Abyssal plain
Abyssal hills
Accretionary prism
Aerial view
Age of rock
Apparent polar wander
Asthenosphere
Atolls
Basement
Benioff zone
Buoyancy
Convection
Continental shelf
Continental slope
Continental rise
Core
Cross-section
Crust
Dating
Fracture zones
Geothermal gradient
Guoyts
Hotspot
Island arcs
Isostatic equilibrium
Lateral extent
Lithosphere
Midocean ridges
Morphology
Oceanic islands
Paleomagnetism
Plateaus
Polar wander (see Apparent polar wander)
Potential energy
Radioactive decay
Radiometric dating
Seafloor spreading
Sediment
Spreading rate
Subduction
Submarine fans
Submarine canyons
Terranes
Transform faults
Trench
Vertical extent
Volcanic arcs
- Plate margin
-
A plate margin is the edge of a plate. All the edges of each plate touch the edge of a neighboring plate beccause the entire surface of the Earth is covered with plate. There are no holes where there are no plates.
The plate margins are important because that is where neighboring plates touch and where most action takes place. It is a little like cars in a minor traffic accident. The outer edges of the car are where most action takes place. The stuff in side is more protected.
At any plate margin, there can be three different kinds of interaction between neighboring plates.
The three kinds of plate margins are:
- Divergent plate margin - where adjacent plates move apart from each other
- Convergent plate margin - where adjacent plates move towards each other
- Transform plate margin - where adjacent plates move ... each other
Ways with words:
1. How we use them here, the words edge, margin and boundary are interchangeable.
2. When people talk or write about "divergent plate margins" for example, they might call them "divergent margins" or "divergent boundaries" too.
- Plate boundary (see Plate margin)
-
Plate tectonics
Subduction zone
Seafloor spreading
TBA
TBA
TBA