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... Oceanic-continental convergence Ocean plate subducted  Continental arc  Oceanic trench  Deep earthquakes ...
Prepared by: Raed M.Khaldi
Prepared by: Raed M.Khaldi

... heat with little change in temperature. Another way of looking at it is that it is difficult to raise or lower the temperature of water; it prefers to remain at whatever temperature it is at. - The latent heat of fusion is the heat required to change 1 gram of pure water from solid to liquid at 0°C. ...
Name ____Justin Powers______ Date ______ Period ____ Plate
Name ____Justin Powers______ Date ______ Period ____ Plate

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

... magma pushing up from the mantle. Picture two giant conveyor belts, facing each other, but slowly moving in opposite directions as they transport newly formed oceanic crust away from the ridge crest (center). Perhaps the best known of the divergent boundaries is the Mid-Atlantic Ridge. This is a sub ...
origin of tsunami
origin of tsunami

... preceded by another natural hazard – the earthquakes. More than 230,000 lives have been lost in the tsunami 2004 in the 11 stricken countries around the Indian Ocean, which include Indonesia, Sri Lanka, Thailand, India, Maldives, and Somalia. ...
Plate Tectonics |Sample answer
Plate Tectonics |Sample answer

... Convergent Boundaries are when two plates come together. The older heavier plate will slip under the younger lighter plate. This is called subduction. Convergent plates are destructive boundaries as the rock is destroyed as it comes into contact with the magma. When two oceanic plates collide the ol ...
DELIVERING INTEGRATED MARINE OBSERVATIONS
DELIVERING INTEGRATED MARINE OBSERVATIONS

... MONITORING WEATHER AND CLIMATE FROM SPACE ...
CEUS Eq Overview
CEUS Eq Overview

... Center for Earthquake Research and Information ...
Ocean Crust - The University of Southern Mississippi
Ocean Crust - The University of Southern Mississippi

... b. The rest of the crust is weakly magnetized, but holds a lot of mass and magnetic signal. 4. The ocean crust (basalt and gabbro) forms the top (<10%) of the lithosphere, which is in total ~100 km thick. The lithosphere below the crust is made of the uppermost mantle (peridotite and related rocks). ...
IBDIOCC - Scientific Committee on Oceanic Research
IBDIOCC - Scientific Committee on Oceanic Research

... Scientific Background and Rationale Deep-Sea Overview: The biodiversity and ecosystem functioning can change quickly and significantly because of direct (e.g. bottom trawling, deep-water oil spills) and indirect (e.g. climate variation) human impacts (Smith et al, 2009). In addition, two new pressu ...
coral reefs - bankstowntafehsc
coral reefs - bankstowntafehsc

... the Year and Scientist at Macquarie Uni) ...
7-2 Restless continents
7-2 Restless continents

... 2. According to Wegener, how many landmasses did all continents once form? ______ 3.______What did Wegener hypothesize happened to the continents? a. They broke up and re-formed. b. They drifted together to form a single continent. c. They broke up and drifted to their current locations. d. They san ...
Downloaded
Downloaded

... as seen from table 1, some nutrients are not associated with carbon such as the nitrogen gas from the atmosphere and furthermore settling particles do not always have a Redfield composition. The availability of nutrients in the oceans and their means of supply vary considerably from one region to ano ...
OCEAN PICTURES - ScholarWorks
OCEAN PICTURES - ScholarWorks

... supernatural. When first spotted, the whale seems sublimely beautiful to Ishmael and the crew—“not Jove did surpass the glorified White Whale as he so divinely swam”—but conceals his true, horrific nature: “…Moby Dick moved on, still withholding from sight the full terrors of his submerged trunk, en ...
Large-scale fluctuations in Precambrian atmospheric and oceanic
Large-scale fluctuations in Precambrian atmospheric and oceanic

... carbonates deposited between  2.22 and 2.06 Ga (8‰ and higher, Karhu and Holland, 1996). Conservative estimates for oxygen release coupled to increased organic carbon burial during the Lomagundi Event range from 12 to 22 times the present atmospheric inventory (Karhu and Holland, 1996). However, so ...
plates - edl.io
plates - edl.io

... The Crust The crust is composed of two rocks. - The continental crust is mostly granite. - The oceanic crust is basalt. Basalt is much denser than the granite. Because of this the less dense continents ride on the denser oceanic plates. ...
Stability of North Atlantic water masses in face of pronounced
Stability of North Atlantic water masses in face of pronounced

... [1] Geochemical profiles from the North Atlantic Ocean suggest that the vertical d13C structure of the water column at intermediate depths did not change significantly between glacial and interglacial time over much of the Pleistocene, despite large changes in ice volume and iceberg delivery from ne ...
Jigsaw Readings
Jigsaw Readings

... Just as when stretching chewing gum or rubber bands, stretching plates will eventually break and begin to rip apart. Geologists can observe this process happening today at many places on Earth. The point where plates have broken apart is called a rift. Rifts occurring in crustal plates under the con ...
Plate Tectonics PowerPoint
Plate Tectonics PowerPoint

... – A subduction zone forms when one oceanic plate, which has become denser as a result of cooling, descends below another plate creating a deep-sea trench. – The subducted plate descends into the mantle and melts. – Some of the magma forms new oceanic crust at the ridge or is forced back to the surfa ...
Answers to Plate Tectonics Study Guide
Answers to Plate Tectonics Study Guide

... Geology = Wegener found the same rock layers in South America and Africa. Climate = Wegener found tropical plant fossils in Greenland which is very cold today. 9. Scientists did not believe Alfred Wegener because he could not explain how the plates in the Earth moved. 10. Divergent 11. The scientist ...
Name Date ______ Period ____ Plate Tectonics Web
Name Date ______ Period ____ Plate Tectonics Web

... 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_____________, beneat ...
The Earth - WordPress.com
The Earth - WordPress.com

... Jupiter in a region called the asteroid belt. A few asteroids follow paths that cross the earth’s orbit. Comets, made of icy dust particles and frozen gases, look like bright balls with long, feathery tails. Their orbits are inclined at every possible angle to the earth’s orbit. They may approach fr ...
Salinity
Salinity

... Survival manuals consistently advise against drinking seawater.[24] A summary of 163 life raft voyages estimated the risk of death at 39% for those who drank seawater, compared to 3% for those who did not. The effect of seawater intake on rats confirmed the negative effects of drinking seawater when ...
1 The Catastrophic Plate Tectonics Model Six of the world`s top
1 The Catastrophic Plate Tectonics Model Six of the world`s top

... forming new rock which would become the new oceanic plates. These rocks reflect the magnetic field of the Earth at the time they cooled. They show this flip-flopping of the Earth’s magnetic field during this time in a zebra stripe pattern. Thing Three – The Rains Came Down and the Floods Came Up As ...
Coupling between Wind-Driven Currents and Midlatitude Storm Tracks
Coupling between Wind-Driven Currents and Midlatitude Storm Tracks

... planetary scale of the wind-driven ocean circulation suggests that a more realistic spherical geometry be used. On a sphere, the westward phase speed of Rossby waves becomes a function of latitude, an effect that might be important given the quasigeostrophic result that the timescale for Rossby wave ...
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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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