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Lesson 2.4
Processes and
Landforms along Plate
Boundaries
Objective
1
At the end
of the
lesson, you
should be
able to:
learn the process of land
formation along plate
boundaries.
Learn about It!
• Most tectonic processes
occur along the three types
of plate boundaries,
namely:
• Divergent plate boundary
• Convergent plate
boundary
• Transform plate boundary
Types of Plate Boundaries
Continental Plate Boundaries
Learn about It!
• Continental rifting occurs
within a continent and is
caused by opposing
tensional forces that stretch
and thin the lithosphere,
causing the outermost
crustal rocks to break
through normal faulting,
thus forming a continental
rift.
Divergent Plate Boundaries
Continental Rifting
Learn about It!
• New ocean basins may
form between two rifted
continents once the
lithosphere thins
sufficiently for magma to
erupt along an axis.
Divergent Plate Boundaries
Formation of Oceanic Basin
Learn about It!
• Convergent plate
boundaries form different
landforms and involve
different processes
depending on the type of
plates involved in the
collision.
Convergent Plate Boundaries
Convergent Plate Boundaries
Learn about It!
• In oceanic-continental
convergent margins, the
denser oceanic crust
subducts under the lighter
continental crust. This
process forms continental
volcanic arcs.
Types of the Convergent Plate Boundaries
Oceanic plate subducting under a
lighter continental plate.
Learn about It!
• In oceanic-oceanic
convergent margins, the
older and much denser
plate subducts under the
younger plate. This process
forms volcanic island arcs.
Types of the Convergent
Plate Boundaries
Volcanic island arcs and associated trenches
along the Pacific Ring of Fire.
Learn about It!
• Convergent plate
boundaries may also
develop through the
collision of two
continental plates, by
continental-continental
convergent margin.
Types of the Convergent Plate Boundaries
Mountain range formed through the
collision of two continental plates.
Learn about It!
• Continental-continental
convergent margin
forms mountain ranges
with linear elevated
regions.
Types of the Convergent Plate Boundaries
Mountain range formed through the
collision of two continental plates.
Learn about It!
• Transform plate
boundaries which are
characterized by horizontal
motion along transform fault
systems parallel to the
boundary separating two
plates form fault systems
around the world.
Transform Plate Boundaries
Transform boundaries along mid-oceanic
ridges forming a step-like pattern.
Learn about It!
• Transform faults are part of
curvilinear breaks in the seafloor
known as fracture zones.
• Earthquake activity is restricted only
to the transform portion of fracture
zones that lies between offset ridge
segments or trenches.
Transform Plate Boundaries
San Andreas Fault in California,
United States (Image from USGS).
Key Points
In oceanic-oceanic convergence, forms volcanic island
arcs, or simply, island arcs.
Divergent plate boundaries are home to landforms
including continental rifts and oceanic ridges.
1
Convergence gives rise to landforms known as
continental volcanic arcs.
2
3
Key Points
Transform faults are part of curvilinear breaks in the
seafloor known as fracture zones.
Continental-continental (C-C) convergence involves a
buoyant landmass (continents, arcs) moving towards the
margin of another buoyant landmass due to the
subduction of an intervening seafloor forming orogenic
plate.
4
5
Check Your Understanding
1. Himalayan Mountain Range
2. San Andreas Fault
3. Andes Mountains
4. Mid-Atlantic Ridge
5. East Pacific Rise
Identify in which boundary the landforms are found. Put DB
for divergent, CB for convergent, and TB for transform.
Challenge Yourself
What is the Ring of Fire and how was it formed?
Bibliography
Carlson, Diane H. and Charles C. Plummer. 2009. Physical Geology: Earth Revealed, 8th Edition. New
York: McGraw-Hill Companies, Inc.
Hefferan, Kevin and John O’Brien. 2010. Earth Materials. United Kingdom: Wiley-Blackwell Publishing.
King, Hobart. “Transform Plate Boundary.” Geology.com. Accessed May 11, 2017. http://
geology.com/nsta/transform-plate-boundaries.shtml
Levin, Harold L. 2013. The Earth Through Time. United States of America: John Wiley & Sons Inc.
Marshak, Stephen. 2009. Essentials of Geology 3rd Edition. New York: W.W. Norton & Company.
Stephen J. Reynolds, et al. 2013. Exploring Geology, 3rd Edition. United States: McGraw-Hill Companies,
Inc.
Bibliography
Tarbuck, Edward J. and Frederick J. Lutgens. 2015. Earth Science. New Jersey: Pearson Prentice Hall.
United States Geological Survey. 1999. “J. Tuzo Wilson: Discovering transforms and hotspots” Accessed
May 11, 2017. https://pubs.usgs.gov/gip/dynamic/Wilson.html
United States Geological Survey. 2014. “Understanding Plate Motions” Accessed May 1, 2017.
https://pubs.usgs.gov/gip/dynamic/understanding.html

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Science 10 2.4 Processes and Landforms along Plate Boundaries.pptx

  • 1. Lesson 2.4 Processes and Landforms along Plate Boundaries
  • 2. Objective 1 At the end of the lesson, you should be able to: learn the process of land formation along plate boundaries.
  • 3. Learn about It! • Most tectonic processes occur along the three types of plate boundaries, namely: • Divergent plate boundary • Convergent plate boundary • Transform plate boundary Types of Plate Boundaries Continental Plate Boundaries
  • 4. Learn about It! • Continental rifting occurs within a continent and is caused by opposing tensional forces that stretch and thin the lithosphere, causing the outermost crustal rocks to break through normal faulting, thus forming a continental rift. Divergent Plate Boundaries Continental Rifting
  • 5. Learn about It! • New ocean basins may form between two rifted continents once the lithosphere thins sufficiently for magma to erupt along an axis. Divergent Plate Boundaries Formation of Oceanic Basin
  • 6. Learn about It! • Convergent plate boundaries form different landforms and involve different processes depending on the type of plates involved in the collision. Convergent Plate Boundaries Convergent Plate Boundaries
  • 7. Learn about It! • In oceanic-continental convergent margins, the denser oceanic crust subducts under the lighter continental crust. This process forms continental volcanic arcs. Types of the Convergent Plate Boundaries Oceanic plate subducting under a lighter continental plate.
  • 8. Learn about It! • In oceanic-oceanic convergent margins, the older and much denser plate subducts under the younger plate. This process forms volcanic island arcs. Types of the Convergent Plate Boundaries Volcanic island arcs and associated trenches along the Pacific Ring of Fire.
  • 9. Learn about It! • Convergent plate boundaries may also develop through the collision of two continental plates, by continental-continental convergent margin. Types of the Convergent Plate Boundaries Mountain range formed through the collision of two continental plates.
  • 10. Learn about It! • Continental-continental convergent margin forms mountain ranges with linear elevated regions. Types of the Convergent Plate Boundaries Mountain range formed through the collision of two continental plates.
  • 11. Learn about It! • Transform plate boundaries which are characterized by horizontal motion along transform fault systems parallel to the boundary separating two plates form fault systems around the world. Transform Plate Boundaries Transform boundaries along mid-oceanic ridges forming a step-like pattern.
  • 12. Learn about It! • Transform faults are part of curvilinear breaks in the seafloor known as fracture zones. • Earthquake activity is restricted only to the transform portion of fracture zones that lies between offset ridge segments or trenches. Transform Plate Boundaries San Andreas Fault in California, United States (Image from USGS).
  • 13. Key Points In oceanic-oceanic convergence, forms volcanic island arcs, or simply, island arcs. Divergent plate boundaries are home to landforms including continental rifts and oceanic ridges. 1 Convergence gives rise to landforms known as continental volcanic arcs. 2 3
  • 14. Key Points Transform faults are part of curvilinear breaks in the seafloor known as fracture zones. Continental-continental (C-C) convergence involves a buoyant landmass (continents, arcs) moving towards the margin of another buoyant landmass due to the subduction of an intervening seafloor forming orogenic plate. 4 5
  • 15. Check Your Understanding 1. Himalayan Mountain Range 2. San Andreas Fault 3. Andes Mountains 4. Mid-Atlantic Ridge 5. East Pacific Rise Identify in which boundary the landforms are found. Put DB for divergent, CB for convergent, and TB for transform.
  • 16. Challenge Yourself What is the Ring of Fire and how was it formed?
  • 17. Bibliography Carlson, Diane H. and Charles C. Plummer. 2009. Physical Geology: Earth Revealed, 8th Edition. New York: McGraw-Hill Companies, Inc. Hefferan, Kevin and John O’Brien. 2010. Earth Materials. United Kingdom: Wiley-Blackwell Publishing. King, Hobart. “Transform Plate Boundary.” Geology.com. Accessed May 11, 2017. http:// geology.com/nsta/transform-plate-boundaries.shtml Levin, Harold L. 2013. The Earth Through Time. United States of America: John Wiley & Sons Inc. Marshak, Stephen. 2009. Essentials of Geology 3rd Edition. New York: W.W. Norton & Company. Stephen J. Reynolds, et al. 2013. Exploring Geology, 3rd Edition. United States: McGraw-Hill Companies, Inc.
  • 18. Bibliography Tarbuck, Edward J. and Frederick J. Lutgens. 2015. Earth Science. New Jersey: Pearson Prentice Hall. United States Geological Survey. 1999. “J. Tuzo Wilson: Discovering transforms and hotspots” Accessed May 11, 2017. https://pubs.usgs.gov/gip/dynamic/Wilson.html United States Geological Survey. 2014. “Understanding Plate Motions” Accessed May 1, 2017. https://pubs.usgs.gov/gip/dynamic/understanding.html