The age of different rocks on earth s surface e.
Theory of sea floor spreading.
Seafloor spreading helps to explain continental drift in the theory of plate tectonics.
What evidence supports hess s theory of seafloor spreading.
When oceanic plates diverge tensional stress causes fractures to occur in the lithosphere.
Sea floor spreading theory.
As upwelling of magma continues the plates continue to diverge a process known as seafloor spreading samples collected from the ocean floor show that the age of oceanic crust increases with distance from the spreading centre important evidence in favour of this process.
As per seafloor spreading theory the mid oceanic ridge is the region where at the crest of oceanic ridges through the rupture of the oceanic crust and the crack continuous new lava eruption thrusts into it consequently pushing the oceanic crust on either side.
It leads to the formation of new material on the ridge.
Seafloor spreading proves that the ocean itself is a site of tectonic activity.
Seafloor spreading theory of lithospheric evolution that holds that the ocean floors are spreading outward from vast underwater ridges.
First proposed in the early 1960s by the american geologist harry h.
Check all that apply.
Pillow shaped rocks found in the sea.
The plates on either side of the.
Supporters of continental drift originally theorized that the continents moved drifted through unmoving oceans.
Seafloor spreading is a geologic process where there is a gradual addition of new oceanic crust in the ocean floor through a volcanic activity while moving the older rocks away from the mid oceanic ridge.
These age data also allow the rate of seafloor spreading to be determined and they show that rates.
Seafloor spreading disproves an early part of the theory of continental drift.
The direction iron in ocean rocks points d.
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.
Arthur holmes in 1930s discussed the possibility of convection currents.
Hess its major tenets gave great support to the theory of continental drift continental drift geological theory that the relative positions of the continents on the earth s surface have.
These cornerstones are convectional current theory and paleomagnetism.
The motivating force for seafloor spreading ridges is tectonic plate slab pull at subduction zones rather than magma pressure although there is typically.
Convection current theory convection current theory is the soul of seafloor spreading theory.
According to hess s theory what might happen if the magma under a mid ocean ridge cools.
This idea played a pivotal role in the development of the theory of plate tectonics which revolutionized geologic thought during the last quarter of the 20th century.
