This document may have been altered from the original. ...
... earthquakes and tsunami waves even with available data © Pearson Education Ltd 2011. Copying permitted for purchasing institution only. This material is not copyright free. This document may have been altered from the original. ...
earthquakes
... • Shaking and trembling of the earth’s crust. • About 8000 occur every day or one every 11 seconds • Caused by plates sliding beside each other • Tsunami - earthquake on the ocean floor: causing waves to become greater than 20 meters high ...
... • Shaking and trembling of the earth’s crust. • About 8000 occur every day or one every 11 seconds • Caused by plates sliding beside each other • Tsunami - earthquake on the ocean floor: causing waves to become greater than 20 meters high ...
Sequence of events in an Earthquake
... above. This shaking generally lasts for less than 40 seconds. Primary waves radiate in all directions from the focus on the earthquake. There are three different types of seismic waves: P waves, S waves and L waves. P waves (primary waves) travel rapidly. They are sound waves and can move through so ...
... above. This shaking generally lasts for less than 40 seconds. Primary waves radiate in all directions from the focus on the earthquake. There are three different types of seismic waves: P waves, S waves and L waves. P waves (primary waves) travel rapidly. They are sound waves and can move through so ...
lecture * 2011 japanese tsunami and wave properties
... by focusing due to refraction. The tsunami caused one death in northern California when a man standing on a pier photographing the event was swept away and drowned. ...
... by focusing due to refraction. The tsunami caused one death in northern California when a man standing on a pier photographing the event was swept away and drowned. ...
Ch - saddlespace.org
... and forth motion. These waves are usually not felt (6-10km/sec). Can travel thru any material. (solid, liquid or gas) S-Waves or Secondary waves travel at right angles to their direction in a Side to Side motion. These waves travel only through solids. (3-6Km/sec) L-Waves are the last and slowest (1 ...
... and forth motion. These waves are usually not felt (6-10km/sec). Can travel thru any material. (solid, liquid or gas) S-Waves or Secondary waves travel at right angles to their direction in a Side to Side motion. These waves travel only through solids. (3-6Km/sec) L-Waves are the last and slowest (1 ...
Earth`s Structural Key Elements
... – Measures strength based on area size that the fault moved, average distance that fault blocks move, and rigidity of blocks in fault zone – The greater the number, the stronger the (E). < 2.5 not felt by people – 6.9 Kobe, Japan 1995 ...
... – Measures strength based on area size that the fault moved, average distance that fault blocks move, and rigidity of blocks in fault zone – The greater the number, the stronger the (E). < 2.5 not felt by people – 6.9 Kobe, Japan 1995 ...
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"".