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Unit 2 Test
Unit 2 Test

... Smoothest part of the ocean The ocean that is getting wider What oceanic crust is made of How oceanic crust compares to continental crust Theory that continents were once joined together & broke apart Submerged part of the continent Feature at the base of a continent composed of sediments eroded fro ...
The Structure and Origin of the Ocean Basins The water Planet
The Structure and Origin of the Ocean Basins The water Planet

... the atmosphere for millions of years. This is because the earth was too hot to allow the vapor to condense to form liquid water. Eventually, the earth cooled enough for water vapor to condense into clouds in the upper cooler atmosphere. Hot rain fell, however, since the earth's surface was so hot, t ...
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 Fault) ...
Chapter One
Chapter One

... Sonar – used to map seafloor depths and formations. Scuba – used for direct human exploration of oceanic environment for longer periods and at deeper depths than would otherwise be available to man. Remotely operated vehicles (ROV’s) – allows for direct exploration of marine environment when scuba i ...
Enhanced convection was evident across parts of Southeast Asia, South... south of Hawaii. Wetter-than-average conditions did not materilaize as expected...
Enhanced convection was evident across parts of Southeast Asia, South... south of Hawaii. Wetter-than-average conditions did not materilaize as expected...

... south of Hawaii. Wetter-than-average conditions did not materilaize as expected across parts of the western Pacific. Suppressed convection developed over parts of the Indian Ocean. The MJO showed signs of weakening during the past week as several observational indicators became considerably less coh ...
Internal Structure of the Earth
Internal Structure of the Earth

... • The material is similar to Jello—not quite a solid, but not a liquid either • The elasticity of the substance allows the plates to move around the planet • The mantle is broken into two parts – Lithosphere: upper mantle and crust – Asthenosphere: lower mantle ...
4.1 & 4.2 Plate Tectonics
4.1 & 4.2 Plate Tectonics

... forming new rock. • Ocean floor is moving away from these rifts ...
Plate Tectonics Chapter Challenge sample
Plate Tectonics Chapter Challenge sample

... seafloor. As the lithospheric plates continue to diverge over time, the new seafloor moves further away from the ridge and cools. As it cools, it becomes more dense and sinks back into the mantle, where it is heated and rises again. This pattern of heating and rising, cooling and sinking in Earth’s ...
FRAMEWORK
FRAMEWORK

... The continental rise. These areas are covered with thick layers of sediments (sand, mud, rocks). • The depth of the ocean varies. Ocean trenches are very deep, and the continental shelf is relatively shallow. • Ocean water is a complex mixture of gases (air) and dissolved solids (salts, especially s ...
tsunamis - MrDanielASBSukMSSci
tsunamis - MrDanielASBSukMSSci

... (750 mi) of fault line slipped 20 m (60 ft) along the subduction zone where the India Plate dives under the Burma Plate. The seabed of the Burma plate is estimated to have risen several metres vertically up over the India plate, creating shock waves in the Indian Ocean that travelled at up to 800 km ...
Seawater Articles - hrsbstaff.ednet.ns.ca
Seawater Articles - hrsbstaff.ednet.ns.ca

... researchers calculate that because the ocean will soak up some of this CO2, its surface pH will drop to 7.4 by 2300 and stay that low for hundreds of years (Nature, vol 425, p 365) Vulnerable creatures Atmospheric CO2 has risen well above 2000 ppm several times in the past 300 million years. Caldeir ...
The oceans are a connected system.
The oceans are a connected system.

... water in the thermocline drops fast with depth. ...
Using Isotopes to Understand the Oceans and Climate Change
Using Isotopes to Understand the Oceans and Climate Change

... ridges. Consequently, oceanographers are starting to use 14C-calibrated circulation models to backcalculate the source location and inputs of 3He needed to account for the world-wide database of 3He measurements. Applying a similar “inverse modeling” strategy to other data, such as to measurements o ...
Unit 6: Dynamic Planet: Plate Tectonics
Unit 6: Dynamic Planet: Plate Tectonics

... Unit 6: Dynamic Planet: Plate Tectonics Lecture 2 ...
Presentation
Presentation

... •Where plates collide, great mountain ranges may be pushed up, such as the Himalayas; or if one plate sinks below another, deep oceanic trenches and chains of volcanoes are formed. •Earthquakes are by far most common along plate boundaries and rift zones: plotting the location of earthquakes allows ...
Balancing global climate research
Balancing global climate research

... ignored. GATEWAYS research focuses on the major ocean current system in the Southern Hemisphere and its role in and impact on ocean circulation and climate. The Agulhas water transports and leakage cause a positive density anomaly in the South Atlantic that is approximately an order of magnitude lar ...
Aerosol pollutants can have long-range effects on ocean oxygen
Aerosol pollutants can have long-range effects on ocean oxygen

... understood. Aerosol pollutants may be partly responsible, according to a new study which modelled the effects of atmospheric pollution over the Pacific Ocean. The findings suggest that air pollution can exacerbate climate impacts on the ocean, even when the source is far away. At least half of the w ...
WIND - Fort Thomas Independent Schools
WIND - Fort Thomas Independent Schools

...  The land will heat up faster during the day than the water.  The cool air blows inland from the water pushing up the warm air.  The wind that blows from the water is known as sea breezes. ...
WIND - Fort Thomas Independent Schools
WIND - Fort Thomas Independent Schools

...  The land will heat up faster during the day than the water.  The cool air blows inland from the water pushing up the warm air.  The wind that blows from the water is known as sea breezes. ...
Plate Tectonics - THS Aquatic Science
Plate Tectonics - THS Aquatic Science

... As the two sides of the mountain move away from each other, magma wells up from the Earth's interior. It then solidifies into rock as it is cooled by the sea, creating new ocean floor. ...
contents - Less Stress More Success
contents - Less Stress More Success

... ● Lava soils are rich in iron, which is good for coffee production. ● Geothermal energy can be generated from hot rock and geysers. ...
ángeles garcía pardo
ángeles garcía pardo

... The dynamics of the seabed, Miquel Canals The deep seabed is far from being the calm place that research pioneers thought. Instead, both natural processes and human activities episodically disturb it. Recent studies have shown that dense shelf water cascading, open ocean deep convection and major st ...
Introduccon to PLATE TECTONICS
Introduccon to PLATE TECTONICS

... •  Earth changes in space •  Energy for change comes (as heat) from: –  an external source (the Sun) –  an internal source (radioac)ve decay in Earth’s core and mantle) ...
Conditions differ away from shore.
Conditions differ away from shore.

... rocks, reefs, or big plants to provide shelter from predators. The open ocean covers a huge area but contains fewer living things than the waters near shore. Life is more spread out in the open ocean. ...
- Google Sites
- Google Sites

... • Plate boundaries are always faults, but not all faults are plate boundaries. ...
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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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