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Magnetic Properties - Help, Science!
Magnetic Properties - Help, Science!

... • How do we apply this concept? – Power is supplied to houses everywhere in the developed world. In the power grid, voltage can be as high as 765000V. This power is stepped down to 72000V at your local substation. From here, the power is stepped down to about 220V at a transformer on a utility pole. ...
Chapter 19 Magnetism
Chapter 19 Magnetism

Magnetic field lines
Magnetic field lines

... permanently magnetized materials since the high temperatures of the core prevent materials from retaining permanent magnetization  The most likely source of the Earth’s magnetic field is believed to be electric currents in the liquid part of the core ...
SATMAGAN S135 MAGNETIC ANALYZER
SATMAGAN S135 MAGNETIC ANALYZER

File - Help, Science!
File - Help, Science!

Electric and Magnetic Forces and the Modern Day Compass
Electric and Magnetic Forces and the Modern Day Compass

Physics 1002 – Magnetic Fields (Read objectives on screen
Physics 1002 – Magnetic Fields (Read objectives on screen

... We know that a magnetic field surrounds the earth, and its shape is like one that would surround a strong bar magnet placed at the earth’s center, like this. But to answer to the question, “Where does the earth’s magnetic field come from?”: We’re not sure. We know there is not a magnetized hunk of i ...
MAGNETISM
MAGNETISM

WBL6_Lecture_Ch19
WBL6_Lecture_Ch19

Powerpoint Presentation Physical Geology, 10/e
Powerpoint Presentation Physical Geology, 10/e

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Household Magnets

... pushes north poles northward, south poles southward exerts torques on magnetic dipoles, such as compasses ...
Magnetism
Magnetism

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What is a Magnetic Monopole?

... Dipole model describes the interactions (not point charges, but oriented dipoles) Dirac string not infinitely thin, rather an observable flux tube Divergence is always zero ...
Nanostorage - Max-Planck
Nanostorage - Max-Planck

... antivortex, fuses with the original vortex core, with the two destroying each other. In the end, only the second of the two additional magnetic needles remains and forms a new vortex core − and it points in the opposite direction from the original vortex core. It was this discovery that suggested th ...
Magnetic.. - PhysicsEducation.net
Magnetic.. - PhysicsEducation.net

File
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... iv) Magnetic Axis is a straight line passing through the magnetic poles of the earth. It is inclined to Geographic Axis nearly at an angle of 17°. v) Magnetic Meridian at any place is a vertical plane passing through the magnetic north and south poles of the earth. vi) Magnetic Equator is a great ci ...
Magnetic Effect of Electric Current
Magnetic Effect of Electric Current

... The pole of a magnet which points toward north direction is called north pole or north seeking. The pole of a magnet which points toward south direction is called south pole or south seeking. Like poles of magnets repel each other while unlike poles of magnets attract each other. Similar to other ef ...
What is a Magnet?
What is a Magnet?

... consists of atoms and molecules that each have a magnetic field and are positioned to reinforce each other. They do not lose their property of magnetism that’s why they are called permanent magnets. ...
A rotating coil - Collins.co.uk.
A rotating coil - Collins.co.uk.

Zeeman effect - University of Toronto Physics
Zeeman effect - University of Toronto Physics

Magnetic Moment
Magnetic Moment

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Plate Tectonics Exercises

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Compass Navigation Terminology

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Continental Drift

UNIT 2 THE BODY
UNIT 2 THE BODY

... MAGNETS HAVE TO POLES: NORTH AND SOUTH Opposite poles attract. Same poles repel LIKEWISE ELECTRICAL CHARGES ...
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Earth's magnetic field



Earth's magnetic field, also known as the geomagnetic field, is the magnetic field that extends from the Earth's interior to where it meets the solar wind, a stream of charged particles emanating from the Sun. Its magnitude at the Earth's surface ranges from 25 to 65 microteslas (0.25 to 0.65 gauss). Roughly speaking it is the field of a magnetic dipole currently tilted at an angle of about 10 degrees with respect to Earth's rotational axis, as if there were a bar magnet placed at that angle at the center of the Earth. Unlike a bar magnet, however, Earth's magnetic field changes over time because it is generated by a geodynamo (in Earth's case, the motion of molten iron alloys in its outer core).The North and South magnetic poles wander widely, but sufficiently slowly for ordinary compasses to remain useful for navigation. However, at irregular intervals averaging several hundred thousand years, the Earth's field reverses and the North and South Magnetic Poles relatively abruptly switch places. These reversals of the geomagnetic poles leave a record in rocks that are of value to paleomagnetists in calculating geomagnetic fields in the past. Such information in turn is helpful in studying the motions of continents and ocean floors in the process of plate tectonics.The magnetosphere is the region above the ionosphere and extends several tens of thousands of kilometers into space, protecting the Earth from the charged particles of the solar wind and cosmic rays that would otherwise strip away the upper atmosphere, including the ozone layer that protects the Earth from harmful ultraviolet radiation.
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