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Oceanography
WCHS Oceanography Chapter 14
| Word | Definition |
|---|---|
| Oceanography | Is a science that draws on the methods and knowledge of geology, chemistry, physics, and biology to study all aspects of the world ocean. |
| Bathymetry | is the measurement of ocean depths and the charting of the shape or topography of the ocean floor. |
| Sonor | Is an acronym for Sound Navigation and Ranging. An electronic depth-sounding mechanism; Sonor calculates ocean depth by recording the time it takes for an energy pulse to reach the ocean floor and return. |
| Submersible | Is a small underwater craft used for deep-sean research. They a;re used to collect data about areas of the ocean that were previously unreachable by humans. |
| Pacific Ocean | Largest ocean, also the largest single geographic feature on earth. Covers more thatn half of the ocean surface area of earth. Average depth is 3940 meters. |
| Atlantic Ocean | Half the size of the Pacific Ocean. |
| Indian Ocean | Slightly smaller thatn Atlantic Ocean, but same average depth. It is entirely in southern hemisphere. |
| Arctic Ocean | About 7 percent of the size of the Pacific Ocean. Is al little more than one-quarter as deep as the rest of the oceans. |
| Continental margin | the zone of transition between a continent and the adjacent ocean basin floor. |
| Continental shelf | the gently sloping submerged surface extending from the shoreline. It is almost nonexistent along some coastlines. |
| submarine canyon | a seaward extension of a valley that was cut on the continental shelf during a time when sea level was lower; a canyon carved into the outer continental shelp, slope and rise by turbidity currents |
| Turbidity current | a downslpoe movement of dense, sediment-laden water created when sand and mud on the continental shelf and slpoe are dislodged and thrown into suspension |
| Continental rise | the gently sloping surface at eht base of the continental slope. |
| ocean basin floor | area of the deep-ocean floor between the coninental margin and the oceanic ridge. |
| abyssal plains | very level area of the deep-ocean floor, usually lying at the foot of the continental rise. |
| Seamounts | an isolated volcainc peak that rises a t least 1000 meters above the deep-ocean floor. |
| Mid-ocean ridge | Or oceanic ridge; a continuous elevated zone on the floor of all the major ocean basins and varying in width from 1000 to 4000 kilometers; the rifts at the crest of ridges represent divergent plate boundaries |
| seafloor spreading | the process by which plate tectonics produces new oceanic lithosphere at ocean ridges. |
| Continental Slope | the steep gradient that leads to the deep-ocean floor and marks the seaward edge of the continental shelf. |
| Terrigenous sediment | seafloor sediment derived from eroded rocks on land |
| biogenous sediment | seafloor sediment of biological origin, such as shells and skeletons of marine life |
| calcareous ooze | thick, common biogenous sediment produce by dissolving calcium carbonate shells |
| siliceous ooze | biogenous sediment composed of the silica-based shells of single-celled animals and algae |
| hydrogenous sediment | seafloor sediment consisting of minerals that crystalize from seawater; an important exampe is manganese nodules |
| gas hydrates | are compact chemical structures made of water and natural gas, most common is methane. |
| manganese nodule | are hard lumps of manganese and other metals that precipitate around a smaller object. they contain high concentration of manganese, iron, and smaller concentrations of compper, nickel, and cobalt. |