Download As we told you in a recent Instruction, much of the Earth`s

Earth Science Lesson 3
Dynamic Earth Processes (Grades 8-12 )
Instruction 3-3
Plate Boundaries
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As we told you in a recent Instruction, much of the Earth's lithosphere (its Crust
and the top layer of its Outer Mantle) is made up of moving masses of rock called
tectonic plates (tectonic means moving).
There are a dozen or so major plates and several minor ones. Most are both
partly oceanic (under oceans) and partly continental (under land).
These plates float on the asthenosphere like an iceberg floats on the ocean.
(The asthenosphere, as you remember, is the bottom layer of the Earth's Outer
Mantle. It is made up of tough liquid rock.)
As we said, these plates are constantly moving -- but they move at different
speeds. The Arctic Ridge moves the slowest -- at less than 2.5 centimeters a
year. The East Pacific Rise (near Easter Island in the South Pacific) is the
fastest. It moves at more than 15 centimeters a year.
To see a diagram of the Earth's major plates, click:
http://www2.nature.nps.gov/geology/usgsnps/pltec/pltec2.html
The boundaries between plates are sometimes hard to see here on Earth. But
it's easy to map them from space with GEOSAT satellites.
There are four major types of plate boundaries:
Divergent boundaries
Convergent boundaries
Transform boundaries
Plate boundary zones
These boundaries are where events like earthquakes, tsunamis (massive tidal
waves) and volcanic eruptions usually occur.
To see simple diagrams of the first three types of boundaries, click:
http://www2.nature.nps.gov/geology/usgsnps/pltec3.html
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California Content Standards Earth Science 3.b.
B. J. Subbiondo © 2004
Earth Science Lesson 3
Dynamic Earth Processes (Grades 8-12 )
Instruction 3-3
Plate Boundaries
www.etap.org
Divergent Boundaries
Divergent boundaries are places where the plates pull away from each other.
When this happens, new crust is created as magna (molten rock) pushes up from
the Earth's Mantle to fill the space the plates left behind.
The best-known divergent boundary is the Mid-Atlantic Ridge. This is a
submerged mountain range that extends from the Arctic Ocean to below the
southern tip of Africa.
The rate at which plates move apart here is 2.5 centimeters a year. This has
been going on for the past 100-200 million years.
It's what caused the Atlantic Ocean to start growing (during the Mesozoic Era)
from a tiny inlet between Europe, Africa and the Americas into the mighty ocean
it is today.
To see a drawing of the Mid-Atlantic Ridge, click:
http://pubs.usgs.gov/publications/text/ridge.html
This ridge also runs right through the country of Iceland, which is splitting
apart between the North American and Eurasian Plates.
Volcanic activity is also frequent here, especially around Krafla Volcano in the
northeastern part of Iceland.
To see a diagram of how these plates diverge in Iceland, click:
http://pubs.usgs.gov/publications/text/understanding.html#anchor1534371
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Convergent Boundaries
Convergent boundaries are places where plates bump into each other, like
bumper cars at a carnival.
When this happens, the Earth's crust is often destroyed as one plate is
subducted (sinks) under another.
What type of convergence takes place depends on what type of plates are
involved.
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California Content Standards Earth Science 3.b.
B. J. Subbiondo © 2004
Earth Science Lesson 3
Dynamic Earth Processes (Grades 8-12 )
Instruction 3-3
Plate Boundaries
www.etap.org
There are three types of convergences:
Oceanic-Continental
Oceanic-Oceanic
Continental-Continental
Oceanic-Continental Convergence
Under the Pacific Ocean, there are trenches that are thousands of kilometers
long. These trenches cut into the ocean floor and were created by oceaniccontinental convergence. They are the deepest parts of the ocean.
Off the coast of South America along the Peru-Chile Trench, the oceanic Nazca
Plate is pushing into (and sinking under) the continental part of the South
American Plate. This is causing the already huge Andes Mountains to rise even
higher.
It is also causing earthquakes.
On June 9, 1994, a huge earthquake (magnitude 8.3) struck near La Paz, Bolivia.
This was within the subduction zone between the Nazca and South American
Plates.
Fortunately little damage was done since the earthquake occurred 636 km deep
in the ocean.
Oceanic-Oceanic Convergence
When two oceanic plates collide, one is usually subducted under the other -- and
an ocean trench is formed.
The Mariana Trench, near the Mariana Islands, marks where the Pacific Plate
bumps up against the Philippine Plate. A portion of this trench, called the
Challenger Deep, is thought to be over 11,000 meters deep.
Oceanic-oceanic convergence frequently results in the formation of volcanoes.
There are two primary types of volcanoes: shield volcanoes and strato
volcanoes.
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California Content Standards Earth Science 3.b.
B. J. Subbiondo © 2004
Earth Science Lesson 3
Dynamic Earth Processes (Grades 8-12 )
Instruction 3-3
Plate Boundaries
www.etap.org
Shield volcanoes have broad gentle slopes and are built up by the eruption of
fluid basalt lava. Strato volcanoes are tall and conical and are made from
hardened lava and volcanic ash.
In either case, debris from volcanoes piles up over time on the ocean floor. After
millions of years, the debris grows tall enough to rise out of the sea.
When this happens, a volcanic island, or chain of islands, is formed -- like the
Mariana Islands or the Aleutians.
Not all volcanoes come about when plates run into each another. Some emerge
in the middle of plates over hot spots (places where rising plumes of molten
Mantel escape to the Earth's crust). We'll tell you more about these is an
upcoming Instruction.
But back to oceanic plates -- sometimes one plate sinks beneath another and
disappears completely. This is happening right now off the coast of Oregon and
Washington.
The small Juan de Fuca Plate, a remnant of the larger Farallon Plate, will one
day be totally consumed as it continues to sink beneath the North American
Plate.
Continental-Continental Convergence
When two continents meet head on, neither is subducted. That is because
continental rocks are relatively light and resist downward motion.
Instead, the crust of the Earth buckles and gets pushed upward or sideways.
About 50 million years ago, the continent of India collided with Asia. This caused
the Eurasian Plate to crumple and override the Indian Plate. After the collision,
continental-continental convergence pushed the Himalayas and the Tibetan
Plateau up to their present astonishing heights.
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California Content Standards Earth Science 3.b.
B. J. Subbiondo © 2004
Earth Science Lesson 3
Dynamic Earth Processes (Grades 8-12 )
Instruction 3-3
Plate Boundaries
www.etap.org
Transform Boundaries
Transform boundaries neither create nor consume the Earth's crust.
Instead, two plates move back and forth --or up and down -- against each other.
This builds up tension that is eventually released in a sudden, violent jerk.
This sudden jerk is an earthquake.
The world's most famous transform boundary is The San Andreas Fault in the
Western United States.
To the west of the San Andreas Fault lies the Pacific Plate, which is moving
northwest. To the east is the North American Plate, which is moving southeast.
Earthquakes occur here frequently.
Land movement occurs daily.
Los Angeles, located on the Pacific Plate, is now 340 miles south of San
Francisco, which is located on the North American Plate.
In 16 million years, the plates will have moved so much that Los Angeles will be
north of San Francisco.
To see what happens daily at the San Andreas Fault line, click:
http://www.pbs.org/wgbh/aso/tryit/tectonics/transform.html
and http://pubs.gov/publications/text/understanding.html
Plate Boundary Zones
Some boundaries between plates are not clear-cut or simple.
In some places, boundaries are not well defined because deformation (structural
change) takes place over a very broad belt called a plate boundary zone.
The Mediterranean-Alpine region between and Eurasian and African Plates
is one such zone. A number of smaller fragments of plates (microplates) have
been discovered here.
These zones have complicated geological patterns and earthquake structures.
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