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Chapter 7 Review - Plate Tectonics
Chapter 7 Review - Plate Tectonics

... This review is simply a tool to help you to begin to think about and review some of the material we covered and you must know for your test. In addition to completing this review, you should look over your notes, worksheets, the book, and any other material given. EVERYTHING we discussed and learned ...
Plate Tectonics
Plate Tectonics

... ________ ______- is liquid. ___________- is the ___________ layer and is described as _______________. It has the characteristics of a ________________, but flows as a _____________ under pressure. ________ - (outermost layer)- varies in thickness & composition. Oceanic crust is more __________ than ...
Marine Provinces and the Ocean Floor
Marine Provinces and the Ocean Floor

... continental shelves, but are best developed on the continental slopes. Some Canyons can be traced across the shelf to associated streams on land. Some can not. Strong currents move through these canyons and are ...
Mid-Ocean Ridge
Mid-Ocean Ridge

...  2. Name the ROV that explored the Titanic.  3. Name the HOV that explored hydrothermal vents.  4. Name the bathyscaphe that traveled to the Mariana Trench  5. What is one piece of information a scientist could gather from an ocean corer? ...
PART 1 - earth science!
PART 1 - earth science!

... 1. Scientists today use sonar to study the ocean floor. Studying the ocean floor helps scientists better understand what is happening to our Earth. ...
1 Part 2. Oceanic Carbon and Nutrient Cycling Lecture Outline 1
1 Part 2. Oceanic Carbon and Nutrient Cycling Lecture Outline 1

... Marine Biogeochemical Cycles) ...
PhET Plate Tectonics Simulation Lab
PhET Plate Tectonics Simulation Lab

... PhET Plate Tectonics Simulation Lab Pre-lab: What does subduct mean, in terms of tectonic plates? _________________________________ Why does subduction occur (what causes it)? ______________________________________ _____________________________________________________________________ Go to https://p ...
Langmuir circulations and enhanced turbulence beneath wind
Langmuir circulations and enhanced turbulence beneath wind

... the NBUC, the deeper and colder flow transporting NADW presents more or less alternate periods with northward and southward (predominant) transports along the continental slope. Examples of speed time series obtained in simulations are plotted in Figure 9. These results correspond to current vectors ...
12.1 Evidence for Continental Drift How Can Continents Move? Sea
12.1 Evidence for Continental Drift How Can Continents Move? Sea

... taken from the Mid-Atlantic Ridge were younger than other ocean rocks.  Sediments along the ridge became thicker farther away from the ridge.  Paleomagnetism shows that iron-based rocks along the ridges are striped with reversing magnetic fields. Volcanoes are frequently found on boundaries betwee ...
12.1 Evidence for Continental Drift
12.1 Evidence for Continental Drift

... taken from the Mid-Atlantic Ridge were younger than other ocean rocks.  Sediments along the ridge became thicker farther away from the ridge.  Paleomagnetism shows that iron-based rocks along the ridges are striped with reversing magnetic fields. Volcanoes are frequently found on boundaries betwee ...
12.1 Notes - power point
12.1 Notes - power point

... taken from the Mid-Atlantic Ridge were younger than other ocean rocks.  Sediments along the ridge became thicker farther away from the ridge.  Paleomagnetism shows that iron-based rocks along the ridges are striped with reversing magnetic fields. Volcanoes are frequently found on boundaries betwee ...
1 Midterm Exam I September 26, 2:10 HW714
1 Midterm Exam I September 26, 2:10 HW714

... Lithosphere & Asthenosphere:: More detailed description of Earth’s layered structure according to mechanical behavior of rocks, which ranges from very rigid to deformable 1. lithosphere: rigid surface shell that includes upper mantle and crust (here is where ‘plate tectonics’ work), cool layer 2. as ...
What is Plate Tectonics?
What is Plate Tectonics?

... Two Causes of Plate Tectonics • Hot ___________ in the Earth moves toward the surface, cools, get denser, and then sinks again with the pull of gravity. This creates ______________________________ in the ______________________ which causes the plates to move. • When plates move together the ________ ...
Divergent Boundaries: Origin and Evolution of the
Divergent Boundaries: Origin and Evolution of the

... Why oceanic lithosphere subducts •Oceanic lithosphere subducts because its overall density is greater than the underlying mantle •Subduction of older, colder lithosphere results in descending angles of nearly 90º •Younger, warmer oceanic lithosphere is more buoyant and angles of descent are small • ...
Theory of plate tectonics - 8th Grade Social Studies
Theory of plate tectonics - 8th Grade Social Studies

... Further evidence existed in the discovery of glacial deposits in Africa and tropical plant fossils in Antarctica At the time, Wegener could not explain what force would be strong enough to move these land masses New discoveries and evidence lead to further develop Wegner’s theory into the developmen ...
Commentary for Nature Climate Change Global Ocean Summit: a
Commentary for Nature Climate Change Global Ocean Summit: a

... program has built a seamless global array of more than 3,500 free-drifting profiling floats, measuring the upper 2,000 meters of the ocean. This program, for the first time, allows continuous monitoring of ocean temperature, salinity and velocity concurrently and on a global scale, with all data rel ...
continental margin
continental margin

...  A mid-ocean ridge is found near the center of most ocean basins. It is an interconnected system of underwater mountains that have developed on newly formed ocean crust.  Seafloor Spreading • Seafloor spreading is the process by which plate tectonics produces new oceanic lithosphere at ocean ridge ...
Plate Tectonics Short Study Guide
Plate Tectonics Short Study Guide

... New seafloor moves away from the ridge, cools, and becomes more dense than the material beneath it. Hot magma which is less dense than surrounding material, is forced toward the crust. New ocean floor forms as the magma hardens. ...
Review Topics for Test I
Review Topics for Test I

... may exhibit foliation (alignment of minerals or apparent “layers” of minerals) due to stress on the parent rock Sedimentary: Formed from existing rock as solid rocks weather mechanically. Pieces are buried, compacted and cemented to form a new rock. Also formed from chemical weathering where mineral ...
Earth and Environmental Science Review with Answers
Earth and Environmental Science Review with Answers

... 81. How does a tornado form? How does it die? Large differences in air pressure cause winds to move quickly and can begin to rotate. They die when they lose their energy (pressure begins to equalize) 82. How does a hurricane form? How does it die? Low pressure systems pick up large amounts of moistu ...
Presentation
Presentation

... broke apart and eventually drifted to their present location.  This land mass was called Pangaea. ...
plate tectonics
plate tectonics

... After analyzing the rock samples, scientists came up with a theory that molten material from Earth’s mantle is forced upward to the surface at midocean ridges and cools to form new sea floor. Movement in Earth’s mantle forces sections of crust apart, allowing magma to flow onto Earth’s surface and f ...
plate tec article and ques from ed helper
plate tec article and ques from ed helper

... Abraham Ortelius noticed that it looked like America had been "torn away from Europe and Africa." Scientists thought that, at one time, all of the continents might have been just one huge continent. They called it a supercontinent and named it Pangaea. It may have existed around 225 million years ag ...
20 facts on ocean acidification
20 facts on ocean acidification

... ocean acidification research and understanding. The FAQs and this fact sheet are intended to aid scientists, science communicators, and science policy advisors asked to comment on details about ocean acidification. In all, 63 scientists from 47 institutions and 12 countries participated in writing t ...
20  FACTS T
20 FACTS T

... ocean acidification research and understanding. The FAQs and this fact sheet are intended to aid scientists, science communicators, and science policy advisors asked to comment on details about ocean acidification. In all, 63 scientists from 47 institutions and 12 countries participated in writing t ...
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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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