Restless earth Flashcards
Conservative plate margin
2 plate margins sliding against each other at a different speed and angle. This causes earthquakes
E.g San Andreas fault
Constructive plate margin
2 plates moving away from each other. This causes cracks and holes where there is a high chance of the magma to come out
Destructive plate margins
Collision: 2 continental plates moving against each other on a head on buckle
Subduction: 2 (oceanic and continental) plates moving against each other with one of them (oceanic) being subduct under the continental plate (volcano)
Structure of the earth
Core - Heats up mantle
Mantle - convection currents
Crust - tectonic plates
Oceanic crust
Newer (less than 200 million years old)
Denser
Can sink
Can be renewed or destroyed
Continental crust
Older (over 1500 million years old)
Less dense
Cannot sink
Cannot be renewed or destroyed
Fold mountains and formation
Large mountain ranges formed with rock layers crumpled together
- forms when plates move against each other. If occurs in the same area with ocean trenches, it is subduction
- if formed by itself, collision has taken place
Ocean trenches and formation
Deep sections of the ocean
- formed when plates move against each other
- if occur in the same area with fold mountains, it is due to subduction
- if by itself, it is collision
Composite volcanoes and characteristics
Volcano made up of lava and ash
Infrequent, violent eruptions
Steep slopes and narrow base
Layers if thick lava and ash
Shield volcano and characteristics
Volcano made of mostly lava
Frequent, non violent eruptions
Wide base and gentle slopes
Layers of runny lava and little ash
Supervolcano and and characteristics
- a big volcano that erupts 1000 km squared of material
Bigger than normal volcanoes
Found in large depressions called calderas
Emits 1000 km squared of material
Formation of a supervolcano
Rising magma cannot escape through crust, this causes a large bulge to appear on the surface
Cracks appear in the surface making gas and ash escaping through
Magma chamber collapses, forming a caldera
Difference between focus and epicenter
Epicenter is on the surface
Focus is below the surface
Strength of Earthquakes at Different plate margins
Destructive: pressure from sinking plates can cause strong earthquakes
Constructive: friction and pressure from moving apart plates causes less severe earthquakes
Conservative: pressure released from stucked plates will cause a great and severe earthquakes
How to measure earthquakes
Using seismographs to record extent of the earthquake
The Richter scale
The mercalli scale