tectonic plates: gateway 1 Flashcards
1
Q
oceanic-oceanic divergence
A
- oceanic north American plate diverges from the Eurasian plate to form the MID ATLANTIC RIDGE
- when the oceanic north american plate diverges from the oceanic eurasion plate
> tensional force is exerted - as magma rises through the cracks and fissures at the zone of divergence, the cool and solidify to form new sea floor through the process of sea floor spreading
> a linear ridge is formed which is known as the mid oceanic ridge
> at various points along the mid oceanic ridge magma may continue to exploit the cracks and fissures along the linear ridge to form submarine volcanoes - submarine volcanoes may rise above the surface of the water, forming volcanic islands
2
Q
continental-continental plate divergence
A
- when the continental nubian plate and the continental somalian plate diverges
> EAST AFRICAN RIFT VALLEY is formed - when the plates diverge, the continental crust is stretched
> the tensional force causes fault lines and fractures to form at the plate boundary
> blocks of land masses will be displaces and subside along the faultlines
> forming a linear depression
> the EAST AFRICAN RIFT VALLEY
3
Q
oceanic-oceanic plate convergence
A
- when the oceanic pacific plate and the oceanic philipenes plate converges
> MARIANA TRENCH is formed - when two plates converge, compressional force is being exerted
> the denser oceanic plate sinks beneath the less dense oceanic plate - at the point of subduction, linear depression is formed
> the OCEANIC TRENCH is formed on the seafloor - part of the subducted plate melts to form magma
> magma rises through the cracks and fissures to the earth’s surface to form submarine volcanoes
> due to multiple eruptions, the submarine volcanoes rises above the surface of the water to form volcanic islands
4
Q
continental-continental convergence
A
- as the indian plate converges with the eurasion plate
> the HIMALAYAS is formed - when the two continental plates converge, compressional force is exerted
> since the two plates are similar in density and are light and buoyant
> they resist subduction during convergence
> the edges fold and buckle upwards and sideways to form a series of fold mountains
5
Q
oceanic-continental convergence
A
- the oceanic australian plate and the continental eurasion plate
> SUNDA TRENCH
- when the oceanic plate converges with a continental plate
> compressional force is exerted - the denser oceanic plate subducts beneath the less dense continental plate
- at the point of subduction, an oceanic trench is formed
- part of the subducted plate melts to form magma
- as the magma rises through the cracks and fissures of overlying plate, a volcano is formed
- the edges of the continental plate folds and buckles upwards and sideways
6
Q
transform plate boundaries
A
- San Andreas fault between the Pacific plate and the North American plate
- in 1960s, an earthquake occurred in San Francisco at the San Andres fault
> caused several hundred kilometers of the North American plate to move an average of 2.5 meters, and at one point almost 7 meters in less than one minute