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  2. Reed Tablemount - Wikipedia

    en.wikipedia.org/wiki/Reed_Tablemount

    Reed Tablemount (also referred to as Reed Bank, Recto Bank and several other names) is a large tablemount or guyot in the South China Sea north-east of Dangerous Ground and north-east of the Spratly Islands.

  3. Diving plane - Wikipedia

    en.wikipedia.org/wiki/Diving_plane

    Diving planes, also known as hydroplanes, are control surfaces found on a submarine which allow the vessel to pitch its bow and stern up or down to assist in the process of submerging or surfacing the boat, as well as controlling depth when submerged.

  4. Boss (engineering) - Wikipedia

    en.wikipedia.org/wiki/Boss_(engineering)

    The word 'boss' is also often used to describe the end of a shaft on a boat to which a propeller might attach. A boss may also refer to a mounting feature that will receive a screw or thread-forming screw. In computer-aided design applications, a boss is a feature used to describe a type of extrusion.

  5. Type 093 submarine - Wikipedia

    en.wikipedia.org/wiki/Type_093_submarine

    These boats have a streamlined sail lengthened by 2.5 meters to reach the Type 093's design speed of 30 knots, a stern towed array sonar deployment tube, and a hump behind the sail; the hump is likely for the towed array handling gear and is not a vertical launching system (VLS). The hump was box-like on the first boat, tall and streamlined on ...

  6. Long-tail boat - Wikipedia

    en.wikipedia.org/wiki/Long-tail_boat

    Long-tail boats in Poda island, Krabi, Thailand. The long-tail boat, (Thai: เรือหางยาว, RTGS: ruea hang yao, pronounced [rɯ̄a̯ hǎːŋ jāːw]) is a type of watercraft native to Southeast Asia, which uses a common automotive engine as a readily available and maintainable powerplant.

  7. Seamount - Wikipedia

    en.wikipedia.org/wiki/Seamount

    t. e. A seamount is a large submarine landform that rises from the ocean floor without reaching the water surface ( sea level ), and thus is not an island, islet, or cliff -rock. Seamounts are typically formed from extinct volcanoes that rise abruptly and are usually found rising from the seafloor to 1,000–4,000 m (3,300–13,100 ft) in height.

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