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6-5 Ocean Life Zones PPT - Lyndhurst School District
6-5 Ocean Life Zones PPT - Lyndhurst School District

... THE GLOBAL OCEAN Ø  vast wilderness, much of it unknown Ø  affects cycles of matter on land, influences ...
Physics 127 Descriptive Astronomy Homework #10
Physics 127 Descriptive Astronomy Homework #10

... 5-2. What is unique about the behavior of water compared to other common substances? Water has several unique properties not exhibited by other common substances: (1) It can absorb or lose a great deal of internal energy with a relatively small consequent temperature change. (In the language of phys ...
Section 1: Earth`s Interior (pages 16 – 24)
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... 2. Fossils 3. Climate Deep in the ocean, the temperature is freezing! There is no light and there are not many living things! Yet some areas of the deepocean floor are filled with life. ...
Ocean Margins - Penn State York Home Page
Ocean Margins - Penn State York Home Page

... Consisting of the “shelf “and “slope”. The continental margin extends to where the granitic continental crustal rock stops and the ocean crust basalt begins. This point is associated with the “rise”. ...
Using oxygen isotope ratios to constrain glacial
Using oxygen isotope ratios to constrain glacial

... 21. Can explain many more details such as: a. we don’t use the true ratios, but d18O (show the equation and explain Standard Mean Ocean Water 18O/16O) b. How are 18O/16O measured (mass spectrometer) c. Other controls on 18O/16O in forams d. Typical forams used in these types of measurements e. Other ...
Conditions differ away from shore.
Conditions differ away from shore.

... (FY-toh-PLANGK-tuhn) live at or near the sunlit surface. Like plants, phytoplankton convert sunlight and carbon dioxide into food and oxygen. In fact, phytoplankton convert about as much carbon dioxide into oxygen as all land plants combined. Phytoplankton are an important source of the oxygen that ...
4 layers of Earth and Plate Activity notes
4 layers of Earth and Plate Activity notes

... Milky Way- cut in half • Chocolate- crust- thinnest layer made of rocks and soil (land we walk on and under the sea) • Caramel- mantle- holt molten rock, what would come out of a volcano • Light brown layer- outer core- liquid iron • Bottom layer of chocolate- inner core, solid iron and is the hott ...
The Ocean Takes Shape
The Ocean Takes Shape

... 4. Students confuse the enhanced greenhouse effect with issues regarding the ozone hole. The enhanced greenhouse effect and ozone hole are often discussed simultaneously, and therefore, students incorrectly think that these two result in global climate change. In fact, the two phenomena are not clos ...
Magma Supply Vs Magma Plumbing
Magma Supply Vs Magma Plumbing

... Earth Plate tectonics replace 2/3 of the surface every ~100 Myr and modifies the remaining 1/3 on geologically short timescales. Evidence at a scale we might see on other planets 1. Linear rifts and arcuate compression zones 2. Transform faults and fracture zones (adjacent transform faults are para ...
Chapter 3
Chapter 3

... • World ocean - single, large interconnected body of water. • Covers 70% of the Earth’s surface • Regulates the Earth’s climate • Largest - Pacific • Atlantic • Indian • Arctic - Smallest ...
•
•

... INVESTIGATING EARTH’S DYNAMIC PROCESSES ...
CHAPTER 13 THE OCEAN FLOOR
CHAPTER 13 THE OCEAN FLOOR

... downslope from the continental shelf to the deep-ocean floor. Turbidity currents deliver these sediments to the base of the continental slope, and when these muddy currents emerge from the mouth of a canyon onto the flat ocean floor, they drop their load in a form of deep-sea fan. ii. Active contine ...
oceanic - Southern Local Schools
oceanic - Southern Local Schools

... does. If it were not for this function of the ocean, the average air temperature on Earth would vary from above 1000 C during the day to below –1000 C at night. This rapid exchange of energy between the atmosphere and the Earth’s surface ...
Earth`s Oceans
Earth`s Oceans

... does. If it were not for this function of the ocean, the average air temperature on Earth would vary from above 1000 C during the day to below –1000 C at night. This rapid exchange of energy between the atmosphere and the Earth’s surface ...
Semester 1 Review - Lemon Bay High School
Semester 1 Review - Lemon Bay High School

... 50. What has a large impact on the heights and patterns of tides? ...
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Review for CFE-answers

... collection, display and analysis Experimental- used when comparing an experimental group to a control group. Typical of the scientific process. ...
Earth 50 2nd Midterm Exam November 14, 2005 Multiple Choice (2
Earth 50 2nd Midterm Exam November 14, 2005 Multiple Choice (2

... B) carbon dioxide (CO2) C) nitrogen (N2) D) oxygen (O2) E) water vapor (H2O) 12. Which area provides the moisture for rainfall in the Amazon Basin of South America? Take into account where evaporation is greatest and wind directions. A) Northern Atlantic B) Southern Atlantic C) Western Atlantic D) E ...
pdf
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... Geostrophic gyres are gyres in balance between the pressure gradient and the Coriolis effect. Of the six great currents in the world’s ocean, five are geostrophic gyres. Note the western boundary currents in this map. ...
Table of Contents - Mr. Tobin`s Earth Science Class
Table of Contents - Mr. Tobin`s Earth Science Class

... Layer of sediment on oceanic crust is only a few hundred meters thick. Layer of sediment on continental crust is 20 kilometers thick. ...
Lique ice heated bel..
Lique ice heated bel..

... sea ice. Based on these findings, Rippeth and colleagues suggest that the spatial variations of vertical mixing are mostly driven by variations in tidal dissipation, which can be locally important. These results improve our understanding of the mechanisms that can transfer heat from warm Atlantic wa ...
Earth`s Interior
Earth`s Interior

... 4. Describe what happens when a. two plates carryingoceanic crust collide, b. two plates carryingcontinental crust collide,and c. a plate carrying oceanic crust collideswith a plate carryingcontinental crust. ...
Ocean Floor
Ocean Floor

... CONTINENTAL CRUST = THICK AND LEIGTHER ...
Oceanography Chapter 4 Bathymetry
Oceanography Chapter 4 Bathymetry

... ♦ water depth – 140 m (460 ft) ♦ exceptions in Antarctica/Greenland (300-400) Submarine Canyons ♦ Cut into shelf and slope ♦ Some as big as Grand Canyon ♦ How? Originally thought that they may have formed from sea level changes and erosion, but there: 1929 Quake in New F. ♦ Broke cables – immediatel ...
Seafloor Spreading
Seafloor Spreading

... The mid ocean ridge goes around the world (just like a baseball seam). ...
How Plates Create
How Plates Create

... When two plates of oceanic crust collide, one plate sinks beneath the other. ...
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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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