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Earthquakes
Earthquakes

... Where do earthquakes occur? (cont.) • seismic waves -When rocks move along a fault, they release energy that travels as vibrations on and in Earth • Focus- These waves originate where rocks first move along the fault, at a location inside Earth ...
ASTR178-Week3
ASTR178-Week3

... carbon dioxide, why does the present atmosphere contain oxygen molecules? A. Volcanoes slowly enriched the Earth’s atmosphere with oxygen. B. When life first developed on the Earth, this life produced oxygen from carbon dioxide by photosynthesis. C. Rainwater slowly broke down carbon dioxide into it ...
earthquake
earthquake

... At the Earth's surface, earthquakes manifest themselves by shaking and sometimes displacing the ground. Earthquakes occur due to faults in the Earth's crust, the uppermost layer of the Earth. This happens when there is discontinuity in the rock, so it appears as if there are two plates sliding or sl ...
How are seismic waves generated-Elastic rebound theory Describe
How are seismic waves generated-Elastic rebound theory Describe

... Studies of the different types of seismic waves can tell us much about the nature of the Earth’s structure. For example, seismologists can use the direction and the difference in the arrival times between P-waves and S-waves to determine the distance to the source of an earthquake. If the seismograp ...
S Waves - new-technologies
S Waves - new-technologies

... releases of energy as one land mass slides against another. ...
Mantle Materials
Mantle Materials

... Garnet, Pyroxene • As pressure increases  Pyroxene  Garnet (primarily pyrope) – Increases from 50 to 520 km ...
Natural Disasters ppt
Natural Disasters ppt

...  http://www.geo.mtu.edu/UPSeis/images/P-wave_animation.gif ...
Features of Earthquakes
Features of Earthquakes

... paths of seismic waves changes as they travel through materials with different _______________________.  By studying __________________________ waves that have traveled through Earth, scientists have identified different ____________________________ with different densities.  In general the ______ ...
Earthquakes
Earthquakes

... travel through the crust are called seismic waves. • A seismic wave starts with shaking caused by rocks scraping against each other. • This shaking results in several kinds of seismic waves. • The waves travel at different speeds. • Three kinds: – Primary Waves – P waves – Secondary Waves – S waves ...
- Schoolnet
- Schoolnet

... 3. Due to extreme pressure, the inner core of Earth is A. ...
Seismic Waves File
Seismic Waves File

... The diagram above shows the paths taken by P and S waves as they travel through the interior of the Earth.  Point A - Both P and S waves are gradually refracted as they travel and therefore follow curved paths as they spread out from the epicentre. This indicates that the density of the material wi ...
PLATE TECTONICS and OCEANS
PLATE TECTONICS and OCEANS

... journey can be used to measure the distance of the laser station from the satellite • The amount this changes from year to year can be used to determine plate motions ...
Notes Earthquakes
Notes Earthquakes

... second fastest kind of seismic wave. S-waves are transverse waves. This kind of motion can only be support by materials that are rigid. For this reason, S-waves cannot travel through liquids. After passing through the deep interior of the earth, Swaves re-emerge at the surface only along paths that ...
Match The description in column A to the term in column B column A
Match The description in column A to the term in column B column A

... A. divergent boundary C. can happen at any type of boundary ...
Plate Teconics - FAU-Department of Geosciences
Plate Teconics - FAU-Department of Geosciences

... journey can be used to measure the distance of the laser station from the satellite • The amount this changes from year to year can be used to determine plate motions ...
Evidence for Plate Tectonics
Evidence for Plate Tectonics

... • Fossils of Mesosaurus are found on _______________________ and on Africa. • Coastline _______ is what started the thinking on plate tectonics. • The Appalachian Mts. Match mountains found in _________ when the plates are put back together. • The ____________________ is diverging at a rate of 2.5 ...
Lesson 3
Lesson 3

... • P-waves are also called primary waves because they arrive first. • P-waves cause rock to squeeze and stretch. Imagine a slinky! ...
Sea Floor Spreading
Sea Floor Spreading

... 1. What information from rocks at the mid-ocean ridge gives evidence ...
The inside of the Earth Earth: Main ingredients Masses
The inside of the Earth Earth: Main ingredients Masses

... – To what extent are the tectonic plates glued to the underlying mantle? – How variable is the composition in the mantle? – What action is at the core-mantle boundary? ...
Glossary
Glossary

... frequent, is around the massive Pacific Plate, commonly referred to as the Pacific Ring of Fire, or simply, the Ring of Fire. sea level: the height of the surface of the sea midway between the average high and low tides secondary waves (S waves): waves of energy released during an earthquake or othe ...
Open file
Open file

... mantle and crust allow scientist to determine how the Earth’s interior is structured? (1) The earth is made up of 4 aligned layers: The inner and outer core, mantle and crust. The crust is the solid surface layer that is made up of tectonic plates. These plates can move and when this occurs pressure ...
File
File

... a linear relationship – exponential relationship ...
SOL 5.6 Interrelationships in Earth/Space Systems (Oceans)
SOL 5.6 Interrelationships in Earth/Space Systems (Oceans)

... Spring tides occur when the Earth, Sun, and Moon are in line. This is during the full moon or new moon. During this time the tides are strong causing extremely high tides and extremely low tides. ...
Slide 1
Slide 1

... • When there is an earthquake, energy travels through the earth and can cause damage to buildings and other structures far away. • The amount of damage caused by an earthquake depends on several things such as the strength of the earthquake, how long it lasts, and where it happens. ...
Seismic Waves
Seismic Waves

... through its interior. make the ground roll up and down or shake from side to side. Slowest moving seismic waves Travel on top of Earth’s surface cause the largest ground movements and the most damage as they bend and twist the surface ...
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Ionospheric dynamo region

In the height region between about 85 and 200 km altitude on Earth, the ionospheric plasma is electrically conducting. Atmospheric tidal winds due to differential solar heating or due to gravitational lunar forcing move the ionospheric plasma against the geomagnetic field lines thus generating electric fields and currents just like a dynamo coil moving against magnetic field lines. That region is therefore called ionospheric dynamo region. The magnetic manifestation of these electric currents on the ground can be observed during magnetospheric quiet conditions. They are called Sq-variations (S=solar; q=quiet) and L-variations (L=lunar) of the geomagnetic field.Additional electric currents are generated by the varying magnetospheric electric convection field. These are the DP1-currents (the auroral electrojets) and the polar DP2-currents. Finally, a polar-ring current has been derived from the observations which depends on the polarity of the interplanetary magnetic field. These geomagnetic variations belong to the so-called external part of the geomagnetic field. Their amplitudes reach at most about 1% of the main internal geomagnetic field Bo.
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