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Plate Boundaries-new
Plate Boundaries-new

... Presentation Objectives: § Define the theory of plate tectonics. § Explain how the Earth is divided into layers based on chemical and physical properties. § Define the asthenosphere and lithosphere. § Describe the plate motion at each of the three different plate boundaries. § Describe the feat ...
Laboratory Studies of Mantle Convection with continents and other
Laboratory Studies of Mantle Convection with continents and other

... fingering structures that result when flows alter their surroundings to retard their continuation. This is typical as hot material from deep in the earth rises to shallow regions where cooling is encountered. We then described recent work concerning the relation between convection cells and material ...
NTI Day 1 Article
NTI Day 1 Article

... the site of earthquakes and volcanoes. Oceanic crust created by seafloor spreading in the East Pacific Rise, for instance, may become part of the Ring of Fire, the horseshoe-shaped pattern of volcanoes and earthquake zones around the Pacific ocean basin. In other cases, oceanic crust encounters a pa ...
Crust
Crust

... The Earth's Crust is like the skin of an apple. It is very thin in comparison to the other three layers. The crust is only about 3-5 miles (10 kilometers) thick under the oceans (oceanic crust) and about 25 miles (30 kilometers) thick under the continents (continental crust). The average temperature ...
Learning Targets Answer Key
Learning Targets Answer Key

... 1. Illustrate and label the layers of the earth including the crust, mantle, outer core and inner core. Crust – Thin solid outer layer of the Earth; includes the lithosphere. Mantle – Thickest layer of the Earth made of semi-solid soft rock; includes the asthenosphere & mesoshpere Outer Core – Liqui ...
Divergent Plate Boundaries
Divergent Plate Boundaries

... Plates slide past one another Fault zones, earthquakes mark boundary San Andreas fault in California ...
The 2011 off the Pacific coast of Tohoku Earthquake related... a strong velocity gradient with the Pacific plate
The 2011 off the Pacific coast of Tohoku Earthquake related... a strong velocity gradient with the Pacific plate

... Figure 3 shows the map view of V P perturbation within the Pacific plate 10 km beneath the boundary. In the inland area, large earthquakes occurred around the region whose lower crust has low-V , suggesting a role of magma and fluid (Zhao et al., 2010). Then we investigate the velocity structure wit ...
3D Imaging of the Earth`s Lithosphere Using Noise from Ocean Waves
3D Imaging of the Earth`s Lithosphere Using Noise from Ocean Waves

... surface wave tomography from its dependence on earthquakes. ANT, in effect, becomes a controlled-source technique; that is, the path coverage in ANT is controlled by desired configurations of seismic stations. To date, most ANT studies focus on surface waves at periods shorter than 40/50 s because a ...
Lab 8A: Investigating Tectonic Plate Boundaries Using Online
Lab 8A: Investigating Tectonic Plate Boundaries Using Online

... 12. Stratovolcanoes (sometimes called composite) are towering volcanoes you see in Hollywood movies. These are built from mainly intermediate composition magmas which result from the subduction (or sinking) of an oceanic tectonic plate beneath a less dense continental plate. These volcanoes are key ...
Earth Science and M.E.A.P
Earth Science and M.E.A.P

... seafloor is formed when magma is forced upward toward the surface at a mid-ocean ridge. ...
FALL 2014
FALL 2014

... The Southern Ocean is the primary gateway through which the intermediate, deep, and bottom waters of the ocean interact with the sea surface and thus the atmosphere (Fig. 1). As a result, the Southern Ocean lends a considerable hand in keeping Earth’s temperature hospitable by soaking up a quarter o ...
Earthquakes and Plate Boundaries
Earthquakes and Plate Boundaries

... S-waves move rock particles up and down, or side-to-side--perpendicular to the direction that the wave is traveling in. An S-wave can be up to 50% slower than a P-wave depending on the rock it is going through. They can only move through solid rock, but not through any liquid medium which includes o ...
ppt
ppt

... influence, 15º20’ - 18º30N, East Pacific Rise: Influence of axial faulting. Geochemistry Geophysics Geosystems. Volume 2. September 2004. AGU and the Geochemical Society. ...
occurrence of the ocean and its evolution toward an
occurrence of the ocean and its evolution toward an

... an island arc volcanism associated with base metal mineralizations and the deposition of arc sedimentary formations. In some special conditions a regional metamorphism and rarely a load metamorphism could manifest themselves. The subduction process is of two types: the Andeantype and the Mariana-typ ...
Density Difference between Subducted Oceanic Crust - SPring-8
Density Difference between Subducted Oceanic Crust - SPring-8

... Since the beginning of plate tectonics, the oceanic lithosphere has been continually subducted into the Earth’s deep mantle for 4.5 Gy. The oceanic lithosphere consists of an upper basaltic layer (oceanic crust) and a lower olivine-rich peridotitic layer. The total amount of subducted oceanic crust ...
Isostasy chap 9 LECT..
Isostasy chap 9 LECT..

... The mountains, I think, are to be explained chiefly as due to thermal expansion of material at depth, whereby the rock layers near the surface are lifted up. The uplifting does not mean the inflow or addition of material at depth, the void within the mountain compensates for the overlying mass (Bosc ...
06 Intrusions
06 Intrusions

... A Cooperative Quiz • True (A) or false (B): Igneous intrusions range in scale from a few cm3 to thousands of km3 ...
File - Leaving Certificate Geography
File - Leaving Certificate Geography

...  The subducting plate is bent downward to form a very deep depression in the ocean floor called a trench.  The worlds deepest parts of the ocean are found along trenches. • E.g. The Mariana Trench is 11 km deep! ...
one ocean final.indd
one ocean final.indd

... turbulent beginnings and its successive incarnations. It’s a journey that introduces the enormity of the ocean over space and time—at four billion years old the ocean is nearly as old as the planet itself. In a remote part of Western Australia, we venture to the stunning, crystal blue waters that ha ...
What Is a Volcano?
What Is a Volcano?

... materials in Earth’s crust Silica content of magma ranges from about 50% to 70% The more silica magma contains the higher its viscosity; ex. Rhyolite The less silica magma contains the lower its viscosity; ex. Basalt ...
Geology 3015 Lecture Notes Week 10
Geology 3015 Lecture Notes Week 10

... • Although coastal and submarine landslides, seafloor faulting, and volcanic explosions cause waves, wind-generated waves have greatest overall influence on shorelines. • Wind velocity and duration are important controls on the size of waves. Fetch, the distance the wind blows over open water, also ...
Explicitly resolved vs parameterized mesoscale processes
Explicitly resolved vs parameterized mesoscale processes

... • Winter mean MLD map in FER (Fig. 3.) shows MLD greater than 2000m (yellow contour) occuping the central Figure 3: (left panel) Winter mean MLD in FER, blue contours for isobaths 1500m, 2500 and Labrador Sea and extending in Irminger Sea; south of 55°N the MLD is reduced due to the presence of the ...
iprc climate vol5 no1
iprc climate vol5 no1

... The alternating jets on these giant planets are thought to result from the evolution of quasi two-dimensional turbulence, in which the turbulent energy cascades from smaller to larger eddies, which are eventually halted in their meridional expansion by the fact that the vertical component of the pla ...
Plate_tectonics_2 - Red Hook Central Schools
Plate_tectonics_2 - Red Hook Central Schools

... Name this plate boundary Match the labels to the letters F E ...
Goal 2 - The learner will demonstrate an
Goal 2 - The learner will demonstrate an

... e. identify living and non living resources from the ocean. f. identify the properties of ocean water. g. explain the significance of upwelling. h. describe the interactions between humans and the ocean. i. identify characteristics of marine ecosystems. j. research ocean life and report on findings. ...
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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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