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Sea-floor Spreading
Sea-floor Spreading

... spreading from vents (underwater holes) in a rift found in the Atlantic Ocean ...
Lecture 3
Lecture 3

... • Progressive spiraling caused by shallower currents pushing on deeper currents results in Ekman Spirals. • As spirals continue, wind shear becomes less and less at depth. • Eventually, deep currents travel ~90° to the wind direction. ...
course outline - Clackamas Community College
course outline - Clackamas Community College

... Explain the ocean system with regards to various regions in the ocean, the structure of the ocean basins and the various life zones found there Explain the structure of mid-ocean ridges, salinity changes in oceans, temperature changes in oceans, tides and ocean currents. Explain the concept of globa ...
sample paper
sample paper

... layer. In this layer density increase gradually increases with depth and water only moves slowly in this layer. There are not many currents in this layer. The three layers exist due to gravitational separation in which the density of a layer is less than the density of the layer below. As the pycnoc ...
New Carbon-Fixation Pathway Unveiled in Ocean Depths
New Carbon-Fixation Pathway Unveiled in Ocean Depths

... nderstanding the flow and processing of carbon in the world’s oceans, which cover 70 percent of Earth’s surface, is central to understanding global climate cycles, with many questions remaining unanswered. Between 200 and 1,000 meters below the ocean surface exists a “twilight zone” where insufficie ...
MSCI 101 - University of South Carolina
MSCI 101 - University of South Carolina

... Marine science is inherently integrative, encompassing four main scientific subdisciplines: biological, chemical, geological, ad physical oceanography. Therefore, in order to understand the oceans and become a marine scientist, one must first know the fundamental concepts within each of these areas. ...
Linking Ocean Management to Climate Change
Linking Ocean Management to Climate Change

... Linking Ocean Management to Climate Change VIKKI SPRUILL President & CEO, Ocean Conservancy June 7, 2007 ...
Ocean Currents
Ocean Currents

...  Crosses the Atlantic Ocean  Causes warmer climate in NW Europe ...
Blue Planet Lecture 2006
Blue Planet Lecture 2006

... last 100,000 years. • Abrupt, rapid climate changes can be strong and can be caused by a breakdown of the atmosphere-ocean interactions that control climate. ...
Grade 8 Science
Grade 8 Science

... Sonar – used to measure depth of ocean – echo location.Sound wave goes down and comes back to the ship.If it takes a short time for wave to come back – shallow water.Visa versa Depth probe – piece of equipment used to measure depth of the ocean. Coriolis Effect – The change in the direction of winds ...
4 spheres and water cycle cornell
4 spheres and water cycle cornell

... Hydro = water ALL water (below ground, on land, in sky) Can be solid, liquid, or a gas ...
Ocean floor - deb-or-ah
Ocean floor - deb-or-ah

... boring. Just off the continental shelf, the ocean floor is known as the abyssal plain. The depth of the abyssal plain is between 2200 and 5500 meters. It cover roughly 40% of the ocean floor. Less than one tenth of 1% of the abyssal plain has been explored by man. ...
Parent Signature_____________________ Ocean Unit
Parent Signature_____________________ Ocean Unit

... Study your notebook notes, study guide, and review pgs. C82-C95 in your textbook. SOL5.6 The student will investigate and understand characteristics of the ocean environment. Key concepts include a) geological characteristics (continental shelf, slope, rise); b) physical characteristics (depth, sali ...
Chapter 11
Chapter 11

... ridges are the abyssal plains and the occasional seamount ...
Seafloor Spreading
Seafloor Spreading

... form new ocean crust – Through time the new ocean crust moves away from the center of the mid-ocean ridge becoming cooler (and thus more dense) and sinks ...
Ocean Circulation
Ocean Circulation

... water away from an area, this area is compensated by the upward movement of deeper waters. The process of upwelling brings nutrient rich waters to the surface allowing large phytoplankton blooms to develop and feed which in turn support major fisheries. • This is a common process near coastlines of ...
The Earth`s Drifting Continents
The Earth`s Drifting Continents

... Alfred Wegener suggested that the continents were once and have since drifted ...
War and Expansion in the United States by marvin
War and Expansion in the United States by marvin

... ...
4.1 & 4.2C Ocean Life PPt
4.1 & 4.2C Ocean Life PPt

... Ch 4.1/4.2C Messana ...
Exam 3 PRACTICE – Winter 2016 KEY
Exam 3 PRACTICE – Winter 2016 KEY

... d. Deep-ocean circulation e. None of the above 15. A loop of connected surface currents is called a a. Gyre b. Coriolis structure c. Thermocline d. Pycnocline 16. What is the direct cause of the ocean’s surface currents? a. Salinity variations b. Density variations c. Vertical circulation d. Wind 17 ...
Seawater Properties - Marine Biology Honors
Seawater Properties - Marine Biology Honors

... • Temperature varies greatly in the ocean (between -2 ºC to 30 ºC). This has a strong influence on density. • Density is mass/volume. It is measured in g/cm3, g/ml or g/L. • A Hydrometer is the instrument used to determine density. • Salinity and temperature affect the density of water (as salinity ...
SeaWater properties
SeaWater properties

... Understand the processes that are continuously changing Earth’s surface as lithospheric plates move relative to one another. Identify the role of oceanic ridges, transform faults and deep-sea trenches in defining the edges of lithospheric plates. Understand the importance of asthenospheric thermal c ...
The Earth was extensively molten in the first 100 million years after
The Earth was extensively molten in the first 100 million years after

... The Earth was extensively molten in the first 100 million years after its formation. In that span of time, it acquired much of its present-day structure: the metallic core segregated and sank towards the center, while the mantle and crust separated at the surface. The primordial evolution of the man ...
Mapping the Ocean Floor
Mapping the Ocean Floor

... For hundreds of years, the only way to measure ocean depth was the sounding line, a weighted rope or wire that was lowered overboard until it touched the ocean floor. Not only was this method time-consuming, it was inaccurate; ship drift or water currents could drag the line off at an angle, which w ...
ocean zones - Somerset Academy
ocean zones - Somerset Academy

... • Guyots: are extinct volcanoes with eroded flat tops. ...
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Ocean



An ocean (from Ancient Greek Ὠκεανός, transc. Okeanós, the sea of classical antiquity) is a body of saline water that composes much of a planet's hydrosphere. On Earth, an ocean is one of the major conventional divisions of the World Ocean, which covers almost 71% of its surface. These are, in descending order by area, the Pacific, Atlantic, Indian, Southern, and Arctic Oceans. The word sea is often used interchangeably with ""ocean"" in American English but, strictly speaking, a sea is a body of saline water (generally a division of the world ocean) partly or fully enclosed by land.Saline water covers approximately 72% of the planet's surface (~3.6×108 km2) and is customarily divided into several principal oceans and smaller seas, with the ocean covering approximately 71% of Earth's surface. The ocean contains 97% of Earth's water, and oceanographers have stated that only 5% of the World Ocean has been explored. The total volume is approximately 1.35 billion cubic kilometers (320 million cu mi) with an average depth of nearly 3,700 meters (12,100 ft).As it is the principal component of Earth's hydrosphere, the world ocean is integral to all known life, forms part of the carbon cycle, and influences climate and weather patterns. It is the habitat of 230,000 known species, although much of the oceans depths remain unexplored, and over two million marine species are estimated to exist. The origin of Earth's oceans remains unknown; oceans are thought to have formed in the Hadean period and may have been the impetus for the emergence of life.Extraterrestrial oceans may be composed of water or other elements and compounds. The only confirmed large stable bodies of extraterrestrial surface liquids are the lakes of Titan, although there is evidence for the existence of oceans elsewhere in the Solar System. Early in their geologic histories, Mars and Venus are theorized to have had large water oceans. The Mars ocean hypothesis suggests that nearly a third of the surface of Mars was once covered by water, and a runaway greenhouse effect may have boiled away the global ocean of Venus. Compounds such as salts and ammonia dissolved in water lower its freezing point, so that water might exist in large quantities in extraterrestrial environments as brine or convecting ice. Unconfirmed oceans are speculated beneath the surface of many dwarf planets and natural satellites; notably, the ocean of Europa is estimated to have over twice the water volume of Earth. The Solar System's giant planets are also thought to have liquid atmospheric layers of yet to be confirmed compositions. Oceans may also exist on exoplanets and exomoons, including surface oceans of liquid water within a circumstellar habitable zone. Ocean planets are a hypothetical type of planet with a surface completely covered with liquid.
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