The Seafloor Spreading Process At Ridges Produces What Kind Of Faults

Seafloor spreading helps explain continental drift in the theory of plate tectonics.

The seafloor spreading process at ridges produces what kind of faults.

The seafloor spreading process at ridges produces what type of faults. Normal faults earlier we discussed the concept of isostasy where lower density rocks rise higher than higher density rocks. Eventually the crust cracks. Q 32 normal faults the seafloor spreading process at ridges produces normal faults.

Magma is pushed up through cracks in the crust along the mid ocean ridge. Find an answer to your question the seafloor spreading process at ridges produces what kind of faults. The seafloor spreading process at ridges produces what kind of faults. 5 points starbae5758 asked 12 04 2017.

Active transform faults are. Plates that are not subducting are driven by gravity sliding off the elevated mid ocean ridges a process called ridge push. The less dense material rises often forming a mountain or elevated area of the seafloor. Seafloor spreading occurs at divergent plate boundaries.

See answers 1 ask for details. Ridges are formed by extensional forces occur in associatio view the full answer. Sea floor spreading occurs when the sea floor spreads apart along divergent boundaries and forms the mid ocean ridge. Normal faults earlier we discussed the concept of isostasy where lower density rocks rise higher than higher density rocks.

Seafloor spreading is a process that occurs at mid ocean ridges where new oceanic crust is formed through volcanic activity and then gradually moves away from the ridge. Seafloor spreading takes place at midocean ridges and produces basalt the rock that makes up the oceanic crust. The motivating force for seafloor spreading ridges is tectonic plate slab pull at subduction zones rather than magma pressure although there is typically significant magma activity at spreading ridges. The mid atlantic ridge and east pacific rise are examples of midocean ridges.

They are the shallowest major features of the seafloor. Midocean ridges reach a typical summit elevation of 2 700 meters below sealevel. The seafloor spreading process at ridges produces what kind of faults.