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Continental Drift - CoconinoHighSchool
Continental Drift - CoconinoHighSchool

... 1. Discovery of the Mid-Atlantic Ridge (Ewing) - Ocean floor mapping led to the discovery of a global mid-oceanic ridge mountain chain zig-zagging around the continents. 2. Magnetic Variations on the Ocean Floor (Palaeomagnetism) - during cooling, minerals in the Basaltic rock, align themselves alon ...
Investigation 5: Earthquakes, Volcanoes, and Mountains Vocabulary
Investigation 5: Earthquakes, Volcanoes, and Mountains Vocabulary

... There are hot spots in the mantle that make magma for a long period of time. Hot spots stay in one spot and don’t move with the lithospheric plates. Volcanoes form over this hot spot, and scientists can tell how plates have moved by the line of volcanoes formed by the hot spot. See Figure 9. Figure ...
Dynamic Crust 4 Plate Tectonics
Dynamic Crust 4 Plate Tectonics

...  The rocks created at the mid-ocean ridge have magnetic minerals that are aligned with Earth’s magnetic field.  Earth’s magnetic field reverses polarity on a cycle of thousands of years. ...
Continental Drift
Continental Drift

... 1. Discovery of the Mid-Atlantic Ridge (Ewing) - Ocean floor mapping led to the discovery of a global mid-oceanic ridge mountain chain zig-zagging around the continents. 2. Magnetic Variations on the Ocean Floor (Palaeomagnetism) - during cooling, minerals in the Basaltic rock, align themselves alon ...
SANCOR Newsletter 210 - National Research Foundation
SANCOR Newsletter 210 - National Research Foundation

... capable  to  absorb  a  percentage  of  the  ...
History of Ocean Exploration and Marine Sciences
History of Ocean Exploration and Marine Sciences

... History of Ocean Exploration and Marine Sciences – Chapter 2 5. How did ancient explorers navigate near shore and in the open ocean? 6. What major ocean discovery is credited to the Greek Pytheas? 7. What two major contributions are credited to the Greek Eratosthenes? 8. What were the significances ...
Convergent Plate Margins, Subduction Zones, and
Convergent Plate Margins, Subduction Zones, and

... Convergent Plate Margin, Subduction Zone, and Arc-Trench System Convergent Plate Margin: 2-D (surficial) plate boundary that is geometrically required for Plate Tectonic theory. Subduction Zone: 3-D region defined by asymmetric sinking of lithosphere into the mantle. Defined by earthquakes at depths ...
Dynamic Earth Interactive Web Quest
Dynamic Earth Interactive Web Quest

... ii. Discovered evidence that the same plant and animal fossils were found along the coasts of these continents, although they were now separated by vast oceans. iii. Noticed geological formations like mountain ranges, on the two continents also matched up. ...
The Creation of the Ocean Floor SCI 209 Oceanography The ocean
The Creation of the Ocean Floor SCI 209 Oceanography The ocean

... the tricks of the oceanic world. The development of the ocean ground is a continuous movement of plate limits shifting as well as moving the ocean bed. With the moving happenings can make natural disasters, for example earthquakes, tsunamis, as well as volcanic outbreaks. The hypothesis of plate tec ...
plate tectonics
plate tectonics

... One of the plates subducts beneath the other. A series of volcanic islands, called an island arc, can form along the plate boundary. ...
Peer-reviewed Article PDF
Peer-reviewed Article PDF

... continental drift. The view is based on the results of experimental studies of Roy and Tuttle [8] that confirmed depression of melting point of silicate rocks under hydrothermal and high pressure condition. 2. Originally the small Earth was entirely covered with a solid supercontinent composed of g ...
Remote Sensing of the Diffuse Attenuation Coefficient and Related
Remote Sensing of the Diffuse Attenuation Coefficient and Related

... ⎝ green ⎠ where χ and γ are determined empirically and CHL is retrieved as a spectral ratio of water reflectance (e.g. the OC3, OC4 algorithms). A generalization of Eq 2.b expresses light attenuation as linear function of the concentrations of the main optically active components in case 2 waters, C ...
Continental Arcs
Continental Arcs

... – Primary basalt magma surrounded by mantle peridotite • Negatively buoyant – Melt more dense than surrounding rocks ...
1 Years of the Maritime Continent (YMC) (2017-2019)
1 Years of the Maritime Continent (YMC) (2017-2019)

... propagation of the MJO. Atmospheric deep convection penetrating the tropopause over the MC makes it a primary spot for vigorous stratosphere-troposphere interaction. The Indonesian Throughflow (ITF), the artery connecting the tropical Pacific and Indian Oceans, is a crucial link of the ocean general ...
theory in ms word format
theory in ms word format

... When in an area between the lithosphere and pyrosphere a high quantity of fluids is concentrated , these fluids move, carried away by pyrosphere from west to east in almost the same speed to this, with small alterations due to the morphology of the lithosphere, that is, it is lower under the contin ...
Name - Hagen. C
Name - Hagen. C

... 93. What country does the Gulf Stream effect? 94. Describe, in terms of temperature, a current that is moving from the equator to the polar regions. 95. Is the California current a cold current or warm current? ________________ 96. Currents in the Northern Hemisphere are deflected which way? _______ ...
Global-scale variations of the ratios of carbon to phosphorus in
Global-scale variations of the ratios of carbon to phosphorus in

... low, and lower ratios in nutrient-rich upwelling zones and high-latitude regions, where organic matter export is high. This suggests that total carbon export is relatively constant throughout the oceans, in agreement with recent estimates of carbon fluxes10 . We conclude that the latitudinal pattern ...
day 1 Objective and HW
day 1 Objective and HW

... Subduction ...
Theory of Plate Tectonics
Theory of Plate Tectonics

... (coal deposits) found in Antarctica • Glaciation in Africa, South America, India, and Australia during the same time ...
Ocean storage
Ocean storage

... circulation system is millennial. Early estimates of the time required for downwelling surface water to fully displace the deep ocean volume based on 14C radioactive tracer measurements put this “ventilation time” of the deep ocean at 1400 years. Subsequent improved understanding of the processes i ...
Effect of air-sea forcing on tropical ocean mixed layer depth (MLD
Effect of air-sea forcing on tropical ocean mixed layer depth (MLD

... their  interactions  are  investigated,  which  show  the  following  results.  (1)  The  thermocline anomalies  in  the  tropical   Pacific  have  a  zonal  dipole  pattern  with  160°W  as  its  axis  and  a  meridional seesaw  pattern  with  6‐8°N  as  its   transverse  axis.  The  meridional osc ...
crust
crust

... the asthenosphere they also move the crust. The crust gets a free ride with these currents, like the cork in this illustration. ...
Organized Opposition to Plate Tectonics: The New Concepts in
Organized Opposition to Plate Tectonics: The New Concepts in

... on subjective, qualitative correlations, and has not been ground-truthed by radiometric dating, and that the stripe pattern is better explained by fault-related bands of rocks of different magnetic properties. They stress the need to drill all the way through the ocean crust and into the mantle befo ...
slides_04 - International Pacific Research Center
slides_04 - International Pacific Research Center

... Ecology: marine life, entanglement, ingestion of plastic, accumulation of organic pollutants in marine life tissues. human health – introduction of organic pollutants in the marine life food chain up to human consumption ...
Slide 1
Slide 1

... currents, ocean plates cool and become denser than the mantle rock beneath them. ...
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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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