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  2. Lodestone - Wikipedia

    en.wikipedia.org/wiki/Lodestone

    Ordinary magnetite is attracted to a magnetic field as iron and steel are, but does not tend to become magnetized itself; it has too low a magnetic coercivity. (resistance to magnetization or demagnetization) [ 9 ] Microscopic examination of lodestones has found them to be made of magnetite (Fe 3 O 4 ) with inclusions of maghemite (cubic Fe 2 O ...

  3. Magnet - Wikipedia

    en.wikipedia.org/wiki/Magnet

    A magnet's magnetic moment (also called magnetic dipole moment and usually denoted μ) is a vector that characterizes the magnet's overall magnetic properties. For a bar magnet, the direction of the magnetic moment points from the magnet's south pole to its north pole, [ 15 ] and the magnitude relates to how strong and how far apart these poles ...

  4. Category:Types of magnets - Wikipedia

    en.wikipedia.org/wiki/Category:Types_of_magnets

    Pages in category "Types of magnets" The following 31 pages are in this category, out of 31 total. This list may not reflect recent changes. B. Bitter electromagnet; D.

  5. Steer clear from the TikTok magnet trend that's landed kids ...

    www.aol.com/lifestyle/steer-clear-tiktok-magnet...

    In the U.K., at least three children have been hospitalized after swallowing magnets for the TikTok trend. Faye Elizabeth's 13-year-old daughter swallowed 15 magnetic beads and required major ...

  6. Nanomagnet - Wikipedia

    en.wikipedia.org/wiki/Nanomagnet

    Canonical examples of nanomagnets are grains [1] [2] of ferromagnetic metals (iron, cobalt, and nickel) and single-molecule magnets. [3] The vast majority of nanomagnets feature transition metal ( titanium , vanadium , chromium , manganese , iron, cobalt or nickel) or rare earth ( Gadolinium , Europium , Erbium ) magnetic atoms.

  7. Natural remanent magnetization - Wikipedia

    en.wikipedia.org/wiki/Natural_remanent_magnetization

    Natural remanent magnetization is the permanent magnetism of a rock or sediment. This preserves a record of the Earth's magnetic field at the time the mineral was laid down as sediment or crystallized in magma and also the tectonic movement of the rock over millions of years from its original position.

  8. Neodymium magnet - Wikipedia

    en.wikipedia.org/wiki/Neodymium_magnet

    A neodymium magnet (also known as NdFeB, NIB or Neo magnet) is a permanent magnet made from an alloy of neodymium, iron, and boron to form the Nd 2 Fe 14 B tetragonal crystalline structure. [1] They are the most widely used type of rare-earth magnet .

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