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PLATE TECTONICS THEORY
PLATE TECTONICS THEORY

Plate Tectonics
Plate Tectonics

... middle of the ocean, being pushed to the side until it is destroyed in a trench. ...
station 1 earth`s layers
station 1 earth`s layers

Lecture - Chapter 5 - Abiotic Components of Ecosystems
Lecture - Chapter 5 - Abiotic Components of Ecosystems

... Plate Tectonics- study of the processes by which the lithospheric plates move over the asthenosphere Plate Boundary- where 2 plates meet ...
The Mid-Atlantic Ridge and Geomagnetism
The Mid-Atlantic Ridge and Geomagnetism

... in hand. The lab will make the ideas taught to them clearer by giving the students a hands-on activity where they analyze the data in real time. By doing the activity, rather than just hearing about it, they will gain a clearer understanding of the alternating polarity of the ocean floor about the M ...
Lesson-2-WSs-for-Upl..
Lesson-2-WSs-for-Upl..

... Key Concept What evidence indicates that Earth has a solid inner core and a liquid outer core? Directions: Scientists have learned about the interior of Earth in a number of ways, such as by digging deep wells and studying the waves created by earthquakes. Complete each item on the lines provided. ...
Lecture 5b (Plate Tectonics)
Lecture 5b (Plate Tectonics)

... but it does not explain everything: 1. Earthquakes in middle of continent? 2. Early, early Earth? 3. Maybe ancient Mars, but today's Venus? ...
The Theory of Plate Tectonics
The Theory of Plate Tectonics

... Data indicate that earthquakes and volcanic activity do not occur randomly throughout the world. Instead, they occur primarily in concentrated belts, as shown on the map below. The theory of plate tectonics helps explain this pattern because the earthquake and volcano belts mark the locations of pla ...
Plate Tectonics - East Hanover Township School District
Plate Tectonics - East Hanover Township School District

... Earth’s Layers The Earth's rocky outer crust solidified billions of years ago, soon after the Earth formed. This crust is not a solid shell; it is broken up into huge, thick plates that drift atop the soft, underlying mantle. ...
Slide 1
Slide 1

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EARTH DIFFERENTIATES
EARTH DIFFERENTIATES

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19.2 Seismic Waves and Earth`s Interior Seismometer (seismograph
19.2 Seismic Waves and Earth`s Interior Seismometer (seismograph

... Deep-focus earthquakes – This type of earthquake generally produces smaller vibrations at the epicenter than shallow-focus earthquakes. The reason for this is that the rocks at this depth are less rigid (more flexible). They do not have the ability to store a lot of energy. Also the seismic waves mu ...
What "Seis" Shake?
What "Seis" Shake?

... waves due to the way they displace the earth as they travel. S waves do not travel through liquids. This important piece of information has helped scientists to understand the material in the earth's crust, mantle, and core. For example, when seismologists monitor S waves and notice they disappear b ...
Introduction - Winthrop Chemistry, Physics, and Geology
Introduction - Winthrop Chemistry, Physics, and Geology

... Mathematics Computer Science ...
Plate Tectonics
Plate Tectonics

... Types of Plate Boundaries • TRANSFORM BOUNDARIES – These occur when two plates grind past each other in a side to side motion (e.g., San Andreas fault in California) • DIVERGENT BOUNDARIES – Two plates moving apart from each other form this type of boundary. The cooling of the molten rock when it r ...
Plate Tectonics
Plate Tectonics

... • As different plates collide and interact, they cause a number of phenomena. Two moving plates, typically on a Transform Fault, could potentially snag on each other and build up energy. If this energy is released suddenly, it causes an earthquake. • If two colliding plates build up friction, that h ...
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... A. The process of moving materials from their source to another location through weathering. B. The breaking down of rock soil and minerals. C. Magma coming up from the Earth’s mantle through openings in the crust. 2. Wind carrying abrasive materials blows against a rock formation, wearing it down o ...
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Slide 1

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Chapter 28 Notes
Chapter 28 Notes

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Earth`s Layers Review
Earth`s Layers Review

... - AKA- the amount of “stuff” in a given space - Example: limestone is more dense than water, _________________________ Tectonic plates - Solid and found in the _______________________ - Move around on top of the ____________________ Be able to compare and contrast the lithosphere and asthenosphere, ...
Unit - MNPSSocialStudies
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1. The figure shows a uniform magnetic field that is normal
1. The figure shows a uniform magnetic field that is normal

... oxygen atoms emit waves that have a frequency of 5.841 • 1014 Hz. Determine the relative velocity of the galaxy with respect to the astronomer on the earth. Note: The speed of light is 2.9979 • 108 m/s. A) 6.724 • 106 m/s, away from earth B) 6.724 • 106 m/s, toward earth C) 2.931 • 108 m/s, away fro ...
Volcanoes, Earthquakes, Islands . . . Oh My!
Volcanoes, Earthquakes, Islands . . . Oh My!

... What lies beneath the tectonic plates? • Below the lithosphere is the asthenosphere, a layer that is solid, but flows. ...
Objective: Students will diagram faults, waves and volcanoes in
Objective: Students will diagram faults, waves and volcanoes in

... • Scientists found that each magnetic reversal is recorded in the __________________________. • As molten material rises and cools, some magnetic minerals ________________ with the Earth's magnetic field. • When the material hardens, these minerals are fixed in place like tiny ________________ point ...
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Geophysics



Geophysics /dʒiːoʊfɪzɪks/ is a subject of natural science concerned with the physical processes and physical properties of the Earth and its surrounding space environment, and the use of quantitative methods for their analysis. The term geophysics sometimes refers only to the geological applications: Earth's shape; its gravitational and magnetic fields; its internal structure and composition; its dynamics and their surface expression in plate tectonics, the generation of magmas, volcanism and rock formation. However, modern geophysics organizations use a broader definition that includes the water cycle including snow and ice; fluid dynamics of the oceans and the atmosphere; electricity and magnetism in the ionosphere and magnetosphere and solar-terrestrial relations; and analogous problems associated with the Moon and other planets.Although geophysics was only recognized as a separate discipline in the 19th century, its origins go back to ancient times. The first magnetic compasses were made from lodestones, while more modern magnetic compasses played an important role in the history of navigation. The first seismic instrument was built in 132 BC. Isaac Newton applied his theory of mechanics to the tides and the precession of the equinox; and instruments were developed to measure the Earth's shape, density and gravity field, as well as the components of the water cycle. In the 20th century, geophysical methods were developed for remote exploration of the solid Earth and the ocean, and geophysics played an essential role in the development of the theory of plate tectonics.Geophysics is applied to societal needs, such as mineral resources, mitigation of natural hazards and environmental protection. Geophysical survey data are used to analyze potential petroleum reservoirs and mineral deposits, locate groundwater, find archaeological relics, determine the thickness of glaciers and soils, and assess sites for environmental remediation.
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