NYU Diverging Converging and Transform Tectonic Plate Boundaries Paper - Humanities
According to plate tectonic theory, Earth’s surface is divided into moving plates. A plate is a large, mobile slab of rock that is part of Earth’s rigid out shell known as the lithosphere. This includes rocks of the crust and upper mantle.The boundaries between plates are of three general types. The boundary between plates that are moving apart is termed diverging while a boundary between plates that are moving toward each other is called converging. A transform boundary is found where two plates are moving horizontally past each other.
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Name:
Date:
LAB #
: Crustal Boundaries
Introduction: According to plate tectonic theory, Earth’s surface is divided into moving plates.
A plate is a large, mobile slab of rock that is part of Earth’s rigid out shell known as the
lithosphere. This includes rocks of the crust and upper mantle.
The boundaries between plates are of three general types. The boundary between plates that are
moving apart is termed diverging while a boundary between plates that are moving toward each
other is called converging. A transform boundary is found where two plates are moving
horizontally past each other.
Objective: You will distinguish between diverging, converging and transform tectonic plate
boundaries.
Vocabulary
lithosphere:
divergent plate boundary:
convergent plate boundary:
transform plate boundary:
subduction:
Andes Mountains:
Procedure:
A. Fill in the data chart below using the Tectonic Plates map provided. Place a check in the
appropriate box identifying the type of plate boundary.
Procedure B:
1. On the graph provided, construct a cross-section along line AB on your map of South
America to show the depth of earthquake foci.
2. After plotting the depth of earthquake foci, connect the points with a smooth line.
3. On your cross-section, copy the arrows that show the direction the crustal plates are moving.
4. Determine which side of the cross-section represents continental crust. Print the word
“continental” in this location.
5. Determine which side of the cross-section represents oceanic crust. Print the word “oceanic”
in this location.
6. Write in the average density of the continental crust and the oceanic crust on the crosssection. Refer to the “Inferred Properties of Earth’s Interior” diagram.
7. On the cross-section, predict the direction of any movement where these two crustal plates
meet. Draw arrows on the cross-section showing the direction of plate movements.
Procedure C:
1. Note that on the “United States Pacific Coastline” map, thick arrows show the directions of
plate movement but no arrow for the North American Plate is shown. Referring to the attached
Tectonic Plate map, draw a thick arrow on the North American Plate indicating its direction of
movement.
2. What is the relative movement of rocks on the west side of the San Andreas fault compared to
the direction the North American Plate is moving?
3. Using separate paper, cut out two pieces of paper that are rectangles 3 cm x 6 cm.
4. The dashed lines in the diagram below represent the rectangles that you cut out.
5. Placing the two cutouts side by side, label each one as shown in the diagram.
6. Place the labeled cutouts side by side on the diagram with the fault at the boundary between
them. The cutout below represents the Pacific Plate and the one on the right represents the North
American Plate. Both are moving in the direction of the arrows.
7. By moving the cutout “plates” in the direction of the arrows, determine how their differing
rates of movement are producing the displacement of rocks on either side of the San Andreas
Fault. Write your conclusions below.
Discussion Questions: (Answer in complete sentences).
1. Using the cross-section of South America, describe the pattern of earthquake depth from west
to east along line AB.
2. Based on your answer to question 1, what appears to happen as the ocean plate to the west
collides with the continental plate to the east?
3. Referring to a world map, what surface feature on the west coast of South America has
apparently formed as a result of collision of two crustal plates?
4. According to your data chart and the Tectonic Plates map, where are most divergent plate
boundaries found?
5. Referring to Procedure C, what type of plate boundary is the San Andreas fault?
6. At which type of plate boundary would a subduction zone be found?
7. At which type of plate boundary is new oceanic crust created?
8. Oceanic trenches are associated with which type of plate boundary?
Conclusion: Describe the three types of plate boundaries.
Topic 2
The Way the Earth Works:
Examining Plate Tectonics
Continental drift:
An idea before its time
◼
Alfred Wegener
• First proposed continental drift hypothesis
in 1915
• Published The Origin of Continents and
Oceans
◼
Continental-drift hypothesis
• Supercontinent called Pangaea began
breaking apart about 200 million years ago
Pangaea approximately
200 million years ago
Evidence for Continental
Drift
Fit of Continents
and Matching
Mountain
Ranges
Evidence for Continental
Drift
Fossils on
Different
Continents
Evidence for Continental
Drift
Paleoclimatic
evidence
Plate tectonics:
The new paradigm
◼
Plate Tectonics
◼ Much more encompassing theory than
continental drift
◼ The composite of a variety of ideas that
explain the observed motion of Earth’s
lithosphere (NOT just the crust).
Plate tectonics:
The new paradigm
◼
Earth’s major plates
• Associated with Earths strong, rigid outer
layer
• Known as the lithosphere
• Consists of uppermost mantle and overlying
crust
• Overlies a weaker region in the mantle called
the asthenosphere
Plate tectonics:
The new paradigm
◼
Earth’s major plates
• Asthenosphere
• Exists beneath the lithosphere
• Hotter and weaker than the lithosphere
• Allows for motion of lithosphere
Plate tectonics:
The new paradigm
◼
Earth’s major plates
• Seven major lithospheric plates
•
•
•
•
•
•
•
North American
South American
Pacific
African
Eurasion
Australian
Antarctic
Plate tectonics: The
new paradigm
◼
Earth’s major plates
• Plates are in motion and continually
changing in shape and size
• Largest plate is the Pacific plate
• Several plates include an entire continent
plus a large area of seafloor
Plate tectonics:
The new paradigm
◼
Earth’s major plates
• Plates move relative to each other at a very
slow but continuous rate
• About 5 centimeters (2 inches) per year
• Cooler, denser slabs of oceanic lithosphere
descend into the mantle
• Grinding movement of plates generate
earthquakes, volcanoes, deform large masses of
rock into mountains
Earth’s
plates
Earth’s
plates
Plate tectonics:
The new paradigm
◼
Plate boundaries
• Interactions among individual plates
occur along their boundaries
• Types of plate boundaries
• Divergent plate boundaries (constructive
margins)
• Convergent plate boundaries (destructive
margins)
• Transform fault boundaries (conservative
margins)
Divergent plate boundary
Divergent plate boundary
Continental
rifting
Continental
Rifting
Oceanic-Continental
Convergence
Oceanic-Oceanic
Convergence
Continental-Continental
Convergence
Convergent plate boundaries
◼
Older parts of oceanic plates are returned to
the mantle in these destructive plate margins
• Surface expression of the descending plate is
an ocean trench
• Also called subduction zones
• Average angle of subduction = 45
India-Asia Collision before
Himalayas
India-Asia Collision produced
the Himalayas
Transform fault boundaries
Plates slide past one another and no new
lithosphere is created or destroyed
◼ Transform faults
◼
• Most join two segments of a mid-ocean ridge
along breaks in the oceanic crust known as
fracture zones
• A few (the San Andreas fault and the Alpine
fault of New Zealand) cut through
continental crust
Transform
faults
What drives plate motions
Researchers agree that convective flow in
the mantle is the basic driving force of
plate tectonics
◼ Forces that drive plate motion
◼
• Slab-pull: descending oceanic crust pulls
the plate
• Ridge-push: elevated ridge system pushes
the plate
• Slab suction
Forces driving
plate motions
Importance of
plate tectonics
◼
The theory provides explanations for
• Earth’s major surface processes
• The geologic distribution of earthquakes,
volcanoes, and mountains
• The distribution of ancient organisms and
mineral deposits
Evidence for Plate Tectonics
Distribution
of Volcanoes
Evidence for Plate Tectonics
Distribution
of
Earthquakes
Evidence for Plate
Tectonics
Paleomagnetic
Reversals
Recorded at
Mid-Ocean
Ridges
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Evidence for Plate Tectonics
Hot Spots
https://
youtu.be/
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Evidence for Plate Tectonics
Age
Vs.
Depth of Ocean
Floor
Evidence for Plate Tectonics
Plate
motions
...
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