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Chapter 02
Chapter 02

... 18. The vast single ocean present about 200 million years ago is called A. Sinus Borealis. B. Pangaea. C. Tethys. D. Panthalassa. E. Gondwana. 19. Lithogenous sediments are those that come from A. plants. B. living organisms in general. C. deep-water volcanoes. D. erosion of land. E. corals. 20. The ...
The Theory of Seafloor Spreading
The Theory of Seafloor Spreading

... seafloor is being created. Rift Valley – The valley between the ridges where lava rises on the ocean floor and forms new rock. Trench – Deep, steep, narrow crack in the ocean floor where old sinks back into the mantle and is recycled. ...
Earth Science Chapter 17: Plate Tectonics
Earth Science Chapter 17: Plate Tectonics

... • Developments in sonar technology enabled scientists to measure water depth and map the topography of the ocean floor. ...
The two major areas of the ocean floor are the and the
The two major areas of the ocean floor are the and the

... 12. Scientists working in the ________________ hemisphere had trouble catching on to his hypothesis. 13. The biggest problem scientists had with his hypothesis was the ________________ that caused the continents to drift. 14. Wegener’s explanation for how the continents moved was based on __________ ...
Bellringer: Oceans are not just places… The Water Planet
Bellringer: Oceans are not just places… The Water Planet

... slope, and continental rise descending to the abyssal plain • Active continental margins have continental shelves and slopes, but the slope extends down into a deep oceanic trench • A mid-oceanic ridge system encircles the globe, typically running down the center of oceans • Numerous conical seamoun ...
THE EARTH`S LITHOSPHERE
THE EARTH`S LITHOSPHERE

... the oceans and 65 km depth in the continental crust formed by the interaction between the lithosphere and upper mantle, which consists of a viscous material called high-temperature magma that is concentrated on the upper mantle from the mantle and sometimes comes to the surface through volcanoes. Is ...
Notes: Plate Tectonics
Notes: Plate Tectonics

... • Mantle rock rises slowly from the bottom of the mantle toward the top. The hot rock eventually cools and sinks back through the mantle. Over and over the cycle of rising and sinking takes place. • Convection currents like these have been moving inside Earth for more than four billion years! ...
Chapter 9 Planetary Geology What are terrestrial planets like on the
Chapter 9 Planetary Geology What are terrestrial planets like on the

... Thought Question What is necessary for differentiation to occur in a planet? a) It must have metal and rock in it b) It must be a mix of materials of different density c) Material inside must be able to flow d) All of the above e) b and c ...
1.7 MB - arcus
1.7 MB - arcus

... two naturally occurring radium isotopes 228Ra (T1/2= 5.77y) and 224Ra (T1/2= 3.6d) are being used. Because these isotopes are derived solely through input from shelf sediments, they are unambiguous markers of water that has been in contact with shelves. Their relative distribution in shelf and basin ...
The first observations, September 1998, CMOS Bulletin.
The first observations, September 1998, CMOS Bulletin.

... American dual-frequency radar sensor that is turned on for nine of ten cycles. “Poseidon” is the French radar unit that samples on the tenth cycle. Early studies showed the rms accuracy of TOPEX/Poseidon sea surface height measurements, after all corrections, to be about 5 to 7 cm. Physical oceanogr ...
Ocean and Coastal Processes Ocean Basins Ocean Basins Tides
Ocean and Coastal Processes Ocean Basins Ocean Basins Tides

... • Both in Atlantic and Pacific • Average storm wave heights are measured ...
Testimony of Mr. Robert C. Penney August 21, 2002 Anchorage, Alaska
Testimony of Mr. Robert C. Penney August 21, 2002 Anchorage, Alaska

... species of marine mammals, birds, and fish. Species in decline in the second half of the 20th Century in Alaska include the Steller sea lion, prominent seabird species, such as the black-legged kittiwake, and keystone prey species such as the sand lance, a small fish that supports marine birds, mamm ...
File - Sturgeon City
File - Sturgeon City

... The crust is a thin outer layer of the earth where we live. It varies from 5k to 70km thick. The part that we live on is the continental crust whereas the part that is in the ocean is the oceanic crust Mantle The second layer is the mantle. The mantle is much thicker than the crust. Together they (c ...
Magnetic Reversals
Magnetic Reversals

... ocean floor. Each strip therefore represents an epoch of one or the other magnetic polarity, and the symmetry is also explained. It is as if the sea-floor was a giant tape recorder, with twin tapes emerging from the mid-Atlantic ridge, recording the Earth's magnetism at the time they emerge and then ...
mauna kea - National Geographic
mauna kea - National Geographic

... The geologic landscape of Hawaii’s islands has changed greatly over time, which has also impacted its ecologic landscape. As Hawaii’s volcanic islands rise and fall, organisms must adapt to a series of transitional habitats both above and below the ocean surface. In terms of the habitats and species ...
A Call for Deep-Ocean Stewardship
A Call for Deep-Ocean Stewardship

... workshop held in Mexico City in 2013 (www.indeep-project. org/deep-ocean-stewardship-initiative), cohosted by Instituto de Ciencias del Mar y Limnología at Universidad Nacional Autonoma de Mexico, Center for Marine Biodiversity and Conservation at Scripps Institution of Oceanography, and the Interna ...
Chapter 9
Chapter 9

... Geology of Venus The thick cloud cover of the planet completely hide the surface of Venus. No visual images from the surface of the planet are available. All the images shown here (except for the image from Venera) are radar images . Radar: Radio waves are emitted towards the surface , they bounce ...
Chapter 4: Plate Tectonics
Chapter 4: Plate Tectonics

...  Wegener’s hypothesis was that all the continents were once joined in a single landmass and have since ...
Test review Key File - Northwest ISD Moodle
Test review Key File - Northwest ISD Moodle

... 17. What are isostatic sea level changes a result of? Plate movement (sea floor spreading) and thermal expansion 18. The magnetic pattern from magnetic field reversal around a sea floor spreading site could be described as a zebra pattern 19. Subduction zones are associated with which type of plate ...
Review sheet for Exam 1, Locations and Maps
Review sheet for Exam 1, Locations and Maps

... ASTR/GEOL 1070: The Earth: Its Physical Environment ...
Chapter 16: Geology of the Ocean
Chapter 16: Geology of the Ocean

... that time, Pangaea began to break up into smaller continents that moved over the surface of Earth, ultimately reaching their present positions. What is the evidence that the present-day continents originated in the single landmass Pangaea? Wegener cited the similarities of fossils and rock formation ...
NANOOS
NANOOS

... international network of observations and data transmission, data management and communications, and data analyses and modeling that systematically and efficiently acquires and disseminates data and information on past, present and future states of the oceans and U.S. coastal1 waters to the head of ...
NOAA Mid Oceanic Ridges
NOAA Mid Oceanic Ridges

... 3. The nearly _______________, global mid-ocean ridge system snakes across the Earth’s surface like the seam on a baseball. It is clearly visible on this map of global topography above and below sea level. 4. The ridge system forms the ___________ and ____________ mountain range on Earth. It winds i ...
convection-and-the-mantel-1st-one-of-week-5
convection-and-the-mantel-1st-one-of-week-5

... continents Africa, South America, Australia, India, and Antarctica. This is very strong evidence that all of the land where the ferns grew was at a different place than now. The ferns need a warm moist climate to grow and Antarctica isn't either of those. ...
The Solid Earth
The Solid Earth

... of plants and animals ...
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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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