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The influence of water mass mixing on the dissolved Si isotope
The influence of water mass mixing on the dissolved Si isotope

... Fiedler and Talley, 2006). During Austral summer 2009, when the samples for this study were taken, the EUC was located at approximately 0◦ N to 1◦ N at a core depth of 90 m (Czeschel et al., 2011), almost exactly at the location of station 152 (Fig. 1a). Another water mass influencing the EEP is the ...
File - Mariana Gil
File - Mariana Gil

... Subduction Zones and Volcanoes At some convergent boundaries, an oceanic plate collides with a continental plate. Oceanic crust tends to be denser and thinner than continental crust, so the denser oceanic crust gets bent and pulled under, or subducted, beneath the lighter and thicker continental cru ...
LT3ActivityPacket
LT3ActivityPacket

... The theory of plate tectonics states that the crust of the Earth is composed of 7 major plates and numerous smaller plates. These plates move on the top of the hot plastic upper mantle known as the asthenosphere. This theory also says that most of these plates are in motion, creating a variety of ...
Catastrophic Plate Tectonics - Liberty Park, USA Foundation
Catastrophic Plate Tectonics - Liberty Park, USA Foundation

... rate, and greater weakening. This positive feedback associated with thermal weakening can result in runaway provided the criterion mentioned above is met [5]. Experimental studies of the deformational behavior of silicate minerals over the last several decades have revealed the strength of such mate ...
2013 Question of the day
2013 Question of the day

... gasses ...
Oceanography and Atmospheric Sciences: 1959–2009
Oceanography and Atmospheric Sciences: 1959–2009

... and nekton studies off the Oregon coast. It grows to include studies on early life histories of fishes, vertical migration, ocean ecology of juvenile salmonids, albacore catches and participation in national and international cooperative studies. Research in benthic ecology, phytoplankton ecology an ...
Regional phases in continental and oceanic environments
Regional phases in continental and oceanic environments

... up to 3 km. The continental side has a region of thickened crust close to the continent–ocean margin and then grades into a homogeneous section. The thickness of the crust on the continental side has been chosen to be quite thin (24 km with a thickening to 37 km) but still sufficient to display the ...
The Messinian Timeline - UMD | Atmospheric and Oceanic
The Messinian Timeline - UMD | Atmospheric and Oceanic

... The Mediterranean is permanently disconnected from the Indian Ocean and land has reached its modern day configuration (www with miocene land mass). The Messinian stage begins ...
A sea of microbes: the diversity and activity of marine microorganisms
A sea of microbes: the diversity and activity of marine microorganisms

... striking biodiversity are some star players that can be considered ‘keystone organisms’ among the ocean’s microbiota. ...
on circulation, phosphate-phosphorus content, and zooplankton
on circulation, phosphate-phosphorus content, and zooplankton

... and of warm water poleward in the western boundary currents). The gyres are relatively narrow zonal features, and therefore the temperature variation within each gyre is small compared with the differences between adjacent gyres. Each of the gyres also acts in a way to hold a substantial part of the ...
1 Scientific Ocean Drilling of Mid-Ocean Ridge and Ridge
1 Scientific Ocean Drilling of Mid-Ocean Ridge and Ridge

... The global mid-ocean ridge system generates two-thirds of the solid earth surface and produces more than half of the annual volcanic volume erupted on the earth. Active volcanic, hydrothermal, and structural processes mainly transpire within the first few million years of seafloor spreading, on the ...
PLATE BOUNDARY LOCALIZATION: WHAT PROCESSES ACTIVE
PLATE BOUNDARY LOCALIZATION: WHAT PROCESSES ACTIVE

... as fundamental as the origin of plate tectonics. Our planet has adopted a global tectonic regime that appears unique in the solar system [1]. Deformation is localized in narrow deformation zones, some of which do no contribute to removing heat from the interior of the planet [2]. Because of the high ...
Plastic photodegradation in the ocean
Plastic photodegradation in the ocean

... populations suggest there may be two distinct zones of concentrated debris in the Pacific.[27] The patch is not easily visible because it consists of very small pieces, almost invisible to the naked eye,[28] most of its contents are suspended beneath the surface of the ...
Crust
Crust

... z Temperature- hot rock is easier to bend z Pressure- higher pressure more likely to ...
Document
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... A. Gravity B. Electromagnetism C. Nuclear forces ...
What happens when plates diverge - KMS 8th Grade Science
What happens when plates diverge - KMS 8th Grade Science

... and Surface Heat Flow layers. Activate the Age of the Ocean Floor layer by clicking on the check box. ...
Chapter 8 and 18 - Mr. Green's Home Page
Chapter 8 and 18 - Mr. Green's Home Page

...  Because it is less dense  The floating crust pushes down  The crust pushes up.  Balance of forces called isostasy ...
Tectonic Landforms
Tectonic Landforms

... Craton: an old and stable part of the continental lithosphere. Having often survived cycles of merging and rifting of continents, cratons are generally found in the interiors of tectonic plates. They have a thick crust and deep lithospheric roots that extend as much as several hundred km into the m ...
Document
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... 3. Nuclear forces ...
Evidence
Evidence

... magne(c  axis  data,  the  warping  of  the  land  under  loads  (such  as  lakes  and  ice  sheets),  which  show  that  the  solid   mantle’s  rocks  can  bend  and  even  flow.                The  lighter  and  less  de ...
Vertical nitrate fluxes in the Arctic Ocean
Vertical nitrate fluxes in the Arctic Ocean

... Upward mixing of remineralized nutrients is essential for photosynthesis in the upper ocean. Weak vertical mixing, which restricts nutrient supply, and sea ice, which leads to low light levels, conspire to severely inhibit marine primary productivity in the Arctic Ocean. However, little has been kno ...
Plankton biodiversity of the North Atlantic: changing patterns
Plankton biodiversity of the North Atlantic: changing patterns

... CPR Surveys address a global challenge – identifying how and why plankton communities are changing as well as what the consequences of such changes are. This challenge requires a global perspective. Fortunately a number of regional CPR surveys (based in USA, Australia, New Zealand as well as UK) are ...
Attachment 1
Attachment 1

... 2. There’s plastic everywhere in the ocean, like confetti, with some patches/regions in higher concentration than other regions. 3. Ocean currents transport plastics, so the areas of higher concentrations are associated with the center of subtropical ocean gyres, where currents converge. 4. Both fie ...
Case Study 6 Monitoring Phytoplankton Productivity from
Case Study 6 Monitoring Phytoplankton Productivity from

... irradiance. The direct light path through the atmosphere is modified according to the transmittance properties of various compounds, including Rayleigh scattering (Tr ), aerosol extinction (Ta ), as well as ozone (T03 ), water vapor (Tw ), and oxygen (T02 ) absorption. The diffuse component is the s ...
Testimony By Admiral James D. Watkins, U.S. Navy (Retired)
Testimony By Admiral James D. Watkins, U.S. Navy (Retired)

... benefit of all Americans. Just as important, every member of the public should recognize the value of the oceans and coasts, supporting appropriate policies and acting responsibly while minimizing negative environmental impacts. • Ocean–Land–Atmosphere Connections: Ocean policies should be based on ...
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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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