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Chapter 11: The coastal ocean
Chapter 11: The coastal ocean

...  5.f - Ocean habitats are defined by environmental factors. Due to interactions of abiotic factors such as salinity, temperature, oxygen, pH, light, nutrients, pressure, substrate and circulation, ocean life is not evenly distributed temporally or spatially, i.e., it is “patchy”. Some regions of th ...
Chapter 18
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... • vents are colonized by organisms shortly after they are formed • when geological changes inactivate the vent (an estimated 20 years later), these organisms all die • vent inhabitants are thought to produce large numbers of larvae which drift to other vent sites ...
The Oceans
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...  Pure water has a density of 1 g/ml  Seawater ranges from 1.02-1.03 g/ml  This is due to variations in salinity and temperature  Density increases with increasing salinity.  Density decreases with increasing temperature  The salinity can alter the freezing point (-2 C) ...
Chemical and Physical Properties of Seawater Chapter 3, p 44
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Southeast Asia`s Seas:global treasures of biodiversity—in peril
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How are Humans Affecting Ocean Salinity? Transcription
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... When  that  sea  ice  melts  it  leaves  a  pool  of  fresh  water  on  the  surface,  and  the  waves  will  blow  that  fresh   water  out  of  the  Arctic  Ocean  towards  the  Atlantic  Ocean,  and  it  will  begin  to  af ...
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... 13. You are on a vacation in Las Vegas and while you are there, you and your family attend a magic show. For the grand finale, the magician takes two glasses of water and places them on the table. He then takes an egg and drops it in one glass of water and it sinks right to the bottom. He takes the ...
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... Describe a few ways in which fish have adapted to the deep sea. Describe two ways in which animals use bioluminescence? Most bioluminescence in the ocean is blue or blue-green, but a few animals have evolved red bioluminescence. Why might this be useful? What are the three major stages of succession ...
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... flooded with 700 tons of seawater, causing them to sink. As this end of FLIP sinks, the other end, kept afloat with air tanks, rises out of the water. Crew members and scientists, on board while FLIP flips, simply step up onto the walls as the walls become decks. In just 20 minutes, FLIP is in a str ...
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...  Scientists believe the oceans are more than ____________ years old.  Water may have originally been released from ______________________________, or arrived on Earth via ____________________________. ...
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Our Changing Earth - Bal Bharati Public School
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... The forces which act in the interior of the earth, are called endogenic forces. The forces which act on the surface of the earth are called enogenic forces. Q3. What is a volcano ? A volcano is a vent in the earth’s crust through which the molten material erupts. Q4. What are lithospheric plates? Wh ...
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... The forces which act in the interior of the earth, are called endogenic forces. The forces which act on the surface of the earth are called enogenic forces. Q3. What is a volcano ? A volcano is a vent in the earth’s crust through which the molten material erupts. Q4. What are lithospheric plates? Wh ...
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...  The slow rise and fall of the ocean. The upper and lower edges of a beach are determined by the high- and lowtide mark. Tides are connected to the motion of the moon and the spinning of the Earth. The moon exerts a greater force of pull than the sun due to its closer proximity to Earth. ...
Unit 5: Ocean Floor Structure and Plate Tectonics
Unit 5: Ocean Floor Structure and Plate Tectonics

...  Maximum depth is about 200 m,  They are often areas of rich in sea life  They are important economic zone of the nearby countries. Continental Slope –  the drop off at the edge of the continental slope  Both the continental shelf and slope are considered structurally part of the continents, ev ...
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... due to the fresh water entering the ocean.  Fresh water also enters where glaciers and icebergs melt and areas of high precipitation.  High amounts of evaporation increases salinity as well as freezing.  *Density Currents are produced by the differences in salinity. The more dense, saltier water ...
Oceanography
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... around the Mid-Oceanic ridges 2) Absence of great amounts of sediment on the sea floor 3) similar mineral deposits in the Eastern part of South America with the western part of Africa 4) Animal living in India are native to Africa 5) Fossils of Marsupials in North America 6) Fossils of green plants ...
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Sea



A sea is a large body of salt water that is surrounded in whole or in part by land. More broadly, the sea (with the definite article) is the interconnected system of Earth's salty, oceanic waters—considered as one global ocean or as several principal oceanic divisions. The sea moderates Earth's climate and has important roles in the water cycle, carbon cycle, and nitrogen cycle. Although the sea has been travelled and explored since prehistory, the modern scientific study of the sea—oceanography—dates broadly to the British Challenger expedition of the 1870s. The sea is conventionally divided into up to five large oceanic sections—including the IHO's four named oceans (the Atlantic, Pacific, Indian, and Arctic) and the Southern Ocean; smaller, second-order sections, such as the Mediterranean, are known as seas.Owing to the present state of continental drift, the Northern Hemisphere is now fairly equally divided between land and sea (a ratio of about 2:3) but the South is overwhelmingly oceanic (1:4.7). Salinity in the open ocean is generally in a narrow band around 3.5% by mass, although this can vary in more landlocked waters, near the mouths of large rivers, or at great depths. About 85% of the solids in the open sea are sodium chloride. Deep-sea currents are produced by differences in salinity and temperature. Surface currents are formed by the friction of waves produced by the wind and by tides, the changes in local sea level produced by the gravity of the Moon and Sun. The direction of all of these is governed by surface and submarine land masses and by the rotation of the Earth (the Coriolis effect).Former changes in the sea levels have left continental shelves, shallow areas in the sea close to land. These nutrient-rich waters teem with life, which provide humans with substantial supplies of food—mainly fish, but also shellfish, mammals, and seaweed—which are both harvested in the wild and farmed. The most diverse areas surround great tropical coral reefs. Whaling in the deep sea was once common but whales' dwindling numbers prompted international conservation efforts and finally a moratorium on most commercial hunting. Oceanography has established that not all life is restricted to the sunlit surface waters: even under enormous depths and pressures, nutrients streaming from hydrothermal vents support their own unique ecosystem. Life may have started there and aquatic microbial mats are generally credited with the oxygenation of Earth's atmosphere; both plants and animals first evolved in the sea.The sea is an essential aspect of human trade, travel, mineral extraction, and power generation. This has also made it essential to warfare and left major cities exposed to earthquakes and volcanoes from nearby faults; powerful tsunami waves; and hurricanes, typhoons, and cyclones produced in the tropics. This importance and duality has affected human culture, from early sea gods to the epic poetry of Homer to the changes induced by the Columbian Exchange, from Viking funerals to Basho's haikus to hyperrealist marine art, and inspiring music ranging from the shanties in The Complaynt of Scotland to Rimsky-Korsakov's ""The Sea and Sinbad's Ship"" to A-mei's ""Listen to the Sea"". It is the scene of leisure activities including swimming, diving, surfing, and sailing. However, population growth, industrialization, and intensive farming have all contributed to present-day marine pollution. Atmospheric carbon dioxide is being absorbed in increasing amounts, lowering its pH in a process known as ocean acidification. The shared nature of the sea has made overfishing an increasing problem.
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