The Seafloor Spreading Process At Ridges Produces What Kind Of Faults

5 points starbae5758 asked 12 04 2017.

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

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. Previous question next question. Q 32 normal faults the seafloor spreading process at ridges produces normal faults. The seafloor spreading process at ridges produces what type of faults.

See answers 1 ask for details. They are the shallowest major features of the seafloor. Normal faults earlier we discussed the concept of isostasy where lower density rocks rise higher than higher density rocks. Normal faults earlier we discussed the concept of isostasy where lower density rocks rise higher than higher density rocks.

Eventually the crust cracks. Active transform faults are. Seafloor spreading helps explain continental drift in the theory of plate tectonics. The seafloor spreading process at ridges produces what kind of faults.

Ridges are formed by extensional forces occur in associatio view the full answer. Find an answer to your question the seafloor spreading process at ridges produces what kind of faults. The mid atlantic ridge and east pacific rise are examples of midocean ridges. Sea floor spreading occurs when the sea floor spreads apart along divergent boundaries and forms the mid ocean ridge.

Seafloor spreading occurs at divergent plate boundaries. Midocean ridges reach a typical summit elevation of 2 700 meters below sealevel. As the magma is thrust up and hardens it forms new crust and the ocean floor on both sides of the mid ocean ridge move outward. 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 less dense material rises often forming a mountain or elevated area of the seafloor. Magma is pushed up through cracks in the crust along the mid ocean ridge. Plates that are not subducting are driven by gravity sliding off the elevated mid ocean ridges a process called ridge push.