Zusammenfassung der Ressource
GEOGRAPHY
- Plate movements
- Divergent
- Oceanic - Oceanic
- Definition
- As two oceanic plates diverge, the edges of the plates are pushed upward to form ridges.
- Material from the mantle wells up through the ridges, cools and hardens
to form a new ocean floor. This is called sea floor-spreading.
- New oceanic crust forming continuously and becomes older as it
moves away from the ridge crest with seafloor spreading.
- Effects
- Mid-oceanic ridges
- Earthquakes
- Volcanoes
- Continental - Continental
- Definition
- As two continental plates pull apart, faults (cracks between rocks) occur.
- Land sinks between the faults, forming rift valleys
- Effects
- Rift valley
- Transform
- Continental - Continental
- Effects
- Earthquakes
- Definition
- Plates move past each other in different directions.
- Tear faults form, acoompanied by earthquakes because
of the great amount of stress built up in these areas.
- There is little volcanic avitivity and little crustal material is destroyed.
- Convergent
- Oceanic - Oceanic
- Effects
- Oceanic trench
- Volcanoes
- Definition
- When two oceanic plates collide, one may sink beneath the other, producing an oceanic trench.
- Subducted plate melts and the magma rises and forms volcanoes.
- Continental - Continental
- Effects
- Fold mountains
- Earthquakes
- Definition
- When two continental plates collide, neither tends to subduct as their densities are similar.
- The two continental plates buckle and upfold, forming fold mountains.
- Oceanic - Continental
- Definition
- When a continental plate collides with an oceanic plate, the denser oceanic plate subducts under the lighter continental plate.
- At the subduction zone, an oceanic trench may form.
- Effects
- Oceanic trench
- Fold mountains
- Earthquakes (due to subduction)
- Volcanoes
- Volcanoes
- Shield volcanoes
- Properties
- Effusive eruptions
- Shield shape with broad base and gentle slopes
- Basaltic lava
- GTV: Low amount of dissolved gas; Higher temperature (1200 degrees); Low viscosity
- Examples
- Kilauea, Hawaii
- Mt. Washington, USA
- Stratovolcanoes
- Examples
- Mt. Fuji, Japan
- Krakatoa, Indonesia
- Mt. St Helens, USA
- Properties
- Violent and explosive eruptions
- Cone shape with steep slopes
- Acidic lava
- GTV: High amount of
dissolved gas; Lower
temperature (800 degrees);
High viscosity
- Definition
- How do volcanoes form?
- Volcanoes can from either when on top of
a hotspot or when tectonic plates converge
or diverge. Magma escapes through cracks
of the plate and rises to form a volcano.
- What is a volcano?
- A volcano is a vent in the earth from which molten rock, lava and steam issue.
- Where are volcanoes located?
- Most volcanoes are found along the Pacific Ring of Fire.