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  2. Polar fleece - Wikipedia

    en.wikipedia.org/wiki/Polar_fleece

    Polar fleece originated in Massachusetts in 1979 when Malden Mills and Patagonia developed Synchilla (synthetic chinchilla). [3] It was a new, light, strong pile fabric meant to mimic, and in some ways surpass, wool.

  3. Millard Sheets - Wikipedia

    en.wikipedia.org/wiki/Millard_Sheets

    Millard Sheets was born June 24, 1907, and grew up in the Pomona Valley, east of Los Angeles. [2] [3] He is the son of John Sheets. [4]He attended the Chouinard Art Institute and studied with painters Frank Tolles Chamberlin and Clarence Hinkle. [5]

  4. Nickel - Wikipedia

    en.wikipedia.org/wiki/Nickel

    Nickel and its alloys are often used as catalysts for hydrogenation reactions. Raney nickel, a finely divided nickel-aluminium alloy, is one common form, though related catalysts are also used, including Raney-type catalysts. [94] Nickel is naturally magnetostrictive: in the presence of a magnetic field, the material undergoes a small change in ...

  5. Graded bedding - Wikipedia

    en.wikipedia.org/wiki/Graded_bedding

    In geology, a graded bed is a bed characterized by a systematic change in grain or clast size from bottom to top of the bed. Most commonly this takes the form of normal grading, with coarser sediments at the base, which grade upward into progressively finer ones. Such a bed is also described as fining upward. [1]

  6. Nickel sulfide - Wikipedia

    en.wikipedia.org/wiki/Nickel_sulfide

    Nickel sulfide is any inorganic compound with the formula NiS x. These compounds range in color from bronze (Ni 3 S 2) to black (NiS 2). The nickel sulfide with simplest stoichiometry is NiS, also known as the mineral millerite. From the economic perspective, Ni 9 S 8, the mineral pentlandite, is the chief source of mined

  7. Ice sheet - Wikipedia

    en.wikipedia.org/wiki/Ice_sheet

    Greenland ice sheet as seen from space. An ice sheet is a body of ice which covers a land area of continental size - meaning that it exceeds 50,000 km 2. [4] The currently existing two ice sheets in Greenland and Antarctica have a much greater area than this minimum definition, measuring at 1.7 million km 2 and 14 million km 2, respectively.

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