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Global Climates and Biomes
Global Climates and Biomes

... - lower pressure of rising air allows air to expand resulting in lower temperature c. heating - air sinks, pressure increases decreasing in volume, and temperatures increase ...
Global Climates and Biomes
Global Climates and Biomes

... - lower pressure of rising air allows air to expand resulting in lower temperature c. heating - air sinks, pressure increases decreasing in volume, and temperatures increase ...
Physical Geology - Geol 1330 (07610) - Spring
Physical Geology - Geol 1330 (07610) - Spring

... 37. Alfred Wegeners idea of continental drift was based on what observations? a) match of different fossils on the continents b) match of rock types and mountain belts c) match of glaciated areas d) all of these 38. What is the evidence that new oceanic crust is created at, and moves away from, dive ...
Plate Tectonics
Plate Tectonics

... •  The Earth is made up of 3 main layers (core, mantle, crust). •  On the surface of the Earth are tectonic plates that slowly move around the globe •  Plates are made of crust and upper mantle (lithosphere) and float on the asthenosphere •  There are 2 types of plates •  There are 3 types of plate ...
Coastal Upwelling Feat From ROMS eatures over Arabian Sea From
Coastal Upwelling Feat From ROMS eatures over Arabian Sea From

...  The increased availability in upwelling regions results in high levels of primary productivity and thus fishery production. Approximately 25% of the total global marine fish catches come from five upwellings that occupy only 5% of the total ocean area  Marine ecosystems in the ocean's eastern bou ...
Chapter 3 The Origin of Ocean Basins LEARNING OBJECTIVES 1
Chapter 3 The Origin of Ocean Basins LEARNING OBJECTIVES 1

... 4. Sea floor increases in age away from the ridge and is more deeply buried by sediment because sediments have had a longer time to collect. 5. Rates of sea-floor spreading vary from 1 to 10 cm per year for each side of the ridge and can be determined by dating the sea floor and measuring its distan ...
Plate tectonics
Plate tectonics

... measure how long the total length of subduction boundaries there are on the planet at present using a printed plate boundary map and a piece of string or cotton (this will be very rough as the maps is a distorted projection). Using this type of map projection, lengths are increasingly over estimated ...
Cooling of the Ocean Plates (Lithosphere)
Cooling of the Ocean Plates (Lithosphere)

... The depth of the seafloor can be calculated using the principal of isostacy - different columns contain the same mass (i.e., the lithosphere floats). Because warm rocks have a lower density (denoted by the symbol  ) than cold ones, the seafloor is shallower above young ocean lithosphere. ...
Year 3 Plate Tectonics
Year 3 Plate Tectonics

... The Andes are located where the Nazca Plate, made of dense oceanic crust, is subducted beneath the South American Plate, made of lighter continental crust. More than 100 million years ago, the Andes began to form by the uplifting and folding of sedimentary rocks accumulated along the edge of the con ...
Deep life: Teeming masses of organisms thrive beneath the seafloor
Deep life: Teeming masses of organisms thrive beneath the seafloor

... entire cast of the Muppets in there.” Plenty of data should be forthcomBy comparing microbes from different seafloor sites, Biddle has found surpris- ing. “We’re not suffering from a lack of ingly high amounts of archaea compared things to do,” Orcutt says. Edwards and with bacteria in some places. ...
Content review with outline and thought questions
Content review with outline and thought questions

... c. Compensation depth is the depth where net primary productivity equals zero. - This is usually located where light intensity is about 1% of its surface value and typically occurs at a depth of about 110 m in clear ocean water. d. Most of the light entering the ocean is converted into heat. - Produ ...
MODULE #1: The Oceans of Our Planet Introduction This course is
MODULE #1: The Oceans of Our Planet Introduction This course is

... In fact, many parameters of our earth have not been constant over time, including the earth’s magnetic field. Thus, there is no reason to believe that the plates have always moved slowly. During a catastrophic event, the plates might have moved apart from each other very quickly. In fact, there is a ...
Take Home 11 Complete the following on your own paper. Do not
Take Home 11 Complete the following on your own paper. Do not

... 2) What kind of movement on a plate boundary causes mountain building? A. Divergent movement C. Transform movement B. Convergent movement D. Biome movement 3) Which of the following discoveries caused science to re-evaluate its opinion of Wegener's hypothesis about continental drift? A. Sea floor sp ...
Chapter 9. Conclusions on Major Ecosystem Services Other than
Chapter 9. Conclusions on Major Ecosystem Services Other than

... Even in cases where the appropriate skills exist, some parts of the world lack institutions with the status, resources and commitment to make the necessary inputs into decision-making that will affect a range of ecosystem services from the oceans. The many institutions that already exist to study th ...
When drilling stopped in 1994, the hole was over seven miles deep
When drilling stopped in 1994, the hole was over seven miles deep

... renovations of the equipment on hand, so drilling stopped on the SG-3 branch. If the hole had reached the initial goal of 15,000 meters, temperatures would have reached a projected 300°C (572°F). When drilling stopped in 1994, the hole was over seven miles deep (12,262 meters), making it by far the ...
volcanic islands
volcanic islands

... •Associated with hot spots and mid-ocean ridges If seamounts break the surface of the ocean, they create volcanic islands •The biggest mountain on earth is Mauna Loa (Hawaii). ...
study guide questions 3rd nine weeks 2017
study guide questions 3rd nine weeks 2017

... Draw and describe the 4 types of weather fronts. Describe the 5 types of air masses and their characteristics. Explain why it is warmer at the equator then other places on earth How are the sun moon and earth aligned during a spring tide? A neap tide? Explain how much salinity ocean water contains o ...
Internal Structure of the Earth File
Internal Structure of the Earth File

... No S waves can travel through angles greater than 1030 hence the boundary at B must separate solid from liquid. This is the evidence that the outer core is made of a dense liquid. ...
Translation Series No. 421
Translation Series No. 421

... of the water in the sea. Tests show that the photosynthesis determined In bottles with the same water samples gave close results when held in the sea and when on deck in the vat. For example, at station 12 bottles. held In the sea had photosynthesis equal to 0.0754 mg/1 9 while bottles in the vat ha ...
The Indian-Atlantic Ocean gateway during the Pliocene: current
The Indian-Atlantic Ocean gateway during the Pliocene: current

... 361 – Southern African Climates and Agulhas LGM Density Profile by Gruetzner et al., this Volume). Our new research proposal focuses on three of these sites forming a latitudinal transect in the Atlantic-/Indian Ocean gateway and combines chemical, physical property and seismic methods. Primary site ...
plate tectonics article from nat'l geo. fall 2012
plate tectonics article from nat'l geo. fall 2012

... There are a few handfuls of major plates and dozens of smaller, or minor, plates. Six of the majors are named for the continents embedded within them, such as the North American, African, and Antarctic plates. Though smaller in size, the minors are no less important when it comes to shaping the Eart ...
The Theory of Tectonic Plates
The Theory of Tectonic Plates

... The volcanic country of Iceland, which straddles the Mid-Atlantic Ridge, offers scientists a natural laboratory for studying on land the processes also occurring along the submerged parts of a spreading ridge. Iceland is splitting along the spreading center between the North American and Eurasian ...
Study Guide for The Theory of Plate Tectonics Chapter 3
Study Guide for The Theory of Plate Tectonics Chapter 3

... Convection Currents: Slow circular motion of molten rock in the Earth’s mantle move the lithosphere around. Older material is more dense, so gravity pulls the material back into the mantle through convection currents. Plate Movement: The plates move very slowly, between 1 and 12 cm per year. The Nor ...
3-2
3-2

... terrestrial and aquatic ecosystems found in an area or on the earth. ...
Vision for 2030 - Ministry of Earth Sciences
Vision for 2030 - Ministry of Earth Sciences

... The first climate model from India to contribute to the forthcoming IPCC climate change assessment process. â A 21-member Global Ensemble Forecasting System (GEFS) based on the GFS (22 km resolution) and a 44 member global ensemble prediction system (33 km horizontal resolution) based on UM for rea ...
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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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