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Simulating the mid-Pliocene climate with the MIROC general
Simulating the mid-Pliocene climate with the MIROC general

... warming of the AOGCM sea surface in parts of the northern North Atlantic Ocean and Nordic Seas is less than that suggested by proxy data. An investigation of the model-data discrepancies and further model intercomparison studies can lead to a better understanding of the mid-Pliocene climate and of i ...
The theory of Plate Tectonics Plate Boundaries
The theory of Plate Tectonics Plate Boundaries

... ● Mid-oceanic ridges are mountain ranges at divergent ...
06_chapter 1
06_chapter 1

... it has revolutionized our understanding of the dynamic planet Earth, upon which we live. In geology the word "plate" refers to thin and rigid slab of rocks, whereas "tectonics" term comes from the Greek root "to build". Plate tectonic theory suggests that outer most layer of the Earth is fragmented ...
Station - Scioly.org
Station - Scioly.org

... D. Heat from within the mantle creates convection currents and causes one plate to move below another at point A. E. Pressure from the volcano is pushing plate A down into the mantle as an equal and opposite force. 3. *The map below shows a group of islands in the Pacific Ocean. The islands have man ...
Understanding Ocean Acidification Prior Knowledge Summary
Understanding Ocean Acidification Prior Knowledge Summary

... dioxide from the atmosphere. Increasing carbon dioxide levels in the atmosphere is causing ocean water to become more acidic, threatening the survival of shell-building marine species and the entire food web of which they are a part. ...
Plate Tectonics - John Bowne High School
Plate Tectonics - John Bowne High School

... in the early 1960s revealed a pattern of magnetic reversals over geologic time. – A magnetic reversal is a change in Earth’s magnetic field.  A magnetic field that is the same as the present has normal polarity.  A magnetic field that is opposite to the present has reversed polarity. ...
PDF File - Tulane University
PDF File - Tulane University

... continental rocks. Furthermore, because continental rocks are at low temperature and have a very high viscosity, convective decompression is not likely to occur. Yet, as we will see, there is evidence that continental crustal rocks sometimes melt. This is called crustal anatexis. The following scena ...
Crustal Features
Crustal Features

... • The crust is part of the lithosphere, the outermost layer of the crust. • Plates are part of the crust. (continental crust/plate and oceanic crust/plate) • The convection currents in the mantle layer below and perhaps also gravity cause the plates to move. ...
Marine geochemical data assimilation in an efficient Earth System
Marine geochemical data assimilation in an efficient Earth System

... basins complicates comparison between model and paleoceanographic data (Ridgwell, 2001). In this paper we present a representation of marine biogeochemical cycling within a 3-D ocean based Earth system model, which we calibrate for the modern carbon cycle via a novel assimilation of marine geochemic ...
Simulations of the mid-Pliocene Warm Period using two versions of
Simulations of the mid-Pliocene Warm Period using two versions of

... bathymetry in this region is uncertain, since we do not know what the thickness of any previous West Antarctic Ice Sheet may have been, nor whether the region was still undergoing glacio-isostatic adjustment after the loss of such ice. The current depth to bedrock in the region varies from 500 to 20 ...
Student Study Guide
Student Study Guide

... - The sea floor is slowly moving away from the ridge (in both directions) at rates that range from about 1–20 cm (0.4–8 in) per year but are generally between 2–10 cm (0.8–4 in) per year. The average rate is about 5 cm (2 in) per year. This is roughly the rate at which fingernails grow. - Although t ...
chapter 3
chapter 3

... - The sea floor is slowly moving away from the ridge (in both directions) at rates that range from about 1–20 cm (0.4–8 in) per year but are generally between 2–10 cm (0.8–4 in) per year. The average rate is about 5 cm (2 in) per year. This is roughly the rate at which fingernails grow. - Although t ...
Sverdrup Study Guide Ch02 PDF
Sverdrup Study Guide Ch02 PDF

... in the geologic past. Evidence from ancient rocks indicates that crustal plates existed as long as 3.5 billion years ago and moved at an average rate of about 1.7 cm/yr. - Iceland is one locality where we can observe spreading activity on land. - Spreading rates can now be measured directly by satel ...
Teacher Resources - Fish Eye Project
Teacher Resources - Fish Eye Project

... ocean  crust  in  the  vicinity  of  spreading  centers  or  subduction  zones  (places  on  Earth  where  two   tectonic  plates  move  away  or  towards  one  another).  The  cold  seawater  is  heated  by  hot  magma   and  re-­‐em ...
How thick is Continental crust?
How thick is Continental crust?

... on top to about 1600 degrees Fahrenheit in the deepest parts of the crust. You can bake a loaf of bread in your oven at 350 degrees F., at 1,600 degrees F. rocks begin to melt. ...
Role of Earth`s Mantle in Water and Gases in the
Role of Earth`s Mantle in Water and Gases in the

... early degassing phase. A comparison of earthly abundance of these gases and other elements with those in the meteorites, the extra-terrestrial bodies which are also part of the solar system retaining the primordial composition, show certain disparities. While there is a general agreement with all el ...
Oceanography Chapter 12
Oceanography Chapter 12

... diameter of the particle.  Grain size and current velocity affect the deposition and erosion of sediment.  Smallest and largest particles behave similarly with respect to transportation and erosion.  Sand in the middle of the graph takes the least amount of energy to erode.  Larger particles req ...
tis the season for science - The School District of Palm Beach County
tis the season for science - The School District of Palm Beach County

... Divergent boundaries Divergent boundaries occur along spreading centers where plates are moving apart and new crust is created by magma pushing up from the mantle. You can picture two giant conveyor belts, facing each other but slowly moving in opposite directions as they transport newly formed ocea ...
tis the season for science - The School District of Palm Beach County
tis the season for science - The School District of Palm Beach County

... Divergent boundaries Divergent boundaries occur along spreading centers where plates are moving apart and new crust is created by magma pushing up from the mantle. You can picture two giant conveyor belts, facing each other but slowly moving in opposite directions as they transport newly formed ocea ...
Eriksen2014-Plastics-in-the-Ocean.pdf
Eriksen2014-Plastics-in-the-Ocean.pdf

... describes oceanic circulation and second virtual particles are introduced into the flow field and allowed to move freely through hydrodynamic forcing. For this study, ocean surface currents are extracted from the oceanic circulation modeling system HYCOM/NCODA [29]. The HYCOM model is forced by the ...
GEO/OC 103 Exploring the Deep… Lab 7
GEO/OC 103 Exploring the Deep… Lab 7

... Seafood makes up  percent of the world’s food supply, with over one billion people depending on its resources for survival. As seafood harvests have increased over the past two centuries, populations of some species of marine life have decreased and even become extinct. Given the ocean’s vast area ...
Persistent organic pollutants in ocean sediments from the North
Persistent organic pollutants in ocean sediments from the North

... the 4th Arctic expedition between July and September 2010 (CHINARE 4). The sampling stations roughly follow a latitudinal northward transect across the Bering Sea through Bering Strait and cover both the Chukchi Sea and Canadian Basin (53–88 N). In addition, 0–2 cm sediment samples were collected d ...
Geology 12
Geology 12

... indicate movement of ice away from the pole ...
pdf version - Woods Hole Oceanographic Institution
pdf version - Woods Hole Oceanographic Institution

... world ocean. Perhaps nowhere on earth is climate change having as dramatic and rapid an effect as in the Arctic, where ice cover, ocean water circulation, geochemistry, and ecosystems are all responding to the pervasive rise in air and sea temperatures. These changing conditions will not only alter ...
ASTR 330: The Solar System
ASTR 330: The Solar System

... rock, to iron, with traces of nickel, sulfur and some other elements. • The boundary occurs at a pressure of 1.3 million bars (1 bar is about the pressure at sea level) and a temperature of 4500 K. • Iron is liquid at these conditions: so the change in composition also marks a transition from solid ...
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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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