PLATE
TECTONICS
G11 Earth Science
The Evidence Comes Together
The seafloor has a large mountain range running through it.
• Deep trenches are found far from the ridges.
• Guyots have eroded tops that are deep below sea level.
• The magnetic polarity of the seafloor changes.
• The center of the ridge is of normal polarity.
• Stripes of normal and reverse polarity are found symmetrical on
both sides of the ridge.
• The youngest seafloor is at the ridge.
• The oldest is farthest from the ridge.
• The oldest seafloor is much younger than the oldest continent.
Tectonic Plate
Motions
Theory of Plate Tectonics
The theory of plate tectonics is what brings
together continental drift and seafloor
spreading. Plates are made of lithosphere
topped with oceanic and/or continental crust.
The plates are moved around on Earth’s surface
by seafloor spreading.
What The Theory Explains
Plate tectonics theory explains why:
• Earth's geography has changed over time and continues to change today.
• some places are prone to earthquakes while others are not.
• certain regions may have deadly, mild, or no volcanic eruptions.
• mountain ranges are located where they are.
• many ore deposits are located where they are.
• living and fossil species of plants and animals are found where they are.
• some continental margins have a lot of geological activity, and some have none.
• Plate tectonic motions affect Earth’s rock cycle, climate, and the evolution of life.
Divergent Plate
Boundaries in the
Oceans
Mid-ocean Ridges
Continental Rifting
Transform Plate
Boundaries
Convergent Plate
Boundaries
Ocean-Continent Convergence
Ocean-Ocean Convergence
Continent-Continent Convergence
Supercontinent Cycle and Pangaea