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Pymble Trial without Solutions
Pymble Trial without Solutions

... (C) It removed toxins and iron from the ocean. (D) It is only found as a fossil in Australia. ...
Where are the jellyfish?
Where are the jellyfish?

... nuclear reactor to shutdown > In 2007, jellyfish wiped out a salmon farm in Northern Ireland killing 100 000 fish ...
EffectofTemponSolubilityofSaltGCCEGLX
EffectofTemponSolubilityofSaltGCCEGLX

... creating a dense solution that begins to sink. Colder, less dense water rushes up to replace the sinking denser water, creating convection currents in our oceans. Ocean currents bring warmth from the equator toward the poles of the Earth. As global temperatures continue to rise, the increase in ocea ...
OCN 201: Plate Tectonics II
OCN 201: Plate Tectonics II

... • Recycling of oceanic sediments and basalt crust back into mantle at subduction zones ...
Commotion Beneath the Ocean
Commotion Beneath the Ocean

... Convection • Heated material expands - becomes less dense - more buoyant • It rises and cold material takes it’s place ...
IODE Regional Coordinator Report for IOCINDIO
IODE Regional Coordinator Report for IOCINDIO

... As a faculty member for the training course on Marine Information Management for ocean Data /information management network held in South Africa 28 Oct.-6 Nov.2001 IOC Mission to assist NODC, Sri Lanka, Colombo, 4-10 November, 2001, Training on oceanographic data/ information management was provided ...
Plate Tectonics 1
Plate Tectonics 1

... A magnetometer towed behind a boat will pick up a weak field if the crystal magnets point the opposite direction from the Earth’s field. (They partly cancel each other out). ...
Plate Tectonics - My Teacher Pages
Plate Tectonics - My Teacher Pages

... liquid by the circulation of currents from one region to another  Convection cell is a circular-moving loop of matter (gas or liquid) involved in convection movement ...
Teacher lesson plan pdf - eGFI
Teacher lesson plan pdf - eGFI

... Scuba diving is an excellent hobby for underwater naturalists. Along the California coast, scuba divers can see kelp forests, sea otters, many species of fish, sea lions, and a variety of invertebrates such as octopuses, crabs and urchins. With the aid of specialized equipment, divers can prolong th ...
I-5 Notes
I-5 Notes

... Volcanoes and Plate Movements • Volcanoes are formed along the midocean ridges • These volcanoes are very numerous • Most are deep in the ocean • If activity is strong enough, may build an island above sea level (Example – Iceland) ...
Chapter 2 Tectonic Theory (A)
Chapter 2 Tectonic Theory (A)

... continents ◦ Edward Bullard fit continents at 2000m water depth Fig. 2.3 ...
Double-Diffusive Convection and Interleaving in the Arctic Ocean
Double-Diffusive Convection and Interleaving in the Arctic Ocean

... Beneath its ice cover the Arctic Ocean is a low energy environment. The weak turbulent activity allows other, more esoteric mixing mechanisms to become important in transforming the water masses. One such process is double-diffusive convection, which is triggered by the different molecular diffusion ...
2012 OCSD Diversion Synthesis Report Template
2012 OCSD Diversion Synthesis Report Template

... more constrained and variable than that seen with CDOM and salinity. However, when present, elevated NH3-N values were typically co-located with higher CDOM and lower salinity. Environmental and Public Health Impacts No phytoplankton blooms were seen during the time the short outfall was in operatio ...
DESTRUCTIVE CONVERGENT PLATE MARGINS: SUBDUCTION
DESTRUCTIVE CONVERGENT PLATE MARGINS: SUBDUCTION

... Subducting plate moves, over-riding plate stationary ...
Lab-Isostasy.doc
Lab-Isostasy.doc

... It is a somewhat puzzling fact that we observe piles of sediment, up to several kilometers deep, that was entirely deposited in a shallow ocean environment. In this exercise we simulate a coastal mountain range, such as the Appalachians, and associated coastal margin sedimentation. We will simulate ...
File
File

... 8. Dividing the Earth into layers based on chemical composition results in three layers--crust, mantle, core--with pronounced differences in chemical composition (or mineral makeup) of these layers. In contrast, dividing the Earth into layers based on how the rocks respond to increased temperature a ...
EARTH/ENVIRONMENTAL SCIENCE REVIEW GUIDE – ANSWERS!!!
EARTH/ENVIRONMENTAL SCIENCE REVIEW GUIDE – ANSWERS!!!

... Cold water is more dense than warm water, therefore the colder water at the bottom of the ocean tends to remain at the bottom due to density differences. The area where temperature changes quickly from warm to cold water is known as the thermocline. The analygous area between the high & low densitie ...
Pre/Co-Requisite Challenge for Field Courses
Pre/Co-Requisite Challenge for Field Courses

... the  course.  The  student  should  have  a  basic  understanding  of  (1)  Rocks  and  the   Rock  Cycle,  (2)  Plate  Tectonics,  and  (3)  Geologic  Time  (see  Topics  of  Study  below).     To  aid  in  studying,  direct  the ...
Slide 1
Slide 1

... enough water to fill a vast ocean. ...
Marine Environmental Prediction in the Atlantic Coastal Region
Marine Environmental Prediction in the Atlantic Coastal Region

... Funding for these upgrades was provided by the CSSF and by grants by the Canada Foundation for Innovation and the British Columbia Knowledge Development Fund to Ross Chapman and Verena Tunnicliffe, both at the University of Victoria. ROPOS has operated from more than a dozen support ships from four ...
Evaluating the lines of evidence for plate tectonics
Evaluating the lines of evidence for plate tectonics

... The
second
map
illustrates
sediment
thickness
on
the
ocean
floor.
The
top
black
and
white
 map
illustrates
the
location
of
mid‐ocean
ridges.
The
lower
black
and
white
map
illustrates,
 among
other
things,
the
location
of
deep‐sea
trenches.
Use
the
appropriate
map(s)
when
 thinking
about
these
questi ...
Plate Tectonics - Nogales High School
Plate Tectonics - Nogales High School

... continents once formed part of a single landmass called a supercontinent. This supercontinent began to break up into smaller continents about 250 million years ago. ...
Chapter 13 - Volcanoes
Chapter 13 - Volcanoes

... › May flow out of a vent, cool, and build up a cone of material that may become a mountain. ...
Oceanography—Plate Tectonics Name
Oceanography—Plate Tectonics Name

... A combination of ideas lead to the development of the theory of plate tectonics. The first important idea—continental drift—was proposed by Alfred Wegener in the early 20th century. Wegener observed that in a number of areas of the contemporary world, coastlines seemed to match as though they had on ...
[1 pt] X.
[1 pt] X.

... surface. The ocean and the atmosphere exchange gas with one another. CO2 increases in surface waters. CO2 dissolved in ocean surface waters forms H2CO3 (carbonic acid), which then dissociates to form H+ (hydrogen ion) and HCO3- (bicarbonate ion). The concentration of each of these ions is pH depende ...
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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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