The Earth's surface, broken up into several large pieces called crustal plates or tectonic plates
Crustal plates
Float on the denser semi-molten rock beneath them
Move very slowly across the surface of the planet, a few centimetres per year
Primary crustal plates
North American
South American
African
Antarctic
Indo-Australian
Eurasian
Pacific
Smaller crustal plates
Nazca
Cocos
Madagascar
Okinawa
Plate boundary/plate margin
The area where the edges of two plates meet
Types of plate boundaries
Convergent
Divergent
Transcurrent
Convergent boundaries
Plates move toward each other
Cause earthquakes, folding, and volcanic activity
About 3/4 of all earthquakes occur along convergent boundaries
Rocks buckle and fold, pushed upward to form mountain ranges
Oceanic crust is pushed under continental crust (subduction)
Divergent boundaries
Plates move away from each other
Magma rises and cools, creating new crust
Earthquakes and volcanic activity can occur
Transcurrent boundaries
Plates slide past each other
Earthquakes can occur
Volcanic activity
The rising of molten material within the lithosphere or onto the Earth's surface
Extrusive volcanic features
Formed on the surface
Intrusive volcanic features
Formed below the surface
Shield volcanoes
Mt. Kilauea in Hawaii
Composite cones
Soufriere Hills volcano in Montserrat
Lava plateau
Incrediblylarge amounts of basalt lava that erupt and cover many square miles, forming a wide flat plateau
Lava plateau
The Columbian River Plateau, covering 160,000 square km
Caldera
A large volcanic depression at least one kilometer in diameter, formed when a volcano empties most of its underground magma chamber in a massive eruption
Caldera
Qualibou caldera in St. Lucia, 3.5 km x 5 km in size
Volcanic plug
Formed when molten magma cools and hardens inside the vent of an active volcano
Sill
Formed when magma flows horizontally between rock layers, cooling to form a horizontal sheet of solid rock
Dyke
A vertical sheet of rock formed when magma moving toward the surface cools and hardens
Batholith
A very large feature formed when an underground reservoir of molten rock cools and hardens
Viscous lava
Thick, flows slowly, erupts explosively and violently, builds steep-sided cones