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Seafloor Spreading
Seafloor Spreading

... 1. Hot, buoyant magma from the mantle rises up a mid-ocean ridge. 2. The magma erupts as lava and forms new seafloor. Magnetic polarity is set when rock cools. 3. The newly-formed rock is pushed away from the ridge axis as more lava erupts. 4. If the oceanic crust reaches a deep sea trench, it sinks ...
Speed installation of system to monitor vital signs of global ocean
Speed installation of system to monitor vital signs of global ocean

... ocean surface has dropped from 8.2 to 8.1 units, "rendering the oceans more acidic than they have been for 20 million years," with expectations of continuing acidification due to high concentrations of carbon dioxide in the atmosphere. ...
Crust
Crust

... 5. How does density change as you move towards the center of the Earth? • As you move from the crust towards the center of the Earth, density increases. ...
Climate effects on North Sea zooplankton
Climate effects on North Sea zooplankton

... community changes. For example, during the last 40 years there has been a northerly movement of warmer water plankton by 10° latitude in the north-east Atlantic and a similar retreat of colder water plankton to the north. This geographical movement is much more pronounced than any documented terrest ...
English
English

... Rasdhoo Island and Madivaru Island is known throughout the world as a famous diving site to spot Hammerhead Sharks. The average depth of the channel is estimated to be 400m. Hammerhead sharks can be seen in abundance throughout the year in depths of 25- 60 meters. Since the Atoll is an isolated Atol ...
Patterns and Processes in Human Coastal Development
Patterns and Processes in Human Coastal Development

... • Federal offshore lands are source of ...
deep-ocean basin
deep-ocean basin

... direction of plate motions, they break into segments that are bounded by faults. ...
U.S. Commission on Ocean Policy Northeast Regional Meeting 23 July, 2002
U.S. Commission on Ocean Policy Northeast Regional Meeting 23 July, 2002

... The character of the coastal zone and environmental priorities of state governments vary regionally from the Gulfs of Mexico and Alaska to the NE seaboard and the Hawaiian Islands. Changes in the marine ecosystems that define the coastal zone in these regions, from changes in sea state and coastal e ...
Script - FOG - City College of San Francisco
Script - FOG - City College of San Francisco

... The ARCHAEA KINGDOM is superficially similar to bacteria, but with genes capable of producing different kinds of enzymes. They are also single-celled prokaryotes. They can be heterotrophs and autotrophs. They include most organisms known as extremophiles, as they often live in environments with extr ...
The Ocean
The Ocean

... When did the expedition take place? – What kinds of instruments were available at that time?Ocean basins are at a much lower level than the land, formed mainly of dense basaltic rock, whereas continental rocks are mostly granite and granite gneiss. The depth can vary greatly from one location to ano ...
South Pacific Ocean - Alvarado High School
South Pacific Ocean - Alvarado High School

... greater in the North Pacific, the cumulative amount of cold deep water is less. In other words, the average temperature of waters in the North Pacific is warmer because there are more coastal areas. Also, the deep currents coming up from Antarctica into the South Pacific bring intensely cold waters ...
274 - CIESM
274 - CIESM

... morphological state indicating their recent origin from shallow waters as diatom cell viability can range from 6.8 – 24 days [1]. Such diatom cells would eventually die due to the lack of light necessary for photosynthetic processes, but their carbon load was transported to depths. The results from ...
Greenhouse Earth
Greenhouse Earth

... water near warmer poles • Configuration of continents could have caused this – Large seaway near northern branch of the Hadley Cell’s descending air – Dry conditions and evaporation • Warm salty bottom water could have - Contributed to poleward heat flux to warm the poles - Reduced the large tempera ...
Deep seabed mining - Pacific Ecologist
Deep seabed mining - Pacific Ecologist

... concern is the rapid decline in the health of coral reefs around the world, mainly due to global warming.6 Back in 1971, ocean visionary Jacques-Yves Cousteau wrote of the Red Sea, comparing it with what he and his team had found in 1953. He noted the damage to coral: “If such destruction can take p ...
mauna kea - National Geographic
mauna kea - National Geographic

... Hawaii is the youngest and largest of a chain of islands making up the Hawaiian archipelago. The archipelago is composed of eight main islands and several smaller islands and atolls, which were once active volcanoes that have since sunk and eroded over millions of years. The Hawaiian archipelago for ...
1 Part 2. Oceanic Carbon and Nutrient Cycling Lecture Outline 1
1 Part 2. Oceanic Carbon and Nutrient Cycling Lecture Outline 1

Citizens Guide to the Territorial Sea Plan
Citizens Guide to the Territorial Sea Plan

... of existing ocean uses and ecological resources to identify and designate specific areas within the territorial sea that may be appropriate for renewable energy development. This process will be aided by the use of digital data that can be used in a computer to create map overlays and analysis of di ...
Humanities 5 Blue Humanities John R. Gillis Although fully half of
Humanities 5 Blue Humanities John R. Gillis Although fully half of

PDF: Printable Press Release
PDF: Printable Press Release

... Cope and Kate Ruck; and William & Mary undergraduate Domi Paxton. Gleiber is studying the long-term changes in the abundance and distribution of copepods, small crustaceans the size of a rice grain that form the base of the Antarctic food web and play an important role in the cycling of carbon and o ...
GEOL 1e Lecture Outlines
GEOL 1e Lecture Outlines

... features in this profile are greatly exaggerated, because the vertical and horizontal scales differ. ...
Powerpoint
Powerpoint

... Amount of sunlight Varies daily and seasonally Sunlight strong enough to support photosynthesis occurs only to a depth of 100 meters (euphotic zone) ...
Ocean Water and Ocean Life Earth Science, 13e Chapter 14
Ocean Water and Ocean Life Earth Science, 13e Chapter 14

... • Pelagic zone – open ocean of any depth • Benthic zone – includes any sea-bottom surface • Abyssal zone – a subdivision of the benthic zone • Deep • Extremely high water pressure • Low temperatures © 2012 Pearson Education, Inc. ...
Beyond_the_Beach
Beyond_the_Beach

... hot basalt, thermal expansion creates elevation moves away from ridge axis in both directions Abyssal basins water depth – 4000-6000 m (only trenches are deeper) abyssal hills, include rough relief from volcanic formation abyssal plains, smooth surface due to burial by sediment Continental margins c ...
Document
Document

... ppt, actual salinity varies from place to place. -The lowest salinity often occurs where large rivers empty into the oceans, creating areas of water called estuaries. ...
School of Marine Science/Virginia Institute of Marine Science
School of Marine Science/Virginia Institute of Marine Science

... Students who are interested in pursuing marine science as a profession should consult with their academic advisor or the Dean of Graduate Studies, School of Marine Science, early in their college careers to identify an academic program that will prepare them for graduate study in marine science. Stu ...
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Marine habitats



The marine environment supplies many kinds of habitats that support marine life. Marine life depends in some way on the saltwater that is in the sea (the term marine comes from the Latin mare, meaning sea or ocean). A habitat is an ecological or environmental area inhabited by one or more living species.Marine habitats can be divided into coastal and open ocean habitats. Coastal habitats are found in the area that extends from as far as the tide comes in on the shoreline out to the edge of the continental shelf. Most marine life is found in coastal habitats, even though the shelf area occupies only seven percent of the total ocean area. Open ocean habitats are found in the deep ocean beyond the edge of the continental shelf.Alternatively, marine habitats can be divided into pelagic and demersal habitats. Pelagic habitats are found near the surface or in the open water column, away from the bottom of the ocean. Demersal habitats are near or on the bottom of the ocean. An organism living in a pelagic habitat is said to be a pelagic organism, as in pelagic fish. Similarly, an organism living in a demersal habitat is said to be a demersal organism, as in demersal fish. Pelagic habitats are intrinsically shifting and ephemeral, depending on what ocean currents are doing.Marine habitats can be modified by their inhabitants. Some marine organisms, like corals, kelp, mangroves and seagrasses, are ecosystem engineers which reshape the marine environment to the point where they create further habitat for other organisms.
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