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Seafloor Spreading
Seafloor Spreading

... Seafloor Spreading “The Crust’s Giant Conveyor Belt” ...
Picture Review Name
Picture Review Name

... Solid iron and nickel Liquid iron and nickel/ molten iron nickel Thicker Upper Right angle or 90 degrees Straight angle or 180 degrees Moon, because it is closer to earth ...
updated 01/10/00 - Oregon State University Remote Sensing Ocean
updated 01/10/00 - Oregon State University Remote Sensing Ocean

... in boreal through sub-tropical (and even tropical) oceanic ecosystems also reflect organismal adaptations to light, temperature, turbulence and nutrients. In contrast, little is known about natural cell and integrated population responses to high frequency (seconds- minutes) variability in nutrient ...
Geological Changes - Woodside Australian Science Project
Geological Changes - Woodside Australian Science Project

... The Australian Plate is presently moving northwards towards South China at roughly the same speed as your fingernails grow. In about 250 million years it will have crashed into Borneo pushing up even more mountains as it ploughs north. Variation of rock types within the Australian plate and friction ...
Coastal Ocean Observing Systems SEACOOS Facilitating Marine
Coastal Ocean Observing Systems SEACOOS Facilitating Marine

... Southeast Coastal Ocean-the domain extending from the Florida Panhandle to the North Carolina shelf north of Cape Hatteras (Fig. 1). Poised between distinct, yet interacting coastal ocean systems, Florida exemplifies the need for integrated, multi-disciplinary information to manage its resources. Fl ...
Paleooceanography and Sea
Paleooceanography and Sea

... • Ocean bathymetry changes significantly only on time scales of 106-107 years – The geoid is the hypothetical surface of the Earth that coincides everywhere with mean sea level and is perpendicular, at every point, to the direction of gravity. • The geoid is used as a reference surface for astronomi ...
Effects of surface current–wind interaction in an
Effects of surface current–wind interaction in an

... dency of the drag coefficient on (a) wind speed (e.g. Smith and Banke, 1975), (b) atmospheric stability (e.g. Hsu, 1974), and (c) wind–wave interaction (e.g. Hsu, 1973). Even so, the transfer of momentum from the atmosphere to the ocean is still associated with considerable uncertainties. For exampl ...
The Indian-Atlantic Ocean gateway during the Pliocene: current
The Indian-Atlantic Ocean gateway during the Pliocene: current

... 361 – Southern African Climates and Agulhas LGM Density Profile by Gruetzner et al., this Volume). Our new research proposal focuses on three of these sites forming a latitudinal transect in the Atlantic-/Indian Ocean gateway and combines chemical, physical property and seismic methods. Primary site ...
Continental Drift - North Mac Schools
Continental Drift - North Mac Schools

... Hess proposed a hypothesis... Mid-Atlantic Ridge valley is a rift in the Earth’s crust where magma from the mantle comes through. He reasoned the ocean floor was moving away from both sides of the ridge, being replaced by rising magma. ...
What are Earth`s Systems
What are Earth`s Systems

...  Vapor. This form of water has no shape or cohesion. It is created when water molecules are heated to such a fast and furious movement that the bonds linking them together break apart. Climate models predict that warmer temperatures will cause increased evaporation of water into the air.  Liquid. ...
What are Earthquakes?
What are Earthquakes?

... • Make the ground roll like ocean waves • Responsible for surface damage and falling buildings. ...
Introduction to Plate Tectonics via Google Earth
Introduction to Plate Tectonics via Google Earth

... Topography of the continents and bathymetry of the sea floor Uncheck all of the layers and focus on the topography of the earth. We are all relatively familiar with the topography of the Earth’s surface above sea level, but less so with the bathymetry of the Earth below sea level. Before this was kn ...
Introduction to Plate Tectonics via Google Earth
Introduction to Plate Tectonics via Google Earth

... Topography of the continents and bathymetry of the sea floor Uncheck all of the layers and focus on the topography of the earth. We are all relatively familiar with the topography of the Earth’s surface above sea level, but less so with the bathymetry of the Earth below sea level. Before this was kn ...
Seismic Waves
Seismic Waves

... waves which are vibrations caused by earthquakes. Seismic waves from even small earthquakes can be recorded by sensitive instruments around the world. ...
Notes Earthquakes
Notes Earthquakes

... to the nature of the resulting groundshaking. The ground moves laterally, or shimmies side-to-side with no vertical component. These are the most damaging type of waves. They can literally move the ground beneath a building faster than the building itself can respond, effectively shearing the base o ...
The Earth's Global Energy Balance
The Earth's Global Energy Balance

... of both hemisphere. The region where the cold polar winds and the warmer westerly flow of the midlatitudes clash has been named the polar front. ...
MISSION TO EUROPA – LANDER AND ORBITER CAPABILITIES
MISSION TO EUROPA – LANDER AND ORBITER CAPABILITIES

... hardware will also permit detection of carbon compounds including methane. Sample handling would significantly differ from the Martian case in that icy material would be the likely medium added to the inlet tubes, rather than soil. An abrasion or shallow drilling tool rather than scoop may be needed ...
Notes: Plate Tectonics
Notes: Plate Tectonics

... toward each other, there are three types: 1.) subduction zone- dense ocean plate sinks under light continental plate ex: deep sea trench, volcanic mountain chains 2.) two ocean plates collide ex: deep sea trench, volcanic island chain 3.) two continental plates collide ex: mountains, earthquakes com ...
19.1 Earthquakes
19.1 Earthquakes

... which it is stretched 2) Secondary Waves: (S-waves) similar to holding a jump rope in one hand and raising and lowering it 3) Surface Waves (Love and Rayleigh): the most destructive, cause the ground to move sideways and up and down like an ocean wave Because they happen INSIDE the earth, P-waves an ...
1. The hotspot‐melting‐through‐lithosphere process forms lines of
1. The hotspot‐melting‐through‐lithosphere process forms lines of

... 8. Linear, magnetic patterns associated with mid‐ocean ridges are configured as ________.       a. normal and reversed magnetized strips roughly perpendicular to the ridge axis  b. normal and reversed magnetized strips roughly parallel to the ridge  c. concentric circles about a rising plume of hot  ...
19.1 Earthquakes
19.1 Earthquakes

... which it is stretched 2) Secondary Waves: (S-waves) similar to holding a jump rope in one hand and raising and lowering it 3) Surface Waves (Love and Rayleigh): the most destructive, cause the ground to move sideways and up and down like an ocean wave Because they happen INSIDE the earth, P-waves an ...
Chapter 14, Section 1
Chapter 14, Section 1

... surface and makes life possible.  The water on earth is continuously circulated between the atmosphere, the oceans, and the earth.  The ocean floor and the continents have similar landforms. ...
Subduction Zones
Subduction Zones

... 60,000 km. They are areas of recently formed ocean crust, and have reasonable levels of shallow seismicity. ...
Document
Document

... – Vibrations cause ground water to rise and turn solid ground into liquid – Structures may sink into the ground ...
Plate Tectonics and Climate— Episodes of Extensive Glaciation and
Plate Tectonics and Climate— Episodes of Extensive Glaciation and

... outgassing of carbon dioxide from volcanoes. On long time scales, carbon dioxide production is balanced by consumption during weathering of igneous and metamorphic rocks. To maintain the atmospheric carbon dioxide concentration, the amount of carbon dioxide consumed by silicate weathering would also ...
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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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