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Chapter Three: The Dynamic Earth
Chapter Three: The Dynamic Earth

... process by which liquid water is heated by the sun and then rises into the atmosphere as water vapor  Condensation: water vapor forms water droplets on dust particles in clouds  Precipitation: the larger water droplets fall from the clouds as rain, snow, sleet, or hail ...
Unit 3: Plate Tectonics: Test Review
Unit 3: Plate Tectonics: Test Review

... 6. Where was it found? Antarctica, South America, India, Africa and Australia. 7. How did it prove the existence of Pangaea? The continents which are now in cooler climates, could not have supported the growth of Glossopteris proving the continents must have been in a warmer climate at one time. ...
The stability of the continents and the tendency for old oceanic
The stability of the continents and the tendency for old oceanic

... The
difference
in
elevation
between
continents
and
oceans
can
be
explained
using
the
principle
of
 isostasy.
Isostasy
says
that
if
we
consider
two
blocks
of
different
density
and
thickness
floating
in
 a
fluid,
the
pressure
at
some
reference
depth
below
both
blocks
must
be
equal.
The
pressure,
P
,
at
 ...
Convergent Boundaries
Convergent Boundaries

... •Focus is the point of sudden energy release •Epicenter is located at the earth’s surface immediately above the focus ...
Session H: Ocean Salinity
Session H: Ocean Salinity

... Surface: Sea-surface temperature, Sea-surface salinity, Sea level, Sea state, Sea ice, Current, Ocean colour (for biological activity), Carbon dioxide partial pressure, air-sea fluxes, Sub-surface: Temperature, Salinity, Current, Nutrients, Carbon, Ocean tracers, Phytoplankton. Furthermore: Ocean bo ...
Why is the Ocean Salty?
Why is the Ocean Salty?

... South Pacific, North and South Atlantic, Indian and Arctic Oceans and the Antarctic waters or seas. Scientists believe that the seas are as much as 500 million years old because animals that lived then occur as fossils in rocks which once were under ancient seas. There are several theories about the ...
report - Woods Hole Oceanographic Institution
report - Woods Hole Oceanographic Institution

... remote sensing, completed by process studies at sea, to track the response of arctic marine ecosystems to climate variability and change. The team develops diagnostic and predictive models of arctic marine ecosystems, perfecting the deployment of profiling floats and autonomous underwater vehicles i ...
- OceanRep
- OceanRep

... from 8:30-11:30 and afternoon practical sessions from 13:30-17:00 at the more than 50 instruments on our Sonne expedition. (Soccer results: Argentina vs Netherlands, 4:2 decided by penalty kicks, the competitors for the final are decided). Preliminary highlights of the measurements: We find ourselve ...
Earthquakes
Earthquakes

... blue) under most parts of the Pacific and Indian Oceans. Large elevations in the surface (red and yellow) under continental regions such as Eurasia, North America, Australia, Antarctica and parts of Africa. In general 400 km discontinuity correlates well continents and ocean basins. 670 km discontin ...
Evolving Earth: Plate Tectonics - Global Change
Evolving Earth: Plate Tectonics - Global Change

... The gross structure of the Earth can be determined from the propagation of elastic waves that are generated from earthquakes. If we look at the wave propagation in more details, we are actually able to recognize second-order variations that define layers in the outer 700 km and lateral variation in ...
OCEAN-ATMOSPHERIC INTERACTION IN THE SUBTROPICAL
OCEAN-ATMOSPHERIC INTERACTION IN THE SUBTROPICAL

... variability of the Subtropical North Pacific. The forcing is in the form of air-sea boundary fluxes, i.e. momentum flux and buoyancy flux. Clear understanding of physical processes of the subtropical Pacific air-sea interaction and quantitatively description of the processes are premise and basis fo ...
Seafloor spreading ws
Seafloor spreading ws

... The greatest challenge for mountain climbers is Mt. Everest, whose peak rises 8,872 meters above sea level. This is the highest mountain in the world, though many mountains around it are almost as high. Mt. Everest is in the Himalayas, a series of massive ranges that extends 2,500 kilometers across ...
8. Earth`s Moving Plates
8. Earth`s Moving Plates

... Cracks in the Earth's Crust The solid crust acts as a heat insulator for the hot interior of the earth. Below the crust, in the mantle, is the molten material called magma. Tremendous heat and pressure within the earth cause the hot magma to flow in convection currents. Periodically it rises to the ...
Tectonic Plate Boundaries
Tectonic Plate Boundaries

... At this point, water from the ocean will rush in, forming a new sea or ocean basin in the rift zone. ...
Name
Name

... deposition : the dropping or settling of eroded material ...
Climate Zones - Lourdes Academy
Climate Zones - Lourdes Academy

... • All three reshape the land by a process called erosion, in which rock and soil are moved from one place on the earth’s ...
Lecture #6 Causes of Ice Ages & Glacial
Lecture #6 Causes of Ice Ages & Glacial

... Inclination of the earth’s magnetic field varies with latitude. It is parallel to the surface over the equator and vertical over the magnetic poles. Paleomagnetic inclination can be used to infer paleo-latitude of igneous rocks and to reconstruct ...
Prince Rupert Community Observatory Information Package
Prince Rupert Community Observatory Information Package

... High Frequency (HF) RADAR (CODAR) system capable of measuring surface current speed and direction, as well as an Automatic Identification System (AIS) antenna to track large vessels in the region. ONC is also installing instrumentation at a second location on the west side of Ridley Island. The inst ...
Exploring the Possibility of Altered Ocean Circulation Patterns Using
Exploring the Possibility of Altered Ocean Circulation Patterns Using

... Several methods have been investigated in the attempt to determine whether or not a significant change in ocean circulation is imminent. Shimokawa and Ozawa (2002) explore the issue as an initial-value-boundary-condition-type problem, investigating irreversible transition to a state with a higher ra ...
TECTONIC PLATES
TECTONIC PLATES

... The locations of volcanoes can also help identify the locations of plate boundaries. Some volcanoes form when plate motions generate magma that erupts on Earth’s surface. For example, the Pacific Ring of Fire is a zone of active volcanoes that encircles the Pacific Ocean. This zone is also one of Ea ...
B - Uplift Education
B - Uplift Education

... The theory of plate tectonics explains that earth’s lithosphere moves due to the unbalanced forces occurring within the mantle. Alfred Wegner was one of the first scientists to collect scientific evidence in an effort to prove that earth’s tectonic plates drifted. Which of the following pieces of ...
Plate Boundaries and Earthquake Science
Plate Boundaries and Earthquake Science

... we will go over some example questions at the start of the lecture today o material covered: first 8 lectures (including the video) o up to next Tuesday's class  Prof. Ramsey will return for that class and answer any exam-related ...
What is carbon cycle?
What is carbon cycle?

... CO2 is also exchanged continuously between the ocean and the atmosphere.  This exchange is largely controlled by sea surface temperatures, ocean acidity, circulating currents and the biological processes of photosynthesis and respiration by marine plants and animals.  Cold ocean waters favour the up ...
Geological Oceanography
Geological Oceanography

... • Length varies in different parts of the world – East Coast of Canada: up to 400km long – West Coast of US: only a couple of km long ...
(b) examine the chemical, physical, and thermal structure of Earth`s
(b) examine the chemical, physical, and thermal structure of Earth`s

... These currents regulate temperatures on the continents. Because global warming is changing the density of these polar oceans due to glacial and ice-cap melt, this current could stop. Ultimately, this could alter the temperatures over the continents by as much as 10˚C. Global warming could cause cont ...
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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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