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Plate Tectonics
Plate Tectonics

... 3. As molten rock rises from the rift in an MOR, it quickly cools and hardens and its ...
Informal Ministerial Meeting on Blue Growth and Ocean Governance
Informal Ministerial Meeting on Blue Growth and Ocean Governance

... joint agenda for the future of our oceans. Aim The aim of the meeting is to discuss the various aspects and the future direction of the Blue Growth Initiative and the development of the implementation of ocean governance in the EU and the Mediterranean. The meeting will also revolve around the impor ...
Physical properties of the atmosphere: Pressure
Physical properties of the atmosphere: Pressure

... which will lead to sinking air A column of warm, less dense air causes low pressure at the surface, which will lead to rising air ...
Continental Drift and Plate Tectonics Part 1 Multiple Choice
Continental Drift and Plate Tectonics Part 1 Multiple Choice

... ____ 10. Crust is neither destroyed nor formed along which of the following boundaries? a. convergent c. transform b. divergent d. magnetic ____ 11. The driving forces of tectonic plates are related to convection currents in Earth’s ____. a. crust c. inner core b. mantle d. outer core ____ 12. A vas ...
Tidal
Tidal

... • Nearly 75% of the surface area of Earth is water. Due to the high heat capacity of water, the, water near the surface is maintained at significant higher temperatures than water at greater depth • It is possible to extract energy from the oceans through the use of heat engines in order to exploit ...
Chapter 6 – Plate Tectonics and Earthquakes
Chapter 6 – Plate Tectonics and Earthquakes

... 2. The Pacific is the largest plate, covering one-fifth of Earth’s surface. ...


... CO2 through specialized openings in their leaves (stomata) • Vertebrates – exchange CO2 for O2 through gills. ...
Class2atxt
Class2atxt

... Volcanism • Pressure on molten rock • Composite volcanoes – Violent and explosive – Along subduction zones – Relatively hard to predict ...
Topography of the Ocean Floor Notes
Topography of the Ocean Floor Notes

... • Underwater mountains, usually volcanic. • The biggest mtn. on earth is Mauna Loa (Hawaii). • Build-up underwater (over a hot spot), & when they break the ocean surface they turn into islands. • Start to “deflate” & sink as the crust carries it away from the hot spot. ...
Unit Six Notes
Unit Six Notes

...  The plates may move in opposite directions or in the same directions but at different rates and frequent earthquakes are created (example: San Andreas ...
Earth`s Structure
Earth`s Structure

... Mesosphere: strong, lower part of mantle Outer Core: liquid Inner Core: solid; both parts iron with some nickel ...
Warm- Up
Warm- Up

... the rock formed will be in another direction Flipping of poles is not dangerous Occurs 3-4 times per million years ...
3.20Ocean Pollution
3.20Ocean Pollution

... • For example, one common high-level waste that is produced by spent nuclear fuel has a half-life of 24,100 years! • It has been suggested that contained nuclear waste should be disposed in the deep sea. So little is known about the deep sea environment or the consequences of containment leakage and ...
Slide 1
Slide 1

... Earth has a layered structure. ...
Plate Tectonics - dhsearthandspacescience
Plate Tectonics - dhsearthandspacescience

... What drives the movement of plates? • The movement of plates is driven by convection currents within the Earth ...
8th Grade Science Final - Union Beach School District
8th Grade Science Final - Union Beach School District

... islands are formed  Oceanic-Continental – the oceanic plate is denser so it slides under the continental plate – deep ocean trenches and coastal volcanic mountains are formed  Continental-Continental- continental crust pushes together and mountains are formed ...
Deformation of the Crust
Deformation of the Crust

... • Small fault – only in small area and through few layers of rock • Large fault system – large area, several layers of rock • San Andreas Fault ...
Quaternary paleo-oceanography from the geochemistry of sediment
Quaternary paleo-oceanography from the geochemistry of sediment

... circulation of the oceans as it interfaces with a major confluence of ocean currents. The warm, Agulhas Current flows along the eastern continental margin leaking flow (“rings”) into the South Atlantic as it retroflects back into the southern Indian Ocean. The cold, Benguela Current flows along the ...
Physical and Ecological Processes
Physical and Ecological Processes

... Tsunamis are giant waves caused by earthquakes or volcanic explosions. Tsunamis can be detected with an early warning system but not all countries have the money to install them. ...
Earth`s Magnetic Field
Earth`s Magnetic Field

... Africa and South America are gradually approaching each other. __________ 2. Most geologists believe that continents are larger now than they were in the past. __________ 3. The size of the earth is gradually increasing over time because of seafloor spreading. __________ 4. Tectonic plates drift in ...
Chapter 2: The Earth`s Mobile Crust Continental Drift
Chapter 2: The Earth`s Mobile Crust Continental Drift

... change in speed of P & S waves ...
Plate Tectonic Test Use the pictures above to answer questions 1
Plate Tectonic Test Use the pictures above to answer questions 1

... ____ 20. One reason that melted material from the Earth’s mantle is rising up at location  is because it isa. cooler than the surrounding material b. older than the surrounding material c. Less dense than the surrounding material ____ 21. The newest rocks are most likely found at a. Location c. L ...
Kump_Ch07_TH - Camosun College
Kump_Ch07_TH - Camosun College

... Glossopteris – giant seed ferns + Mesosaurus ~ croc • Geological ties: belts of correlative Precambrian through Paleozoic geology: plutons, sediment basins • Fit of Continents – especially at 2000 m isobath • Paleomagnetism, inclinations, apparent polar wander • Now recognized to be caused by seaflo ...
Chapter 2
Chapter 2

... that has been heated by the mantle forces its way through the ...
Ch 5 Notes
Ch 5 Notes

... i. They vary greatly in size, composition, temperature, and pressure b. Temperature i. As we begin to tunnel to the center, we go through cool rock ii. At about 20 meters down the rock is getting warmer iii. For every 40 meters from that point, the temperature increases 1°C iv. After several tens of ...
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Physical oceanography



Physical oceanography is the study of physical conditions and physical processes within the ocean, especially the motions and physical properties of ocean waters.Physical oceanography is one of several sub-domains into which oceanography is divided. Others include biological, chemical and geological oceanographies.
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