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What are waves? - the National Sea Grant Library
What are waves? - the National Sea Grant Library

... As the moon rotates around the earth, the bulges move as well resulting in 2 high and 2 low tides per day at most locations on the coast with a tidal period of approximately 12 ½ hours. The exact number of the tides is dependent on the shape of the ocean bottom along the coast. This can have a signi ...
Dropping pH in the Oceans Causing a Rising Tide of...
Dropping pH in the Oceans Causing a Rising Tide of...

... reduce the alkalinity of the oceans. And as the pH drops, marine organisms that produce shells and carbonate skeletons grow weak and die off. The discovery that carbon dioxide emissions can lower global ocean pH is very recent, even though chemists and biologists have for long known that when carbon ...
Paleozoic Plate Tectonics Quiz
Paleozoic Plate Tectonics Quiz

... 3) When continents converge to make a supercontinent a) The convergent plate boundary goes from ocean-continent to continent-continent. b) Island arcs and microcontinents may also join in. c) Processes take place over tens or hundreds of millions of years. d) All of these. ...
Workshop_Ackleson
Workshop_Ackleson

... 1994: UNCLOS, established an international legal framework defining ocean-related rights and responsibilities of nations. 1999: Joint Commission for Oceanography and Marine Meteorology, established by WMO and IOC to coordinate international activities in oceanographic and atmospheric research. 1999: ...
Evolution of Ocean Observatories
Evolution of Ocean Observatories

... 1987: International Geosphere/Biosphere Program, established to coordinate international efforts to determine the impact of human activities on natural processes. 1992: Global Ocean Observing System, support office established under aegis of IOC and other international environmental groups. 1994: UN ...
File
File

... more sodium and chlorine than any other element. What compound do these two elements form? Sodium and chlorine. Sodium chloride (SALT) is the compound that the two elements form. ...
Constructive and Destructive Landforms
Constructive and Destructive Landforms

...  Constructive forces: forces that build up an existing landform or create a new one.  Caused by: water, gravity, wind and glaciers.  Ex: deposition, landslides, volcanic eruptions, floods ...
Harbor Branch Executive Director Presents “Our Changing Oceans
Harbor Branch Executive Director Presents “Our Changing Oceans

... Both lecture times are followed by a meet-the-speaker reception. The event will be held in the Johnson Education Center auditorium on the Harbor Branch campus, located at 5600 N. U.S. 1 in Fort Pierce. There is no charge to attend. Leinen will give an overview of some of the large-scale changes in o ...
Chapter 16
Chapter 16

... (which is denser) moves deep beneath the surface. a. As this water releases heat to the air, keeping Europe warmer than it would otherwise be, the water cools, becomes saltier through evaporation, and thus becomes denser and sinks, creating a region of downwelling known as the North Atlantic Deep Wa ...
Lecture 7. Marine Sediments
Lecture 7. Marine Sediments

... CaCO3 is variable, depending on P, T, pH ...
Modeling the Ocean Floor Lab
Modeling the Ocean Floor Lab

... Seamounts (submerged volcanoes), and Guyots (flat-topped inactive seamounts). The Ocean Basin Floor accounts for 30% of Earth’s surface and lies in between the continental margin and the mid oceanic ridge. The Mid Oceanic Ridge is located along divergent plate boundaries where the seafloor is spread ...
Theory of Plate Tectonics
Theory of Plate Tectonics

... sea-floor spreading. This theory was formed as new information was learned about the nature of the ocean floor, Earth’s ancient magnetism patterns, the location of volcanoes and earthquakes, the flow of heat from Earth’s interior, and the worldwide distribution of plant and animal fossils. Earth’s o ...
(1 point
(1 point

... EARTHQUAKE NOTES(40 points) ...
Worksheet as a MS Word file ( format)
Worksheet as a MS Word file ( format)

... different water depths in south Atlantic Ocean just off Brazil (Latitude 0.5 o N, Longitude 37.5o W), as shown by the white dot on the map below. The samples were taken to the shipboard laboratory and analyzed for the variation in nitrogen (in the form of nitrate - NO3), phosphorous (in the form of ...
File
File

... activity occurs on the ocean floor *Most volcanoes are found where the plates that make up Earth’s crust meet each other *Volcanoes tend to erupt where one plate is pushed under another plate *The Ring of Fire follows the boundaries of the plates that meet around the Pacific Ocean *An eruption is an ...
by downloading expedition 12 worksheet as a pdf
by downloading expedition 12 worksheet as a pdf

... different water depths in south Atlantic Ocean just off Brazil (Latitude 0.5o N, Longitude 37.5o W), as shown by the white dot on the map below. The samples were taken to the shipboard laboratory and analyzed for the variation in nitrogen (in the form of nitrate - NO3), phosphorous (in the form of p ...
Glossary
Glossary

... primarily north-south in the Pacific and rises 1 to 1.5 miles (1.6-2.4 km) above the ocean floor, with a width of 1 to 2 miles (1.6-3.2 km), at an average depth of 1.7 miles (2.7 km). It abuts the North American Plate at the Gulf of California. ecotone: zone where two ecosystems overlap, each of whi ...
Seafloor Spreading PPT
Seafloor Spreading PPT

... In the 1960’s, technology allowed scientists to take pictures with the help of a submersible called ALVIN. It could withstand crushing pressures up to 4 kilometers. ...
Ch - saddlespace.org
Ch - saddlespace.org

... Ch. 15 Earthquake Notes 1. An Earthquake is movement of the Earth’s crust caused by a release of energy. 2. Elastic Rebound is when the rock snaps back to its shape when the built up stress is released. 3. Where the rock actually breaks is called the focus. The point directly above the focus on the ...
Ch. 34 Powerpoint - Plain Local Schools
Ch. 34 Powerpoint - Plain Local Schools

... C. Rising, falling air masses and Earth’s Rotation cause predictable wind patterns which combine with the uneven heating of the Earth and the shapes of the continents create currents - riverlike flow pattern within a body of water, circulates water back and forth from poles to equator ...
A. temperate deciduous forest
A. temperate deciduous forest

... C. Rising, falling air masses and Earth’s Rotation cause predictable wind patterns which combine with the uneven heating of the Earth and the shapes of the continents create currents - riverlike flow pattern within a body of water, circulates water back and forth from poles to equator ...
Properties of sea-water and their distribution in the oceans
Properties of sea-water and their distribution in the oceans

... • Affects many other properties in the ocean (e.g., density, speed of sound, etc.) as well as weather and climate. • Many oceanic features and circulation patterns can be inferred from temperature measurements. • Scientific units: Celsius or Kelvin (absolute temperature) °C = °K – 273.15 (not Fahren ...
marine ecosystem
marine ecosystem

... Marine topographies include coastal and oceanic landforms ranging from coastal estuaries and shorelines to continental shelves and coral reefs. Further out in the open ocean, they include underwater and deep sea features such as ocean rises and seamounts. The submerged surface has mountainous featur ...
1 Billion Years Ago 450 Million Years Ago 400 Million Years Ago
1 Billion Years Ago 450 Million Years Ago 400 Million Years Ago

... continent as plates in the Earth’s crust moved apart. Today’s Green Mountains formed as these plates eventually collided again, closing the ancient ocean and forcing the bottom sediments up into new mountains. The finishing touches to the scene you see today occurred when glaciers scoured the landsc ...
geology
geology

... continent as plates in the Earth’s crust moved apart. Today’s Green Mountains formed as these plates eventually collided again, closing the ancient ocean and forcing the bottom sediments up into new mountains. The finishing touches to the scene you see today occurred when glaciers scoured the landsc ...
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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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