17.3 Plate Boundaries
... continental and oceanic crust moves as enormous slabs which geologists call tectonic plates Huge pieces of crust and rigid upper mantle that fit together at their edges to cover Earth’s surface Theory describes how plates move and shape Earth’s surface Attributes earthquakes, volcanoes, mounta ...
... continental and oceanic crust moves as enormous slabs which geologists call tectonic plates Huge pieces of crust and rigid upper mantle that fit together at their edges to cover Earth’s surface Theory describes how plates move and shape Earth’s surface Attributes earthquakes, volcanoes, mounta ...
Plate Tectonics Unit - Spring
... How were divergent boundaries discovered? In the 1960s, new technologies began to be used to study the ocean floor. What they were used to discover new features on the ocean floor This would eventually lead us to the discovery of seafloor spreading 1. Ocean floor topography was mapped using SO ...
... How were divergent boundaries discovered? In the 1960s, new technologies began to be used to study the ocean floor. What they were used to discover new features on the ocean floor This would eventually lead us to the discovery of seafloor spreading 1. Ocean floor topography was mapped using SO ...
lecture 01s - Kean University
... Third type of plate boundary Plates slide past one another and no new lithosphere is created or destroyed ...
... Third type of plate boundary Plates slide past one another and no new lithosphere is created or destroyed ...
U4-T2.6-Plate Boundaries
... Ocean-Continent collisions involve an oceanic plate and a continental plate. Compressional forces cause an ocean plate and a continent plate to move together, due to a greater density (basaltic vs. granitic), the oceanic plate will most likely subduct beneath the continent forming a trench and s ...
... Ocean-Continent collisions involve an oceanic plate and a continental plate. Compressional forces cause an ocean plate and a continent plate to move together, due to a greater density (basaltic vs. granitic), the oceanic plate will most likely subduct beneath the continent forming a trench and s ...
Plate Tectonics
... plate tectonics. According to this theory the earth is broken into irregularly shaped sections that move on a plastic like layer called the mantle. ...
... plate tectonics. According to this theory the earth is broken into irregularly shaped sections that move on a plastic like layer called the mantle. ...
AMERICAN METEOROLOGICAL SOCIETY EDUCATION
... In addition to possible collaboration through OCCEA, AMS would welcome a more formal partnership between the two educational networks in the areas of ocean and climate science. The AMS Education Program has 20 years of experience creating and sustaining networks of K-12 educators and college facult ...
... In addition to possible collaboration through OCCEA, AMS would welcome a more formal partnership between the two educational networks in the areas of ocean and climate science. The AMS Education Program has 20 years of experience creating and sustaining networks of K-12 educators and college facult ...
Layers of the Earth
... • Top layer - hot solid rock 1590 degrees Fahrenheit • Bottom layer - hot liquid rock 3992 degrees Fahrenheit • The Mantle’s density and temperature increase with it’s depth. ...
... • Top layer - hot solid rock 1590 degrees Fahrenheit • Bottom layer - hot liquid rock 3992 degrees Fahrenheit • The Mantle’s density and temperature increase with it’s depth. ...
17.3 Plate Boundaries The evidence of seafloor spreading
... Oceanic – oceanic this is when one oceanic plate, which is denser than the other, subducts beneath another oceanic plate. The subduction process creates an ocean trench. The subducted plate descends into the mantle where it will be recycled. During this subduction process, water is also being subduc ...
... Oceanic – oceanic this is when one oceanic plate, which is denser than the other, subducts beneath another oceanic plate. The subduction process creates an ocean trench. The subducted plate descends into the mantle where it will be recycled. During this subduction process, water is also being subduc ...
H: Chapter 5: Oceanography
... Continental Shelf Deposits A high amount of organic activity occurs in the waters above the continental shelf, and sediment accumulates to great thickness on the ocean floor. This is why many different kinds of resources can be found there, such as petroleum and natural gas deposits. Approximately 2 ...
... Continental Shelf Deposits A high amount of organic activity occurs in the waters above the continental shelf, and sediment accumulates to great thickness on the ocean floor. This is why many different kinds of resources can be found there, such as petroleum and natural gas deposits. Approximately 2 ...
Weathering and Erosion
... True or False: The Earth’s surface has stayed the same for thousands of years. Think about the statement in the box above. Do you think it is a true statement or a false statement? Circle True or False on. ...
... True or False: The Earth’s surface has stayed the same for thousands of years. Think about the statement in the box above. Do you think it is a true statement or a false statement? Circle True or False on. ...
Seafloor Spreading
... Earth has a magnetic field generated by the flow of molten iron in the outer core. This field is what causes a compass needle to point to the North. A magnetic reversal happens when the flow in the outer core changes, and Earth’s ...
... Earth has a magnetic field generated by the flow of molten iron in the outer core. This field is what causes a compass needle to point to the North. A magnetic reversal happens when the flow in the outer core changes, and Earth’s ...
L10
... Magma rises to surface and forms new oceanic crust. Occur in oceanic crust (oceanic ridges) and in continental crust (rift valleys). Continental rift valleys may eventually flood to form a new ocean basin. ...
... Magma rises to surface and forms new oceanic crust. Occur in oceanic crust (oceanic ridges) and in continental crust (rift valleys). Continental rift valleys may eventually flood to form a new ocean basin. ...
chapter 2 - Geophile.net
... 17. What keeps the Appalachians standing as a mountain range even though they have been continuously eroding since they formed hundreds of millions of years ago? a. They are actually becoming lower by the amount that material is eroded off the top. b. They are again being pushed up by collision betw ...
... 17. What keeps the Appalachians standing as a mountain range even though they have been continuously eroding since they formed hundreds of millions of years ago? a. They are actually becoming lower by the amount that material is eroded off the top. b. They are again being pushed up by collision betw ...
chapter 2 - Geophile.net
... 17. What keeps the Appalachians standing as a mountain range even though they have been continuously eroding since they formed hundreds of millions of years ago? a. They are actually becoming lower by the amount that material is eroded off the top. b. They are again being pushed up by collision betw ...
... 17. What keeps the Appalachians standing as a mountain range even though they have been continuously eroding since they formed hundreds of millions of years ago? a. They are actually becoming lower by the amount that material is eroded off the top. b. They are again being pushed up by collision betw ...
File
... 1. During the 1940s and 1950s, scientists began using ________________________ on moving ships to map large areas of the ocean floor in detail. 2. ________________________ echo off the ocean bottom – the longer the sound waves take to return to the ship, the deeper the water is. 3. Using ___________ ...
... 1. During the 1940s and 1950s, scientists began using ________________________ on moving ships to map large areas of the ocean floor in detail. 2. ________________________ echo off the ocean bottom – the longer the sound waves take to return to the ship, the deeper the water is. 3. Using ___________ ...
Chapter 19 - Mr. Goodenough
... Continental Shelf Deposits A high amount of organic activity occurs in the waters above the continental shelf, and sediment accumulates to great thickness on the ocean floor. This is why many different kinds of resources can be found there, such as petroleum and natural gas deposits. Approximately 2 ...
... Continental Shelf Deposits A high amount of organic activity occurs in the waters above the continental shelf, and sediment accumulates to great thickness on the ocean floor. This is why many different kinds of resources can be found there, such as petroleum and natural gas deposits. Approximately 2 ...
Technical Abstract of the First Global Integrated Marine Assessment
... biological diversity of areas beyond national jurisdiction. The purpose of this Technical Abstract is to provide scientific, factual background to the issues being discussed in these processes. In this regard, the Technical Abstract provides a synthesis of the information in World Ocean Assessment I ...
... biological diversity of areas beyond national jurisdiction. The purpose of this Technical Abstract is to provide scientific, factual background to the issues being discussed in these processes. In this regard, the Technical Abstract provides a synthesis of the information in World Ocean Assessment I ...
Most-Missed Questions
... Squid are considered meroplankton (opposite = holoplankton) “mero” – part “holo” - whole ...
... Squid are considered meroplankton (opposite = holoplankton) “mero” – part “holo” - whole ...
3rd Nine Weeks Study Guide Earth + Space 6.6B Calculate density
... core, outer core, mantle, crust, asthenosphere, and lithosphere ...
... core, outer core, mantle, crust, asthenosphere, and lithosphere ...
Census of Marine Life-Translation 9-13-10
... tracking network for animals, invented Autonomous Reef Monitoring Structures to standardize global assessment of reef life, and fostered acoustic systems to measure abundances over tens of thousands of square kilometers. Together, these technologies show that the incipient Global Ocean Observing Sys ...
... tracking network for animals, invented Autonomous Reef Monitoring Structures to standardize global assessment of reef life, and fostered acoustic systems to measure abundances over tens of thousands of square kilometers. Together, these technologies show that the incipient Global Ocean Observing Sys ...
Meaning and Effects 2014-2015 Mechanical or Physical Weathering
... Ans. Exfoliation- This is more common in arid regions. The peeling away of the surface layers of the rocks made up of homogeneous minerals ( same type of minerals) is called Exfoliation. In the arid regions the alternate heating & expansion of the surface layer in the day & cooling and contraction ...
... Ans. Exfoliation- This is more common in arid regions. The peeling away of the surface layers of the rocks made up of homogeneous minerals ( same type of minerals) is called Exfoliation. In the arid regions the alternate heating & expansion of the surface layer in the day & cooling and contraction ...
Marine Geophysics
... 2. This type of force can be thought of as created by the horizontal pressure gradient attributable to the cooling and thickening of the oceanic lithosphere, 3. and its magnitude can be determined by the regional bathymetry, which is largely a function of plate age. 4. The term “ridge push” is misle ...
... 2. This type of force can be thought of as created by the horizontal pressure gradient attributable to the cooling and thickening of the oceanic lithosphere, 3. and its magnitude can be determined by the regional bathymetry, which is largely a function of plate age. 4. The term “ridge push” is misle ...
Plate Tectonics PowerPoint
... 3. Ocean-Ocean Collision • When two oceanic plates collide, one runs over the other causing it to sink into the mantle forming a subduction zone. • The subducting plate is bent downward to form a very deep depression in the ocean floor called a deep-sea trench. • The deepest parts of the ocean are ...
... 3. Ocean-Ocean Collision • When two oceanic plates collide, one runs over the other causing it to sink into the mantle forming a subduction zone. • The subducting plate is bent downward to form a very deep depression in the ocean floor called a deep-sea trench. • The deepest parts of the ocean are ...
chapter 15A - plate tectonics 1
... ridges) that circle the globe, often parallel to continental boundaries – dredging of sea floor sediment and rocks indicated the age of the oldest ocean crust was much younger than that of continental crust. – Recurring patterns of earthquakes and volcanoes in places such as the Circum-Pacific Belt ...
... ridges) that circle the globe, often parallel to continental boundaries – dredging of sea floor sediment and rocks indicated the age of the oldest ocean crust was much younger than that of continental crust. – Recurring patterns of earthquakes and volcanoes in places such as the Circum-Pacific Belt ...
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.