Plate Tectonics the movement of Earth

Plate Tectonics Tectonic plates: pieces of the Earth’s crust & upper mantle Plate boundaries: places where plates meet

Plate Tectonics Movement of plates creates forces that affect Earth’s surface at the plate boundaries and causes them to move. Plates move in 3 ways: 1. slide past each other 2. move apart (divergent) 3. collide (convergent)

Transform Fault Boundaries Faults form when plates slide past each other A fault is a large crack in rocks that can break EARTHQUAKES can happen along fault lines

San Andreas Fault, CA

Divergent Plates Plates move apart b/c of pulling forces (tension) that act in opposite directions. New crust forms in the gaps where plates pull apart. Form mid ocean ridges (in oceans), and rift valleys (on continents)

Divergent Boundaries Boundary between two plates that are moving apart or rifting   RIFTING causes SEAFLOOR SPREADING

Divergent Plate Movement: Seafloor Spreading the movement of two oceanic plates away from each other (at a divergent plate boundary), which results in the formation of new oceanic crust (from magma that comes from within the Earth's mantle) along a mid-ocean ridge. Ocean floor spreading was first suggested by Harry Hess and Robert Dietz in the 1960's.

Features of Divergent Boundaries Mid-ocean ridges

Features of Divergent Boundaries Rift valleys Quilotoa, Ecuador

Features of Divergent Boundaries Fissure volcanoes Hawaii, USA

Mid-Atlantic Ridge a divergent tectonic plate boundary located along the floor of the Atlantic Ocean the longest mountain range in the world. separates the Eurasian Plate and North American Plate and the African Plate from the South American Plate

Divergent Plates Bridge between continents in Reykjanes peninsula, southwest Iceland across the Alfagja rift valley, the boundary of the Eurasian and North American continental tectonic plates.

Oceanic Ridges

Convergent Plates When plates collide, different things can happen (depends on the density of the plates involved). There can be: continental-continental collisions, oceanic-oceanic collisions & continental-oceanic collisions

Continental-Continental Collisions Forms a mountain range

Oceanic-Continental Collisions Forms a trench and volcanic arc

Andes Mountains, South America

Oceanic-Oceanic Collisions Forms an island arc

Aleutian Islands, Alaska

Subduction Zones When one plate plate sinks underneath another plate. The denser plate sinks underneath & into the mantle.

Fold When rocks bend due to force.

Fold: When rocks bend Anticline (Upward) Syncline (Downward)

Anticline

Syncline

Convection the circulation of heat A theory explaining why the plates move. Theory says plates move b/c the mantle material is being circulated b/c of the difference in densities in the mantle.