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The seabed (also known as the seafloor, sea floor, ocean floor, and ocean bottom) is the bottom of the ocean. All floors of the ocean are known as 'seabeds'. The structure of the seabed of the global ocean is governed by plate tectonics. Most of the ocean is very deep, where the seabed is known as the abyssal plain. Seafloor spreading creates ...
The machine was designed to be fixed to a sounding lead and line. It featured a rotor which turned a dial as the lead sank to the sea floor. On striking the sea floor, the rotor would lock. Massey's sounding machine could then be hauled in and the depth could be read off the dials in fathoms.
The motels are very stylized, with Vegas-like neon signs, plastic palm trees, and fantastic architecture. [4] Construction of condominia in the area has resulted in the demolition of many motels, but the Wildwood Doo Wop Preservation League has taken action to help save and restore the remaining historic buildings. [5]
Playland (also known as Playland-at-the-Beach and Whitney's Playland, beginning in 1928 [1] – some say 1926 [2]) was a 10-acre (40,000-square-meter) seaside amusement park located next to Ocean Beach, in the Richmond District at the western edge of San Francisco, California, along Great Highway, bounded by Balboa and Fulton streets. [1]
Globally, there are over 50 major ocean trenches covering an area of 1.9 million km 2 or about 0.5% of the oceans. [4] Trenches are geomorphologically distinct from troughs. Troughs are elongated depressions of the sea floor with steep sides and flat bottoms, while trenches are characterized by a V-shaped profile. [4]
Siliceous ooze is a type of biogenic pelagic sediment located on the deep ocean floor. Siliceous oozes are the least common of the deep sea sediments, and make up approximately 15% of the ocean floor. [1] Oozes are defined as sediments which contain at least 30% skeletal remains of pelagic microorganisms. [2]
A Hidden Universe on the Ocean Floor? oxygen - Getty Images "Hearst Magazines and Yahoo may earn commission or revenue on some items through these links." A new neutrino sensor array, ARCA, lines ...
Mid-ocean ridges exhibit active volcanism and seismicity. [3] The oceanic crust is in a constant state of 'renewal' at the mid-ocean ridges by the processes of seafloor spreading and plate tectonics. New magma steadily emerges onto the ocean floor and intrudes into the existing ocean crust at and near rifts along the ridge axes. The rocks ...
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