The Seafloor Spreading Process At Ridges Produces What Kind Of Faults

Sea floor spreading occurs when the sea floor spreads apart along divergent boundaries and forms the mid ocean ridge.
The seafloor spreading process at ridges produces what kind of faults. Previous question next question. Eventually the crust cracks. Seafloor spreading helps explain continental drift in the theory of plate tectonics. Ridges are formed by extensional forces occur in associatio view the full answer.
As tectonic plates slowly move away from each other heat from the mantle s convection currents makes the crust more plastic and less dense. Find an answer to your question the seafloor spreading process at ridges produces what kind of faults. See answers 1 ask for details. The less dense material rises often forming a mountain or elevated area of the seafloor.
5 points starbae5758 asked 12 04 2017. Normal faults earlier we discussed the concept of isostasy where lower density rocks rise higher than higher density rocks. The mid atlantic ridge and east pacific rise are examples of midocean ridges. They are the shallowest major features of the seafloor.
Seafloor spreading takes place at midocean ridges and produces basalt the rock that makes up the oceanic crust. Midocean ridges reach a typical summit elevation of 2 700 meters below sealevel. Q 32 normal faults the seafloor spreading process at ridges produces normal faults. The seafloor spreading process at ridges produces what type of faults.
The seafloor spreading process at ridges produces what kind of faults. Plates that are not subducting are driven by gravity sliding off the elevated mid ocean ridges a process called ridge push. Normal faults earlier we discussed the concept of isostasy where lower density rocks rise higher than higher density rocks. Active transform faults are.
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. Seafloor spreading occurs at divergent plate boundaries. Magma is pushed up through cracks in the crust along the mid ocean ridge.