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  2. Floating shelf - Wikipedia

    en.wikipedia.org/wiki/Floating_shelf

    A floating shelf can be supported on hidden rods or bars that have been attached to studs. A thick floating shelf may be made of a hollow-core shelf glued to a cleat. [7] A floating shelf may have two or more channels open from the back towards, but without reaching, the front, into which slide fasteners attached to the wall, typically held in place by screws inserted through the bottom of the ...

  3. List of companies in Houston - Wikipedia

    en.wikipedia.org/wiki/List_of_companies_in_Houston

    Fortune 500 companies based in Houston [1]: Rank Company name 12: ExxonMobil: 48: Phillips 66: 60: Sysco: 105: Enterprise Products Partners: 106: Hewlett Packard Enterprise: 127: Plains GP Holdings

  4. Derrick - Wikipedia

    en.wikipedia.org/wiki/Derrick

    The Stülcken derrick is used for heavy cargo. It stems from the German shipyard HC Stülcken & Sohn, later taken over by neighboring yard Blohm & Voss. This derrick can handle up to 300 tonnes. The Stülcken can be made ready in few minutes (faster than a traditional heavy derrick), does not require much space, and is operated by four winches.

  5. Crane vessel - Wikipedia

    en.wikipedia.org/wiki/Crane_vessel

    A crane vessel, crane ship, crane barge, or floating crane is a ship with a crane specialized in lifting heavy loads, typically exceeding 1,500 t (1,476 long tons; 1,653 short tons) for modern ships. The largest crane vessels are used for offshore construction .

  6. Stafford, Texas - Wikipedia

    en.wikipedia.org/wiki/Stafford,_Texas

    Fort Bend County operates the 5-acre (20,000 m 2) Stafford Community Center in Fifth Street, an unincorporated area near Stafford. [22] In 2014 the Sugar Land Youth Cricket Club, a children's cricket club, was established. In 2016 it played its home games at Everest Academy in Stafford. [23]

  7. Continental shelf - Wikipedia

    en.wikipedia.org/wiki/Continental_shelf

    The shelf usually ends at a point of increasing slope [3] (called the shelf break). The sea floor below the break is the continental slope. [4] Below the slope is the continental rise, which finally merges into the deep ocean floor, the abyssal plain. [5] The continental shelf and the slope are part of the continental margin. [6]

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