Seafloor spreading is the process of splitting apart of tectonic plate
The process illustrated by the area labeled G in figure 9–1 is subduction
D. Subduction
Strips of alternating magnetic polarities is found in rocks in the ocean basins;
D. Provide evidence for sea floor spreading
Reason:
Subduction is a process in geology that occur where two plates converge
(usually ocean ocean plate convergence or oceanic continental
convergence) such that lithosphere of one plate is subducted or dives
beneath a less dense plate into the mantle, where it is recycled
The observations of the strips located on the ocean floor are as follows;
- The stripes of opposite polarities alternates
- The stripes on either sides of the mid-ocean ridges are a reflection of each other
- There is an abrupt end of the stripes at continental edges
The above observation are an evidence of seafloor spreading
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