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Understanding the Quiet Revolution of Geoscience
Oct 3, 2024
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Lecture Notes: The Quiet Revolution of Plate Tectonics
Introduction
Shift in understanding of Earth in the 1960s
Development of the theory of plate tectonics
Influences structure and behavior of Earth
Historical Context
16th-century speculation on landmass shapes
Alfred Wegner (1912):
Proposed Pangaea
Evidence: Fossils, rock types, mountain ranges
Concept of continental drift
Skepticism from scientific community
Post-World War II Developments
New oceanic evidence re-emerges
Bruce Heason and Marie Tharp (1957):
Published the first physiographic map of the Atlantic Ocean floor
Mid-Atlantic Ridge: Discovery of ocean floor features
Harry Hess (1960):
Theory of seafloor spreading
Conveyor belt model of ocean floor creation and recycling
Robert Dietz (1961):
Similar spreading seafloor theory
Seafloor Spreading Evidence
Vine and Matthews (1963):
Earth's magnetic field reversals recorded in rocks
Magnetic stripes as historical records
The Concept of Subduction
Oceanic crust subduction under continental crust
Formation of subduction zones and ocean trenches
Example: Pacific Ring of Fire
The Plate Tectonics Theory
Development of the theory in the 1960s
Tectonic plates floating on the asthenosphere
Types of plate boundaries:
Divergent:
Plates moving apart (e.g., East-Pacific Rise)
Convergent:
Plates colliding (e.g., Andes and Himalayas)
Transform:
Plates sliding past each other (e.g., San Andreas Fault)
Continuing Exploration and Future Questions
Ongoing research with satellite technology
Comparison with Venus
Understanding the origin of plate tectonics
Connections between tectonics and life evolution
Conclusion
The revolution continues to impact our understanding and exploration of Earth sciences
Upcoming topics in further lectures
Additional Notes
Importance of contributions from young, innovative scientists
The role of technology and funding in advancing geoscience research
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