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The Layers of the Earth
The Layers of the Earth

... different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball smaller than a marble if you wer ...
Crust - www .alexandria .k12 .mn .us
Crust - www .alexandria .k12 .mn .us

... different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball smaller than a marble if you wer ...
Crust - MentorMob
Crust - MentorMob

... different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball smaller than a marble if you wer ...
Earth’s Interior PowerPoint - Marcia's Science Teaching
Earth’s Interior PowerPoint - Marcia's Science Teaching

... different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball smaller than a marble if you wer ...
Structure of the Earth
Structure of the Earth

... –  Very rich in Mg-Fe (very dense) –  Extends from base of crust (Moho) to the top of the core ...
The Gaian Theory Essay Research Paper IntroductionContinental
The Gaian Theory Essay Research Paper IntroductionContinental

... oceanic crust sufficiently to cause subduction. This seems rather unlikely, however, and unless more evidence is gathered supporting this hypothesis, it will probably never be taken seriously.(Stolz,39) The presence of water in the liquid state is also vital to plate tectonics as well as life. Water ...
Plate Tectonics * Lab
Plate Tectonics * Lab

... The transform boundary is represented by areas where two plates are grinding or sliding past one another. In the area of the grinding or fracture zone, faults typically occur and are known as transform faults. Most transform faults are located on the ocean floor where they primarily offset spreading ...
Plate Tectonics – Lab
Plate Tectonics – Lab

... The transform boundary is represented by areas where two plates are grinding or sliding past one another. In the area of the grinding or fracture zone, faults typically occur and are known as transform faults. Most transform faults are located on the ocean floor where they primarily offset spreading ...
Ocean Currents and Their Impact on Marine Life
Ocean Currents and Their Impact on Marine Life

... larger than the average calculated for the open ocean. This difference is indicative of the very strong impact that upwelling systems exert on marine life in their area of influence. However, their contribution to global marine productivity is limited to only 5% of the total because upwelling areas ...
oceanic crust - Duluth High School
oceanic crust - Duluth High School

... weight. The movement of the middle mantle (asthenosphere) is the reason that the crustal plates of the Earth move. ...
File
File

... one ocean plate pushed under the other, back into the mantle where it melts; this process (subduction) takes place at a subduction zone which creates a deep-sea trench; can also create a volcanic island arc Describe fully all the characteristics of an oceanic-continental convergent boundary. ocean p ...
fact finding answers
fact finding answers

... ...
No Slide Title
No Slide Title

... • The Earth’s surface is continually battered by wind and scoured by running water, which moves rocks around and changes their appearance. • Erosion is the process in which the materials of the Earth’s surface are loosened, dissolved, or worn away and transported form one place to another by a natur ...
GSA_2012 - Geological Society of America
GSA_2012 - Geological Society of America

... These protists reside endosymbiotically within the cells of the coral polyps, where they take in sunlight and share the products of photosynthesis with the coral. In return, the protists get nutrients and a place to live. And this is only possible in areas with shallow, clear water and where sunligh ...
Interocean Exchange of Thermocline Water - Lamont
Interocean Exchange of Thermocline Water - Lamont

... NADW formation. The path of the return flow of warm water is as follows: Pacific to Indian flow within the Indonesian Seas, advection across the Indian Ocean in the 10ø-15øS latitude belt, southward transfer in the Mozambique Channel, entry into the South Atlantic by a branch of the Agulhas Current ...
9693 AS Marine Science
9693 AS Marine Science

... (a) Explain the meaning of the terms ecosystem, habitat, population, community, species, biodiversity, ecological niche. The term ecosystem refers to living organisms and the physical and chemical factors which influence them. In other words, it includes both biotic and abiotic components. A rocky s ...
ALABAMA COURSE OF STUDY SIXTH GRADE SCIENCE
ALABAMA COURSE OF STUDY SIXTH GRADE SCIENCE

... would release 100 times the energy of the earthquake of 5. ...
Full Text
Full Text

... marine “dead zones”... for better or worse, the Anthropocene is certainly proving to be an interesting time for marine science, and particularly for marine geochemistry. Add to this the advent of vast and vastly accessible information, as well as technological advances in analytics and computing, an ...
- Frost Middle School
- Frost Middle School

... • There is more pressure than the mantle but less pressure than the inner core ...
Light: The Cosmic Messenger
Light: The Cosmic Messenger

... high-density material to center • Lower-density material rises to surface • Material ends up separated by density ...
Sea Floor Spreading, Thomas
Sea Floor Spreading, Thomas

... magnetic field when the rocks were formed. The polarity of the rocks at the ridge have the same polarity as the Earth does today. What effect do you think sea-floor spreading has on the size of the ocean floor? It causes it to expand because it produces more crust. Where does all of this crust go? D ...
Chapter 13 Next Generation Sunshine State Standards
Chapter 13 Next Generation Sunshine State Standards

... largest single geographic feature on the planet, accounts for over half of the ocean surface area on Earth. In fact, the Pacific Ocean is so large that all of the continents could fit into the space occupied by it—with room left over! It is also the world’s deepest ocean, with an average depth of 3, ...
GEOLOGIC HAZARDS PART 1
GEOLOGIC HAZARDS PART 1

... increases.    The  wave  period  (the  time  necessary  for  successive  waves  to  pass  a  given  point)  and  the  total   energy  of  the  wave,  however,  remains  constant.    In  the  deep  water  of  the  open  ocean  the ...
8.1 Earth has several layers
8.1 Earth has several layers

... (land and land) • continental-continental collision—occurs where two plates carrying continental crust push together • Because both crusts are the same density, neither plate can sink beneath the other • Their edges crumple and fold • Sometimes the folds can be pushed up and form mountains http://em ...
Fundamental discoveries about the growth and recycling of continents
Fundamental discoveries about the growth and recycling of continents

... Rica, Guatemala, Mexico, Alaska, and the Aleutians. Data from these sectors of the Pacific rim imply that, globally, the longterm (> 5-10 my) rate at which sediment is globally subducted to mantle depths is conservatively estimated at 0.7 km3/yr (solid-volume). Upper plate material loss by subductio ...
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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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