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Visitors to this site can access information on tropical storms and hurricanes in the Atlantic Ocean as far back as 1851. Information provided here includes a yearly map showing the tracks of all storms, and individual maps for each storm. The individual maps are accompanied by data tables that show latitude, longitude, wind speed, dates, and times.
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This document outlines the development of the theory of contintental drift and how many lines of evidence collected over several decades by various researchers were brought together to explain how the seafloor spreads and the continents move about. Links to additional information are included.
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Visitors
to
this
site
can
learn
about
conditions
necessary
to
view
auroras
from
their
geographical
location.
Materials
provided
include
an
explanation
of
geomagnetic
activity
and
maps
showing
its
distribution,
and
an
explanation
of
how
geographic
latitude
differs
from
magnetic
latitude,
with
tables
showing
magnetic
latitudes
for
major
cities
around
the
world.
Links
are
provided
to
auroral
activity
...
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This site explains how core samples are taken from the ocean floor. Topics include how research cruises are planned, who makes up the crew of a research vessel, and what a cruise track is. Links to additional information are embedded in the text.
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This resource describes what mineral sands are, and discusses the heavy, dark-colored minerals that they contain (rutile, ilmenite, zircon, monazite). A map shows locations of mineral sands deposits in Australia.
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Visitors can use sea surface temperature data to build animations that show seasonal and yearly fluctuations, and compare them to data from other selected months and years. The animations can be constructed in map or globe formats and may be viewed on the website or downloaded.
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This
account
of
the
history
and
evolution
of
the
Mississippi
River
Delta
makes
use
of
text,
photographs,
and
satellite
imagery
to
describe
how
the
delta
has
formed
and
migrated
throughout
recent
geologic
history.
Users
can
read
about
the
formation
and
subsequent
abandonment
of
various
delta
lobes
and
how
deltaic
landforms
(back
bays,
levees,
barrier
islands)
are
formed
and
destroyed
as
a
result
of
...
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This site discusses the loss of ice from the West Antarctic Ice Sheet, which has been observed for the last thirty years. Topics include why, when, and how much ice was lost by the ice sheet since the last glacial maximum, and whether the ice sheet was ever smaller than it is today.
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This resource uses text, images, maps and a laboratory exercise to explain how differences in the temperature and salinity of ocean water cause the formation of deep-ocean currents. It is part of the Jet Propulsion Laboratory's "Ocean Surface Topography from Space" website. This material is also available on the "Visit to An Ocean Planet" CD-ROM.
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The
most
profound
deformational
event
involving
the
interaction
of
lithospheric
plates
is
a
collision
between
continents;
for
example,
the
collision
of
the
Indian
continent
with
the
Eurasian
continent,
which
began
in
the
Eocene.
This
continuing
collision
has
produced
intracontinental
thrust
sheets
responsible
for
the
highest
mountains
in
the
world.
Mount
Everest,
the
Annapurna
Range,
and
the
rest
...
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