By the use of the sonar hess was able to map the ocean floor and discovered the mid atlantic ridge mid ocean ridge.
The sea floor spreading theory was proposed by.
The pattern of magnetic strips shows that the seafloor is expanding at mid ocean ridges.
The idea that the seafloor itself moves and also carries the continents with it as it spreads from a central rift axis was proposed by harold hammond hess from princeton university and robert dietz of the u s.
Who proposed the theory of seafloor spreading.
What evidence supports hess s theory of seafloor spreading.
Naval electronics laboratory in san diego in the 1960s.
Seafloor spreading and other tectonic activity processes are the result of mantle convection.
Harry hess princeton university scientist what does seafloor spreading help support.
The phenomenon is known today as plate tectonics.
First proposed in the early 1960s by the american geologist harry h.
Seafloor spreading theory of lithospheric evolution that holds that the ocean floors are spreading outward from vast underwater ridges.
Seafloor spreading was proposed by an american geophysicist harry h.
Which statement accurately describes how magnetic stripes in ocean rock provide evidence of seafloor spreading.
Hess its major tenets gave great support to the theory of continental drift continental drift.
Seafloor spreading theory of lithospheric evolution that holds that the ocean floors are spreading outward from vast underwater ridges.
Seafloor spreading is a geologic process in which tectonic plate s large slabs of earth s lithosphere split apart from each other.
A mystery solved in 1912 when alfred wegener proposed that the continents had once been joined together and had split apart the biggest weakness in his hypothesis was the lack.
Hess proposed the idea that are places where.
Hess its major tenets gave great support to the theory of continental drift continental drift.
He also found out that the temperature near to the mid atlantic ridge was warmer than the surface away from it.
Check all that apply.
First proposed in the early 1960s by the american geologist harry h.
Theory that new seafloor formed when magma was forced upwards toward surface at mid ocean ridge.