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File

... amount of “carbon fixation”, but absence of dissolved nutrients (N and P) in the clear, tropical water. It has plenty of sunlight and it’s temperature and salinity levels are stable because corals will die if the temperature increases or decreases beyond their strict ...
Earthquakes - Leon County Schools
Earthquakes - Leon County Schools

... Liz LaRosa http://www.middleschoolscience.com 2009 ...
power point notes
power point notes

... The movement of crustal plates results from convection currents in the Mantle. Heat from the formation of the Earth and radioactive decay escapes at the Earth’s surface. ...
Exam Review with Answers
Exam Review with Answers

... a. Deforestation- The removal of large areas of forest for human purpose. b. Desertification- The development of desert-like conditions due to human activities, and/or climate change. c. Overgrazing- Allow animals (such as cows, horses, and goats) to eat so heavily that the vegetation is damaged and ...
Version A - Partners4results
Version A - Partners4results

... D. folding of the sedimentary layers ...
2nd_nine_weeks_exam_review_answers
2nd_nine_weeks_exam_review_answers

... 18. Give an example of a divergent plate boundary involving two continental plates. Great Rift Valley of Africa 19. Plates that move towards one another are called? convergent plate boundary 20. What is a subduction zone? A more dense oceanic plate is forced under a less dense continental plate 21. ...
The Geological Record of Ocean Acidification
The Geological Record of Ocean Acidification

... indicated in blue. Anthropogenic perturbations are marked in italics. Approximate fluxes are printed in parentheses (PgC year−1), whereas reservoir inventory values are shown in brackets [PgC]. Natural carbon cycle fluxes are from (70); anthropogenic fluxes for 2008 are from (57), which for the land ...
Chapter 5
Chapter 5

... quality of the data. Most wave survey legs will be longer than 300km to observe gravity waves with long wavelengths. Most wave surveys will be flow in a direction close to the wind vector. For example, if the wind direction is westerly at 270T, the tracks will be flown at 270T and 090T. If the wind ...
marine technology
marine technology

... the port and facilities have expanded for increased shipping and business. This expansion has seen a renewed focus on the interplay between the port’s operational, maritime and natural environments. For example, a large tidal range of almost 8 m drives strong and complex currents, having speeds to 2 ...
Chapter 16: Marine and Costal Systems
Chapter 16: Marine and Costal Systems

... targeted now because of the lack of the commonly fished in the past to prevent this, consumers can chose which product to buy according to fishing practices ...
Jon D - Laconia School District
Jon D - Laconia School District

... • The thirteen major plates are all part of the lithosphere. They float on the mantle and move at extremely slow rates. They move from convection. Convection is when something is hot it rises and then when it cools it will sink. When the mantle is moving from convection it pulls the lithosphere wit ...
Cracking Up
Cracking Up

... fissures, or narrow cracks, that opened during a series of earthquakes in Ethiopia several years ago. The event wasn’t just any earthquake. It was one step in a geological process that is slowly building a new ocean in eastern Africa. ...
Slide 1
Slide 1

... body waves from a particular earthquake can be detected. B. Waves bend and change directions as they pass through Earth C. They exist because the materials that make up ...
pices xv - North Pacific Marine Science Organization
pices xv - North Pacific Marine Science Organization

... An intensive phytoplankton bloom forms every spring in the Oyashio region of the western subarctic Pacific Ocean. This bloom is dominated by coastal diatom species, most of which are known to form resting spores. Resting spores have been recognized as a resting survival stage under unfavorable condi ...
Plate Tectonics
Plate Tectonics

...  Subduction is the process by which old oceanic crust is pushed back down into the mantle melting rock and turning it back into molten material.  Subduction takes place at deep ocean trenches where convection currents are causing two lithospheric plates to move/push together. ...
Heat Flow (التدفق الحراري) عند وضع جسمين عند درجات حرارة مختلفة
Heat Flow (التدفق الحراري) عند وضع جسمين عند درجات حرارة مختلفة

... whereby hot material upwells at spreading centers and then cools. Because the strength of rock decreases with temperature, the cooling material forms the strong plates of the lithosphere. The cooling oceanic lithosphere moves away from the ridges, and eventually reaches subduction zones where it des ...
AICE Environmental Management GIZMOS Class Code
AICE Environmental Management GIZMOS Class Code

... An earthquake is a vibration of the ground. Some earthquakes are associated with volcanic eruptions, but most earthquakes are caused by motion along fractures called faults. Faults occur along plate boundaries. As the plates slowly move over, under, or past one another, stress builds up where the ro ...
Convection Currents and the Mantle
Convection Currents and the Mantle

... During convection heated particles of fluid begin to flow, transferring heat energy from one part of the fluid to another. ...
File - Things of the World
File - Things of the World

... The Pacific and Atlantic subtropical high: These are semi-permanent high pressure systems caused by descending sectors of the equatorial Hadley cells. The air masses are relatively warm and dry, and move in an anticyclonic circulation pattern over the sub-tropical oceans. The Pacific High is general ...
Plate Tectonics
Plate Tectonics

... have found that in the curve of islands, the largest and least eroded of the islands is at one end of the string, and contains active volcanoes. At the other end, is a small, eroded island, time-dated to be much older than the currently volcanic island. Also, on all the islands is increasingly older ...
Key Action 3: Sustainable Marine Ecosystems
Key Action 3: Sustainable Marine Ecosystems

... Main MAST III (FP4) projects with relevance to the new FP5, EESD KA3 topics. Important note: the projects below were not aimed specifically to nor funded under the headings of FP5. Therefore their association to those headings is only orientative and has no official character. For a search of the pr ...
Earthquakes and Damages Name
Earthquakes and Damages Name

... ____ 37. To determine how far away from a seismograph station an earthquake occurred, scientists plot the difference in arrival times between... A. P and S waves B. seismic waves and tsunamis ____ 38. The concept that Earth's upper layer, or lithosphere, is divided into large, quite rigid segments w ...
Earthquakes The theory of plate tectonics states that Earth`s crust is
Earthquakes The theory of plate tectonics states that Earth`s crust is

... waves are very damaging to buildings, also. 4. R Waves. R (or Rayleigh) waves are transverse waves which move on the surface of the Earth. R waves have the same type of motion as water waves, the particles of the Earth move in circular orbits as the wave passes. R waves are slower than S waves, but ...
Essay Question Outline
Essay Question Outline

... • Started: All land was joined into 1 supercontinent called “Pangaea: • Over Time: Continents drifted apart creating Gondwanaland and Laurasia, then Laurasia broke apart into North America, Europe and Asia. Then Gondwanaland broke into Africa, South America, Antarctica and Australia. ...
8. Earth`s Moving Plates
8. Earth`s Moving Plates

... Cracks in the Earth's Crust The solid crust acts as a heat insulator for the hot interior of the earth. Below the crust, in the mantle, is the molten material called magma. Tremendous heat and pressure within the earth cause the hot magma to flow in convection currents. Periodically it rises to the ...
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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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