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  2. AOL Mail Help - AOL Help

    help.aol.com/products/new-aol-mail

    You've Got Mail!® Millions of people around the world use AOL Mail, and there are times you'll have questions about using it or want to learn more about its features. That's why AOL Mail Help is here with articles, FAQs, tutorials, our AOL virtual chat assistant and live agent support options to get your questions answered.

  3. Thaddeus S. C. Lowe - Wikipedia

    en.wikipedia.org/wiki/Thaddeus_S._C._Lowe

    Thaddeus Sobieski Constantine Lowe (August 20, 1832 – January 16, 1913), also known as Professor T. S. C. Lowe, was an American Civil War aeronaut, scientist and inventor, mostly self-educated in the fields of chemistry, meteorology, and aeronautics, and the father of military aerial reconnaissance in the United States. [1]

  4. Schengen Area - Wikipedia

    en.wikipedia.org/wiki/Schengen_Area

    The Schengen Area (English: / ˈ ʃ ɛ ŋ ən / SHENG-ən, Luxembourgish: [ˈʃæŋən] ⓘ) is an area encompassing 29 European countries that have officially abolished border controls at their mutual borders.

  5. University of Southern Maine - Wikipedia

    en.wikipedia.org/wiki/University_of_Southern_Maine

    The University of Southern Maine (USM) is a public university with campuses in Portland, Gorham and Lewiston in the U.S. state of Maine. It is the southernmost of the University of Maine System . It was founded as two separate state universities, Gorham Normal School and Portland University.

  6. Hell's Kitchen, Manhattan - Wikipedia

    en.wikipedia.org/wiki/Hell's_Kitchen,_Manhattan

    Hell's Kitchen, formerly also known as Clinton, is a neighborhood on the West Side of Midtown Manhattan in New York City, United States.It is considered to be bordered by 34th Street (or 41st Street) to the south, 59th Street to the north, Eighth Avenue to the east, and the Hudson River to the west.

  7. Quartzite - Wikipedia

    en.wikipedia.org/wiki/Quartzite

    Quartzite can have a grainy, glassy, sandpaper-like surface. Quartzite is a hard, non-foliated metamorphic rock which was originally pure quartz sandstone. [1] [2] Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts.

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