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... a) Magma rises beneath the continent. b) The continent becomes thinner. c) The continent undergoes faulting and splits. d) All of the above. ...
Earth Systems & Resources
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... Put two graham crackers side by side, and slide one up away from you and the other one down toward you. When plates move past each other like this, things don't exactly go smoothly. In fact, the plates usually get stuck on each other and then give a lurch and move on, sending waves of vibrations thr ...
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... The intertidal zone is the shallowest benthic zone. It is located on the beach between the low-tide and hightide limits. At high tide, the intertidal zone is covered with ocean water. At low tide, the zone is exposed to the air and sun. Therefore, organisms in the intertidal zone are adapted to livi ...
The Risk of Tsunamis - University of North Carolina Wilmington
The Risk of Tsunamis - University of North Carolina Wilmington

... e know more about the features of the moon’s surface than Earth’s. This is because our oceans form an opaque layer that covers more than 70 percent of the earth’s surface. Dr. Nancy Grindlay has spent much of her scientific career working to reveal the mysteries of the seafloor using sonar, submersi ...
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... •Hydrosphere includes the liquid and frozen surface water, groundwater, and water vapor in and around oceans, lakes, and rivers on Earth. •Lithosphere is the land or surface areas on Earth, including the continents, islands, and ocean basins. ...
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... deep-sea drilling into the sediments on the ocean floor  The data on the ages of seafloor sediment confirmed what the seafloor spreading hypothesis predicted  The youngest oceanic crust is at the ridge crest and the oldest oceanic crust is at the continental margins  No sediment older than 180 mi ...
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... from the sun transfers heat to air, land and water at different rates. (Clarification statement: Heat transfer should include the processes of conduction, convection, and radiation.) c. Develop a model demonstrating the interaction between unequal heating and the rotation of the Earth that causes lo ...
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... • A continental slope is the steep gradient that leads to the deep-ocean floor and marks the seaward edge of the continental shelf. • A submarine canyon is the seaward extension of a valley that was cut on the continental shelf ...
ocean basin floor - Plain Local Schools
ocean basin floor - Plain Local Schools

... • A turbidity current is the downslope movement of dense, sediment-laden water created when sand and mud on the continental shelf and slope are dislodged and thrown into suspension. ...
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... washed into the sea. The build up of nutrients combined with warming waters causes the algae to be overfed and grow rapidly to become a thick blanket on the surface of the water. These blankets of algae are so thick they block sunlight from reaching beyond the ocean's surface. They also use up exces ...
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Ocean



An ocean (from Ancient Greek Ὠκεανός, transc. Okeanós, the sea of classical antiquity) is a body of saline water that composes much of a planet's hydrosphere. On Earth, an ocean is one of the major conventional divisions of the World Ocean, which covers almost 71% of its surface. These are, in descending order by area, the Pacific, Atlantic, Indian, Southern, and Arctic Oceans. The word sea is often used interchangeably with ""ocean"" in American English but, strictly speaking, a sea is a body of saline water (generally a division of the world ocean) partly or fully enclosed by land.Saline water covers approximately 72% of the planet's surface (~3.6×108 km2) and is customarily divided into several principal oceans and smaller seas, with the ocean covering approximately 71% of Earth's surface. The ocean contains 97% of Earth's water, and oceanographers have stated that only 5% of the World Ocean has been explored. The total volume is approximately 1.35 billion cubic kilometers (320 million cu mi) with an average depth of nearly 3,700 meters (12,100 ft).As it is the principal component of Earth's hydrosphere, the world ocean is integral to all known life, forms part of the carbon cycle, and influences climate and weather patterns. It is the habitat of 230,000 known species, although much of the oceans depths remain unexplored, and over two million marine species are estimated to exist. The origin of Earth's oceans remains unknown; oceans are thought to have formed in the Hadean period and may have been the impetus for the emergence of life.Extraterrestrial oceans may be composed of water or other elements and compounds. The only confirmed large stable bodies of extraterrestrial surface liquids are the lakes of Titan, although there is evidence for the existence of oceans elsewhere in the Solar System. Early in their geologic histories, Mars and Venus are theorized to have had large water oceans. The Mars ocean hypothesis suggests that nearly a third of the surface of Mars was once covered by water, and a runaway greenhouse effect may have boiled away the global ocean of Venus. Compounds such as salts and ammonia dissolved in water lower its freezing point, so that water might exist in large quantities in extraterrestrial environments as brine or convecting ice. Unconfirmed oceans are speculated beneath the surface of many dwarf planets and natural satellites; notably, the ocean of Europa is estimated to have over twice the water volume of Earth. The Solar System's giant planets are also thought to have liquid atmospheric layers of yet to be confirmed compositions. Oceans may also exist on exoplanets and exomoons, including surface oceans of liquid water within a circumstellar habitable zone. Ocean planets are a hypothetical type of planet with a surface completely covered with liquid.
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