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Background Knowledge – Layers of the Earth 1. List the layers of the
Background Knowledge – Layers of the Earth 1. List the layers of the

... 3. True or False: Changes in the mantle material’s heat and density is causes convection currents. 4. How does a lava lamp represent convection currents in the mantle? The light bulb heats the material unevenly just like the outer core heats the mantle unevenly. As the temperature rises, the volume ...
scientific synthesis on the impacts of ocean fertilization on
scientific synthesis on the impacts of ocean fertilization on

... water to the surface for cooling or energy-generating purposes (Ocean Thermal Energy Conversion – OTEC). The latter utilizes the significant temperature difference between shallow and deep waters to produce renewable energy. Furthermore, the definition of ocean fertilization in resolution LC-LP.1 (2 ...
Drilling at sea: Hydrocarbon Exploration
Drilling at sea: Hydrocarbon Exploration

... take place without extensive uplift; in such cases it may be the convective processes in the underlying asthenosphere which are causing the extension. To rift a continent apart it needs the rifts associated with various possible thermal domes to link together. Morgan (1981, 1983) has suggested that ...
LLVSPs vs. LVAs - Do plumes exist?
LLVSPs vs. LVAs - Do plumes exist?

... lithospheric stress field associated with upper mantle downwellings but have much poorer correlations with stresses inferred from upwellings and from lower mantle effects. For a search radius of 100 km, only 3 minor volcanic provinces are in regions of substantial inferred convergence rather than ex ...
Key Points on the Earth`s Layers - Greenville Public School District
Key Points on the Earth`s Layers - Greenville Public School District

... A. It is sometimes called “plastic” which means it can be bent and shaped while hot and will hold its shape when it hardens. 3. The asthenosphere is very hot. It has a much higher temperature than the lithosphere. 4. The asthenosphere is a liquid and convection currents form in it just like they do ...
Expedition #8 - SJSU Geology Online Classes
Expedition #8 - SJSU Geology Online Classes

... pattern) - which supported Hess' seafloor spreading hypothesis -- it therefore appeared that the oceanic lithosphere should be older with greater distance from the center of the mid-ocean ridge where it first formed By matching the reversal history to the magnetic patterns under the sea, and assumin ...
Arthur C. Clarke and the Limitations of the Ocean as a Frontier
Arthur C. Clarke and the Limitations of the Ocean as a Frontier

... In 1960, the bathyscaphe Trieste reached the bottom of the Marianas Trench at the Challenger Deep, the deepest point of the ocean. The first human to orbit the earth did not do so until two years later. Yet for three decades after the Trieste’s epoch achievement, no further efforts were launched to ...
Changes in seismic anisotropy shed light on the nature of the
Changes in seismic anisotropy shed light on the nature of the

... layer (layer 2) by a better alignment with the APM. Layer 1 is also characterized by high seismic velocities away from ocean ridges [4-5% with respect to our reference model (16)], and its thickness increases with crustal age, similar to past surface wave studies (13, 17-19). Furthermore, layer 1 is ...
2006 Thomson-Brooks Cole Chapter 3 Geology of the Oceans
2006 Thomson-Brooks Cole Chapter 3 Geology of the Oceans

... • The world ocean has four main basins: the Atlantic, Pacific, Indian, and Arctic. • Life first evolved in the ocean. • The earth’s crust is composed of moving plates. • New seafloor is produced at ocean ridges and old seafloor is removed at ocean trenches. © 2006 Thomson-Brooks Cole ...
Intergovernmental Oceanographic Commission (IOC)
Intergovernmental Oceanographic Commission (IOC)

... Main Line of Action 2: To further develop, within the GOOS and GCOS, the monitoring and forecasting capabilities needed for the management and sustainable development of the open and coastal ocean DESCRIPTION: The IOC, leading a partnership with WMO, UNEP and ICSU, began implementing GOOS in 1998. ...
2. Products - Dragoness - Nansen Environmental and Remote
2. Products - Dragoness - Nansen Environmental and Remote

... NMEFC has developed a high resolution typhoon storm surge numerical model with nesting techniques. The main improvement lies in model horizontal resolution and the grid nesting techniques which avoid the boundary extraneous wave and enhance the model stability. The model has a 3.7 km resolution and ...
Lecture 9b: Upper Mantle Structure and Composition
Lecture 9b: Upper Mantle Structure and Composition

... knowledge of layering is recent (late 1800s); prior to that, only knew interior must be hot (volcanoes) ...
Water column methanotrophy controlled by a rapid oceanographic
Water column methanotrophy controlled by a rapid oceanographic

... Together with the reduction in MOx activity and community size, we observed a strong spatiotemporal change in the distribution of water mass properties. During the August 18/19 survey, bottom waters consisted of cold AW with an admixture of AIW and ArW (Fig. 1d,e), which we subsequently refer to as ...
Arctic observation initiatives of Korea Polar Research Institute for
Arctic observation initiatives of Korea Polar Research Institute for

... change. This region is characterized by the local complexity in topography and intersection of Pacificorigin waters from the south and Atlantic waters from the west. The Pacific water inflow through the Bering Strait is a key conveyor for heat, salt, nutrients, and biological material to the upper l ...
Changes in Marine Prokaryote Composition with Season and Depth
Changes in Marine Prokaryote Composition with Season and Depth

... 2008), contributing a single annual major input of organic carbon and energy to the microbial communities residing in dark mesopelagic and deep waters. This subsurface realm dominates the global ocean biome and whereas the Arctic Ocean is the shallowest of the five major oceanic divisions, still its ...
Floral Response of Coccolithophores to Progressive
Floral Response of Coccolithophores to Progressive

... (upwelling). Moreover, a strong coastal upwelling off the coast of Ecuador and Peru supplies nutrient-rich, cold, deep water to the surface of the Eastern Pacific (Brown et al., 1989). Therefore, the SEC is a suitable current for studying the floral response to hydrographic changes. By kindly provid ...
Hydrothermal circulation in oceanic crust
Hydrothermal circulation in oceanic crust

... • What is the significance of the shaded area in the figure? ...
Estimation of glacial meltwater discharge into Svalbard coastal waters*
Estimation of glacial meltwater discharge into Svalbard coastal waters*

... surface waters of the innermost fjord basins and to 34.4 PSU in the deeper layers and outer fjord waters corresponded to a freshwater fraction of 10 to 0.6%. For the fjords in question, the instantaneous volume of freshwater in summer was estimated at 0.79 km3 in Horsund and 0.33 km3 in Kongsfjord. ...


... and we and our growing group of CORK collaborators have gone on to deploy similar instrumentation in a total of 11 sites (see map opposite) in three representative types of seafloor hydrological environments: spreading centers, where new seafloor is spreading outward from mid-ocean ridges (ODP Holes ...
EENS 2120 Petrology Prof. Stephen A. Nelson Igneous Rocks of the
EENS 2120 Petrology Prof. Stephen A. Nelson Igneous Rocks of the

... At 30 kb pressure the first liquids to form from melting of peridotite would be those farthest away from the peridotite. Note that these liquids would be highly silica undersaturated. With increasing degrees of melting the liquid composition would change along a path toward the Ol - Plag join and ev ...
The dynamics of the marine nitrogen cycle across the last deglaciation
The dynamics of the marine nitrogen cycle across the last deglaciation

... benthic denitrification [Codispoti, 1989] (Figure 1). If the N:P ratio of the nutrient pool is lowered, the rate of export production will decrease due to an even stronger limitation by NO–3 , causing a drop in export production, a lower oxygen demand from organic matter remineralization, and thus hi ...
Sediments...Chapter 4
Sediments...Chapter 4

... Microscopic tests sink slowly from surface ocean to sea floor (10(10-50 years) „ Tests could be moved horizontally „ Most biogenous tests clump together in fecal pellets ...
The Engine that Drives the Earth
The Engine that Drives the Earth

... Earth’s mantle is the solid, rocky interior of our planet that extends from the base of the crust all the way down to Earth’s core, about 2,900 kilometers (1,800 miles) below the surface. Although they are solid, the rocks in Earth’s mantle can deform and flow by viscous creep over long time periods ...
Protection and conservation of the living resources of the Area
Protection and conservation of the living resources of the Area

... the Mid Atlantic Ridge, at 3,650 meters depth, measures more than 48 m in high and 182 m in diameter. Some deposits can contain approximately 100 million metric tons, competing with giant ore bodies on land, although most marine deposits are much smaller. Sometimes the structures fall, but chimneys ...
Isotopic Tracers of the Marine Nitrogen Cycle: Present and Past
Isotopic Tracers of the Marine Nitrogen Cycle: Present and Past

... Trichodesmium lacks heterocysts and in fact couples photosynthetic energy production to N2 fixation. How O2 inhibition is overcome is not well understood. The high requirement for Fe has further suggested an interaction between Fe and N biogeochemistry [6]. Since Fe is chiefly supplied by eolian dust ...
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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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