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Name: Pd: Plate Tectonics Unit Test Study Guide S6E5a. Compare
Name: Pd: Plate Tectonics Unit Test Study Guide S6E5a. Compare

... 11. Most geologists rejected Alfred Wegener’s idea of continental drift because he could not explain HOW they moved or the force that caused them to move 12. What causes the movement of tectonic plates? Convection currents below the lithosphere 13. What is Pangaea? The name of the super continent wh ...
Waves and Tides
Waves and Tides

... When the trough of a wave gets close to land, it starts to drag while the crest moves on, getting higher and higher until it tumbles over. ...
File - Native Expeditions
File - Native Expeditions

... Formed deep within the lithosphere from extreme pressure and/or heat Metamorphic rocks form in a solid state and the composition is change chemically (usually from hot water) Examples: Limestone to Marble, Shale to Slate, Granite to Gneiss ...
What is the name of the SUPERCONTINENT that was once one land
What is the name of the SUPERCONTINENT that was once one land

... B. The mantle rock is cooled near the crust, becoming more dense. C. The mantle rock is warmed near the crust, becoming less dense. D. The mantle rock does not change near the crust. ...
marine and esturian ecosystem-2012
marine and esturian ecosystem-2012

... enhanced. The lower specific gravity of sea water is most beneficial to marine organisms. As the sea water contains large number of salts it is a most suitable, environment for living cells. Further it has been found that the ratio of total saIt content of seawater is almost same as that of body flu ...
Plate Tectonics II
Plate Tectonics II

... False: The deep ocean sediment cover is very thin at the mid-ocean ridge and, although it thickens toward the continents, is much thinner than would be expected after billions of years of accumulation. ...
MB 20 : Marine Biology
MB 20 : Marine Biology

... ocean (19 yrs. to publish, 50 volumes) • Challenger Expedition (1872-1876): measuring systems used, species samples ...
Eons, Eras, Periods and Epochs Dating by radioactive isotopes
Eons, Eras, Periods and Epochs Dating by radioactive isotopes

... Discharge: The amount of water flowing through a cross section of a stream (Q in m3/s). Fluctuates seasonally and diurnally Q=wdv Capacity: The amount of sediment that can be carried by a stream (m3/s or kg/s). Capacity ...
Action at the Edge
Action at the Edge

... and weak spots in Earth's crust. You'll find those mostly along the boundaries of tectonic plates that are moving apart. Volcanoes are also common where two plates are slowly colliding and one plate is subducting under the other. The Pacific Plate is one of Earth's largest tectonic plates. It lies b ...
Lesson: Landforms and Oceans
Lesson: Landforms and Oceans

... 5-3.2 Illustrate the geologic landforms of the ocean floor (including the continental shelf and slope, the mid-ocean ridge, rift zone, trench, and the ocean basin). 5-3.3 Compare continental and oceanic landforms. 2014 Standards Correlation: Grade Four Earth Science: Changes in Landforms and Oceans ...
A unifying view of climate change in the Sahel linking intra
A unifying view of climate change in the Sahel linking intra

... Mechanisms to connect dynamics of variability and change: • Indian Ocean/warming of the tropical oceans  controls vertical stability  related to frequency of daily rainfall? • Atlantic Ocean/  controls moisture supply  related to intensity of daily rainfall? ...
Cornell Notes Template
Cornell Notes Template

... melts, forming magma o A major volcanic zone is around is around the Pacific Ring of Fire o Oceanic-oceanic → island arcs form in the ocean o Oceanic-continental → volcanoes form on land 2) Mid-ocean ridges- occur at divergent plate boundaries as plates pull apart and moves upward. As the magma reac ...
Divergent Boundary
Divergent Boundary

... ocean crust sinks into the mantle. • Subduction- process by which ocean crust sinks beneath a deep-ocean trench and back into the mantle ...
Section Quiz - TheVirtualNeal
Section Quiz - TheVirtualNeal

... zone, the lithosphere is denser than it is at a mid-ocean ridge. Convection causes oceanic lithosphere to move away from the mid ocean ridge. Oceanic lithosphere is also higher at a mid-ocean ridge, so oceanic lithosphere moves down toward the subduction zone because of gravity. Answers will vary. T ...
OUTDOOR SCIENCE SCHOOL VOC (#1 – Test)
OUTDOOR SCIENCE SCHOOL VOC (#1 – Test)

... *North American Plate *Antarctic Plate *South American Plate *Indo-Australian Plate *Eurasian Plate (c) North American Plate = continental USA, most of CA, and the San Bernardino Mountains Pacific Plate = mostly oceanic crust, Southern California & Hawaii (d) Plate movement in one year = 3-5 cm (ver ...
Dynamic Ocean Floor
Dynamic Ocean Floor

... • Two plates move away from one another. • This is a zone of weakness. • As two plates move apart at the mid-ocean ridges, magma from the mantle up wells through a crack in the oceanic crust and cooled by the sea creating new ocean floor. • Energy is released in the form of earthquakes. • Shallow fo ...
Poor Wegener - Issaquah Connect
Poor Wegener - Issaquah Connect

... In the 1950’s, new data from studies of the ocean floor provided an explanation of how continents moved. Wegener was proven right! ...
Canadian Consortium of Ocean Research Universities (CCORU
Canadian Consortium of Ocean Research Universities (CCORU

... “ocean estate” covers a surface area of approximately 7.1 million square kilometres, an area that would cover about 70 per cent of our land mass. Canada’s exclusive economic zone has a surface area of approximately 2.9 million square kilometres and extends our reach 200 nautical miles beyond its ter ...
10.2 Intrusive Igneous Activity
10.2 Intrusive Igneous Activity

... ...
sci-10-18-1 - St John Brebeuf
sci-10-18-1 - St John Brebeuf

... Yoho National Park, but you’ll find fossils of marine organisms high up in the Rockies near Field, B.C. (Figure 3). The Burgess Shale found in Yoho is fossil-bearing rock that was laid down underwater more than 500 million years ago at the edge of an oceanic plate. About 200 million years ago, as th ...
Plate Tectonics Notes
Plate Tectonics Notes

... The mid-ocean ridge is a mountain range at the bottom of the ocean that is composed mainly of volcanoes and lava flows. See m ap p. 5 E S R T The rocks created at the mid-ocean ridge have _____________ minerals that are aligned with Earth’s magnetic field. Earth’s magnetic field ______________ on a ...
Continental Margins and Marginal Seas
Continental Margins and Marginal Seas

... On the ocean side, biogeochemical processes principally occur within the top 200 meters of the sea, which are waters often associated with continental margins. Actually, the continental margins are shallower than 200 m, and they occupy only 7 per cent of the total ocean surface and even less than 0. ...
GCOS and ECVs – Some background
GCOS and ECVs – Some background

... The specific observational needs of the World Climate Programme and related earth system science and service programs; The climate change assessment role of the Intergovernmental Panel on Climate Change (IPCC); and The requirements of the UNFCCC and other international conventions and agreements. Th ...
Earth Science Milestones Review Notes Packet
Earth Science Milestones Review Notes Packet

... Weather: atmospheric conditions of a location at a certain time. Climate: the average conditions of a location over a long time (is it usually rainy, usually hot, usually cold, etc). Atmosphere: mixture of gases that distributes heat and allows life on Earth to exist. ...
Answer Key - With Teacher Comments given in class Plate
Answer Key - With Teacher Comments given in class Plate

... _Fossils_: from ancient animals appear to link continents together as wellmesosaurus (the part colored brown yesterday), lystrosaurus (freshwater reptiles) (the part colored blue yesterday), glossopteris (plant) the part colored green yesterday). Students should be able to discuss how fossils of dif ...
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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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