Plate Boundaries
Both Hess’s discovery and Wegner’s continental drift theory combined into what scientists now call the Plate Tectonic Theory
Theory of Plate Tectonics: • The Earth’s crust and part of the
upper mantle are broken into sections, called plates which move on a plastic-like layer of the mantle
Plate Tectonic Theory
Effects of Plate TectonicsThere are several geological processes that occur where plates meet:
1. Volcanoes - tend to erupt at plate margins as a result of a process called subduction
2. Earthquakes - occur where plates grind against or over one other
3. Mountain building - occurs as one plate is pushed over another
4. Seafloor spreading - occurs where two oceanic plates pull apart
Plate BoundariesThe earth’s tectonic plates continue to gradually move even today. The plates interact. Where one plate meets another, it is called a boundary.
Divergent: Boundary between two plates that are moving apart
Convergent: Boundary between two plates that are pushing together.
Subduction Zone: The area where one plate pushes down under another. Volcanoes are often created by this.
Transform (Strike-slip): Boundary between two plates that are sliding past one another.
The 3 Types of Plate Boundaries
Convergent BoundariesDescription: two plates that are pushing together
Land Features Formed: island arcs, trenches, volcanoes
Actual Examples: Himalayas, Mariana Trench, Hawaiian Islands
Picture of Motion:
“Convergent, means to come together.”
convergent boundary animation
Convergent Boundaries
What can convergent boundaries create? earthquakes island formation mountain forming volcanoes
Oceanic-Continental
Oceanic-Oceanic
Continental-Continental
ocean floor plate collides with a less dense continental plate
ocean floor plate collides with another ocean floor plate
continental plate collideswith another continental plate
Types of Convergent Boundaries
Convergent Boundaries
Oceanic/oceanic Subduction occurs
Oceanic/continental Oceanic plate sinks
Continental/continental Mountain ranges form
When two plates collide (converge) one plate moves under the other. This process is called “subduction.”
Convergent boundary of two oceanic plates.
Creates an ________ and a _____. Example: _____island arc trench Japan
Trench FormationSUBDUCTIONWhen two plates collide (converge) one plate moves under the other
Convergent boundary of an oceanic plate and a continental plate. Forms a _______ mountain range and a ______. Examples: _______ or _______ Mts
volcanictrench Cascades Andes
Convergent boundary of two continental plates. Forms a ______ mountain range. Examples: ___________, Alps, ______________
folded HimalayasAppalachians
The convergent boundary of the Eurasian and Indian Plates has resulted in the formation of the highest mountain range in the world – The Himalayas
This illustration shows the movement of the
land mass known as
India today. As it moved
on the Indian plate through
time, over millions of years,
it finally collided with the
Eurasian plate forming the
Himalayan Mountains
Mount Everest is the tallest mountain in the world, at over 29,000 ft. and is part of the Himalayas. This is a result of the Eurasian and Indian Plates colliding and it is still getting higher as these two plates continue to collide.
This map shows the large Himalayan Mountain range that has resulted from the collision of these two continental plates; which continues today.
Indian Plate
Eurasian Plate
Convergent Boundary – Indian and Eurasian Plates
Divergent BoundariesDescription: two plates that are diverging, or moving away from each other
Land Features Formed: earthquakes, rift valleys, and volcanoes
Actual Examples: African rift valley, mid-Atlantic ridge
Picture of Motion:
“Convergent means to spread apart.”
divergent boundary - seafloor
Divergent BoundariesDivergent Boundaries are the boundaries between two plates that are diverging, or moving away from each other.
divergent boundary - rift valley
When plates are spreading apart from one another there is a lot of geological activity. Earthquakes, and volcanoes occur here.
• In some places like East Africa, a rift valley can form that is hundreds of feet deep.
Divergent Boundary – Arabian and African Plates
Arabian Plate
African PlateRed Sea
Divergent boundary of two continental plates
East African Rift Zone
The Mid-Atlantic Ridge is one of the world’s largest divergent plates, running North to South in just about the center of the Atlantic Ocean. All along this ridge, volcanic activity takes place and the sea floor is spreading East and West at a rate of 1.25 cm per year. The divergent plate in Iceland is part of the Mid-Atlantic Ridge.
This map shows a divergent plate in Iceland. You can tell from the arrows that the Eurasian Plate and the North American Plate are spreading apart from one another
Transform BoundariesDescription: two plates that are sliding past one another
Land Features Formed: earthquakes
Actual Examples: San Andreas Fault
Picture of Motion:
“Transform means slide past one another.”
Transform Boundary
Transform Fault Boundaries
Transform Boundaries are the boundaries between two plates that are sliding horizontally past one another.
Plates Move Side by SideTransform boundaries neither create nor consume crust. Rather, two plates move against each other, building up tension, then releasing the tension in a sudden and often violent jerk. This sudden jerk creates an earthquake.
Earthquakes in Austin
Transform-fault boundary where the North American and Pacific plates are moving ____ each other.
Example: ________________ in California
past
San Andreas Fault
The San Andreas Fault, seen
here, is the result of the Pacific
Plate sliding past the North
American Plate. This is the site
of many of the earthquakes that
occur in the United States.
Changing Earth’s Surface
Plate movement can alter Earth systems and produce changes in Earth’s surface
Deformation of the crustFaultsMountain buildingLand subsidenceVolcanoes
Mechanism for Plate Tectonics
Why do the plates move?
• Due to tremendous heat, rock in the asthenosphere is like hot taffy
• This allows plates to ride on top of hot, flowing rock
• Plates move because heat is being released from deep inside the earth
• Convection currents cause hot material to rise and expand (plates diverge) and cooler material to sink and contract (plates converge)
Plates are “pushed” and “pulled” over the surface of the Earth due to unbalanced forces.
When convection currents reach the surface, plates are pushed apart
As the plates move away from each other, part of them are pulled into the Earth’s mantle
Convection Currents
Because temperature increases with depth, the inside of the earth is very hot. Rock near the core is heated and becomes less dense. It slowly rises while cooler rock nearer the surface is more dense and sinks. This forms convection currents just like those in our atmosphere.
As these convection currents in the mantle circulate, they cause the continents above them to move. What Wegener had no way of knowing is that the force that is driving plate tectonics is convection currents in the mantle.
Con
vect
ion
Cur
rent
s
Another way to relate to
convection currents is like
when you boil soup. As the
soup heats up, it rises to the
top of the container where it
begins to cool and sinks,
causing convection currents
to form, re-creating the same
process that takes place in
our Earth.
As two continental plates move toward each other, what landforms would you expect to see?a. Volcanoes
b. Cliffs
c. New Land
d. Mountains
No - These form at edges of plates or over hot spots
No - Forms when plates move apart
No - These are erosional landforms or minor uplift areas
Yes - because 2 continental masses will push into each other and “crumple” the edges to form mountains
Where would you find the newest land on Earth?a. In areas of continental convergence
b. In areas where two ocean plates come together
c. In areas where plates are moving apart
d. In areas where two plates are sliding past each other
No - Mountains would form here from existing land.
No - You would find land movement but not new land being formed
No - You would find trenches in this area.
Yes - When plates move apart it is due to magma reaching the surface. When magma cools new land is formed.