Hess proposed the idea that are places where.
The sea floor spreading theory was proposed by.
The phenomenon is known today as plate tectonics.
Theory that new seafloor formed when magma was forced upwards toward surface at mid ocean ridge.
Seafloor spreading and other tectonic activity processes are the result of mantle convection.
Seafloor spreading theory of lithospheric evolution that holds that the ocean floors are spreading outward from vast underwater ridges.
What evidence supports hess s theory of seafloor spreading.
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.
Naval electronics laboratory in san diego in the 1960s.
By the use of the sonar hess was able to map the ocean floor and discovered the mid atlantic ridge mid ocean ridge.
The pattern of magnetic strips shows that the seafloor is expanding at mid ocean ridges.
Harry hess princeton university scientist what does seafloor spreading help support.
He also found out that the temperature near to the mid atlantic ridge was warmer than the surface away from it.
Mantle convection is the slow churn ing motion of earth s mantle.
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.
The seafloor spreading hypothesis was proposed by the american geophysicist harry h.
Seafloor spreading was proposed by an american geophysicist harry h.
Hess its major tenets gave great support to the theory of continental drift continental drift.
Hess its major tenets gave great support to the theory of continental drift continental drift.
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.
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Who proposed the theory of seafloor spreading.
First proposed in the early 1960s by the american geologist harry h.