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Historical Geology, Plate Tectonics, and
Historical Geology, Plate Tectonics, and

Do now! - MrSimonPorter
Do now! - MrSimonPorter

Chapter 6 Part1: Multiple choices
Chapter 6 Part1: Multiple choices

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Magnets - OptionsHighSchool
Magnets - OptionsHighSchool

... The difference between them is that magnetic poles do not exist without both north and south poles together, whereas electric charges, such as plus and minus, can exist alone. ...
What is a Magenit? - Spring Branch ISD
What is a Magenit? - Spring Branch ISD

... The field has many lines, like you have many fingers You get slapped (feel a force) which the palm of the hand If a person needs to go we use the thumb ...
Chapter 17 Vocabulary
Chapter 17 Vocabulary

... slowly moved to their present positions. Pangaea (p.444) Ancient landmass made up of all the continents that began to break apart about 200 million years ago. Isochron (p. 452) Line on the map that connects points of the same age. Magnetic Reversal (p. 451) Changes in the Earth’s magnetic field over ...
Magnetic electricity
Magnetic electricity

... Magnetic monopoles were first predicted to exist over a century ago, as a perfect analogue to electric charges. Although there are protons and electrons with net positive and negative electric charges, there were no particles in existence which carry magnetic charges. Rather, every magnet has a "nor ...
N2-1,2,3 Study Guide
N2-1,2,3 Study Guide

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Skeleton

... Our best reading pointed almost directly to the magnetic South Pole – perhaps off by 2 degrees at most. The reading was 0.022 mT. c) Turn the detector surface in the opposite direction and verify that the minimum value is achieved there. Yes, it worked. The reading in the opposite direction was -0.0 ...
Magnets and Magnetic Field
Magnets and Magnetic Field

... Why are things magnetic? • All moving charges cause a magnetic field – All of the electrons within an object moving create their own small magnetic fields – The movement of protons within the nucleus of the atom creates a small magnetic field – The “electron spin” also produces a tiny magnetic fiel ...
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... change is produced. This back emf causes a current in the opposite direction, recharging the capacitor. The process then repeats itself, giving an oscillating current. A capacitor and inductor, together with an energy source such as a battery can be connected to drive a small speaker to give a sound ...
magnetism - bYTEBoss
magnetism - bYTEBoss

Magnetism Notes
Magnetism Notes

... Like electric charges, there are two types called ______ and _______ because of the way they react to the earth’s magnetic field Unlike electrical charges, can’t have __________ N or S pole; always have both Like electrical charges, opposite poles _____________, like poles ___________ Forces between ...
The Physics of Magnetic Resonance Imaging
The Physics of Magnetic Resonance Imaging

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Changes in Sea Travel

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Lunar Magnetic Anomalies

Magnetism and Electricity
Magnetism and Electricity

... when all the electrons spin in the same direction. When you bring two magnets together they exert a push or pull called a magnetic force. This force results from spinning electric charges of electrons in the magnet. The force can either push magnets apart, or pull them together. Magnetic force is on ...
Ferro-fluid
Ferro-fluid

...  Use a straw to transfer a small drop of ferrofluid into the bottom of a plastic cup  Choose a small magnet to place under or on the side of the cup (I suggest some round fridge magnets, some small medium strength bar magnets, one ree magnet, and a bunch of oblong ‘magnetic sizzlers’)  DO NOT ALL ...
Plate Tectonics - Earth and Environmental Sciences
Plate Tectonics - Earth and Environmental Sciences

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Lecture29

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Threat of Sunshine

Magnetism guide 2
Magnetism guide 2

... _____9) electromagnetic field i) is the process of generating a current by moving a current an electrical conductor relative to a magnetic field. _____10) generator ...
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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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