1.2 seafloor spreading Flashcards
(18 cards)
seafloor spreading
a process where magma from deep within the earth rises through mid ocean ridges to create new oceanic crust at divergent plate boundaries
landforms
formation on land due to plate movement
mid ocean ridge
a submarine mountain chain linearly located on the ocean floor at divergent plate boundaries
oceanic trench
deep depression found in the ocean floor where one oceanic plate is subducting beneath another plate
evidence of seafloor spreading
- where 2 oceanic plates move away from each other at divergent plate boundaries, seafloor spreading occurs
- magma from deep within the earth rises through the mid oceanic ridge
- new oceanic crust is formed
- overtime a mid oceanic ridge is formed. this is why divergent boundaries are also known as constructive boundaries.
- evidence of seafloor spreading
when two oceanic plates move away from each other at divergent plate boundaries, seafloor spreading occurs
- evidence of seafloor spreading
- magma from deep within the earth rises through the mid oceanic ridge
- evidence of seafloor spreading
new oceanic crust is formed
- evidence of seafloor spreading
overtime, a mid oceanic ridge is formed. this is why divergent boundaries are also known as constructive boundaries
description of age of rocks
- the age and distance of crust from the mid oceanic ridge has a direct relationship
- crust increase in age with increasing distance from the oceanic ridges and vice versa
explanation of age of rocks
- pattern supports the concept of seafloor spreading, where new crust is continuously created at the zone of divergent plate boundaries where oceanic ridges can be found
- as divergence continues, older crusts are pushed laterally outwards on both sides of the ocean ridge
- hence, the pattern shows that this is not a random or isolated occurrence and proving that plates move away
- explanation of age of rocks
the pattern supports the concept of seafloor spreading, where new crust is continuously created at the zone of divergent plate boundaries where oceanic ridges can be found
- explanation of age of rocks
as divergence continues, older crusts are pushed laterally outwards on both sides of the ocean ridges
- explanation of age of rocks
hence, the pattern shows that this is not a random or isolated occurrence and proving that plates move
description of limited sediment accumulation
as plates continue to move away from, the divergent boundary, little sediment accumulation is found at the convergent boundary at the oceanic trenches
explanation of limited sediment accumulation
- proving that new crust is continually formed at divergent boundaries at mid oceanic ridges and mover laterally, where older crust is destroyed at oceanic trenches
- hence oceanic crusts are usually younger than continental crust
- explanation of limited sediment accumulation
proving that new crust is continually formed at divergent boundaries at mid oceanic ridges and mover laterally, where older crust is destroyed at oceanic trenches
- explanation of limited sediment accumulation
hence oceanic crusts are usually younger than continental crusts