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PHYSICS 571 – Master`s of Science Teaching “Electromagnetism
PHYSICS 571 – Master`s of Science Teaching “Electromagnetism

Plate Tectonics
Plate Tectonics

magnetic field
magnetic field

... • The motion of charges cause magnetism. Example: Currents, spinning electrons. ...
Continental Drift
Continental Drift

`magnetic field`.
`magnetic field`.

... • Named after region where it was discovered: the Greek island of Magnesia ...
Earth`s Interior Information- Core-Innermost layer Inner Core
Earth`s Interior Information- Core-Innermost layer Inner Core

... currents flow up towards the lithosphere Asthenosphere-Not liquid, but there is melted rock, carries the lithosphere, moves slowly Lithosphere-broken into giant plates that fit around the globe like puzzle pieces. The pieces move a little bit each year. They slide on a somewhat liquid asthenosphere ...
Magnetic Fields
Magnetic Fields

... monopoles, as these are called are predicted by some theories, but their existence has not been confirmed. One way to produce a magnetic field is to use moving electric charges to create an electromagnet. This is done in motors, telephones and computer disk drives as well as many other places. Magne ...
Experiment 5: Magnetic Fields of a Bar Magnet and of the Earth
Experiment 5: Magnetic Fields of a Bar Magnet and of the Earth

... Identify the direction in the x-y plane in which the horizontal component of the magnetic field is largest. (Unless you’re clever about how you “Tare” the sensor, your measured field component will probably NOT be symmetric about zero). Mark this direction as best you can, with a ruler or pencil on ...
Effects of a Magnetic Field on Fuel
Effects of a Magnetic Field on Fuel

... are paired. For want of a truly intimate knowledge, we say that one electron of an electron pair is spinning in one direction and the other electron of the pair spinning in the opposite direction. Paired electrons with this balanced arrangement exhibit no external magnetic activity, because the spin ...
Plate Tectonics
Plate Tectonics

... In 1908 Taylor and Baker noticed a correlation of global mountain chains. ...
Maxwell`s equations
Maxwell`s equations

... Maxwell’s equation are extensions of the known work of Gauss ,Faradays and Ampere. There are two forms of Maxwell’s equation namely: ...
Atmosphere – The various layers of air that surround Earth. The
Atmosphere – The various layers of air that surround Earth. The

Nanowire by Tunneling Magnetoresistive Sensor
Nanowire by Tunneling Magnetoresistive Sensor

A Brief History of the Earth
A Brief History of the Earth

... subsection. Paste in the urls of the websites you use. Do not move on to the next question without citing because that is also a form of plagiarism if you used the page to paraphrase. Wikipedia (nor any wiki) may be used. 1. What is the “Big Bang” theory. What elements were most abundant in the univ ...
Solid State 2 – Homework 9  Use the Maxwell equation
Solid State 2 – Homework 9 Use the Maxwell equation

... Suppose a material is a perfect conductor. Apply an external magnetic field. What is the magnetic field in the material? Explain ! Suppose the material is a perfect conductor only at temperatures below Tc. Start with a sample at T>Tc, apply an external magnetic field and then, keeping the external f ...
Blizzard Bag 1 - Maplewood Career Center
Blizzard Bag 1 - Maplewood Career Center

... were found by the Greeks more than 2000 years ago. These stones, called lodestones, had the unusually property of attracting pieces of iron. Magnets were first fashioned into compasses and used for navigation by the Chinese in the twelfth century. In the sixteenth century, William Gilbert, Queen Eli ...
Earth`s Structures and Earthquake Study Guide
Earth`s Structures and Earthquake Study Guide

... 28. In a strike-slip fault, the rocks on either side of the fault slip past each other sideways with little up-or-down motion. 29. The Mercalli Scale would most likely be used to tell how much earthquake damage was done to homes and other buildings. 30. A fold in rock that bends upward into an arch ...
Lecture 20
Lecture 20

A Day on Earth Rotation Notes
A Day on Earth Rotation Notes

... A Day on Earth Rotation Notes 1. All planets rotate. 2. The Earth spins on its axis. 3. One rotation = One day = 24 hours. 4. An orbit is the circular path a planet makes around the sun. 5. Planets orbit the sun and moons orbit their planets. 1 orbit = 1 year. 6. Orbit + tilt of planet give us our s ...
Introduction to magnetism
Introduction to magnetism

... once a copious source of loadstones. Since magnetite is already magnetized when found in nature, it is called natural magnet. Magnets that are made by man are called artificial magnets. The magnetic compass, which is obtained by magnetizing an iron needle by contact with another magnet, was invented ...
Plate Tectonics Notes
Plate Tectonics Notes

... 2) Asthenosphere (weak sphere)—inner layer, including the rest of the upper mantle (it doesn’t include the lower mantle or core!) - Hotter than the lithosphere - very close to the melting point, so it’s very plastic (viscous), flows slowly—it’s also more dense The lithosphere “floats” on the Astheno ...
The Structure of the Earth
The Structure of the Earth

SA Power Networks 1 Electric and Magnetic Fields
SA Power Networks 1 Electric and Magnetic Fields

6. Magnets and Motors
6. Magnets and Motors

... Experiment with additional magnets to see if you can change the speed of the motor. For example, hold another magnet with your fingers and bring it near the coil from above, facing the original magnet, as the motor is operating. Questions for Data and Discussion 1. Estimate how many revolutions per ...
Word
Word

... 19) A magnet is dropped down a copper tube and it falls much slower than an otherwise identical but demagnetised magnet did. This is because the magnet a) is repelled by a permanent magnetic field b) is repelled by an induced magnetic field c) experiences more air resistance d) both answers b) and c ...
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History of geomagnetism



The history of geomagnetism is concerned with the history of the study of Earth's magnetic field. It encompasses the history of navigation using compasses, studies of the prehistoric magnetic field (archeomagnetism and paleomagnetism), and applications to plate tectonics.Magnetism has been known since prehistory, but knowledge of the Earth's field developed slowly. The horizontal direction of the Earth's field was first measured in the fourth century BC but the vertical direction was not measured until 1544 AD and the intensity was first measured in 1791. At first, compasses were thought to point towards locations in the heavens, then towards magnetic mountains. A modern experimental approach to understanding the Earth's field began with de Magnete, a book published by William Gilbert in 1600. His experiments with a magnetic model of the Earth convinced him that the Earth itself is a large magnet.
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