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Understanding Divergent Plate Boundaries

Sep 10, 2024

Lecture Notes: Divergent Plate Boundaries

Introduction

  • Earth is over four billion years old.
  • Ocean basin rocks are much younger, forming less than 200 million years ago.
  • Ocean basins are recycled starting with new oceanic lithosphere formation at divergent plate boundaries.

Divergent Plate Boundaries

  • Plates move away from each other along divergent boundaries.
  • Examples found in all major ocean basins.
  • Characterized by:
    • Continuous oceanic ridges forming submarine mountain ranges.
    • Shallow earthquake activity.
    • Presence of the youngest oceanic lithosphere.

Observations

  • Bathymetry: Depth and topography of ocean features.
  • Divergent boundaries have:
    • Oceanic ridges higher than surrounding sea floor.
    • Volcanic activity sources.
    • Younger ocean floor near the ridge, older as you move away.

Formation of Ocean Basins

  • Start without an ocean; examine a continent splitting apart.
  • Rift valleys form from stretching and thinning of continental crust.
    • Marked by volcanoes or lava flows
    • Example: African continent splitting (e.g., Red Sea region)
  • Rift valley lowers below sea level, forming a narrow ocean as it floods.

Historical Context

  • Atlantic Ocean formed post-Pangaea breakup.
  • Red Sea opened 30 million years ago, seawater filled 5 million years ago.
  • Evidence of volcanism through newly formed volcanic islands.

Evolution of Ocean Basins

  • Ocean basins can expand from hundreds to thousands of kilometers.
  • Width depends on plate motion rates and duration of process.

Summary of Plate Separation Process

  • Separation occurs in rift zones associated with oceanic ridges.
  • Mantle convection drives the process.
  • Rift zone faulting causes shallow earthquakes.
  • Magma rises, forming new oceanic crust.
    • Surface magma forms basaltic lava.
    • Subsurface magma solidifies into plutonic rock like gabbro.
  • High heat flow results in higher ridge elevations.
  • Oldest crust near continents, youngest at ridges.

Learning Objectives

  • Understand features and processes of divergent plate boundaries.
  • Practice by drawing a labeled sketch.

Reflection

  • Reflect on learning objectives and personal understanding.⭕️