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diatom shells settle on the ocean floor from the surface
An isochron is a line on a map that connects points that have the same age. An isochron map of the ocean floor supports the theory of seafloor spreading because it shows the older rock near the deep sea trenches and the younger rocks near ocean ridges.
you can find the youngest rocks on the top of the ocean floor.
New floor forms and spreads from mid-ocean ridges
The seafloor rocks vary in different places. Rock samples near ocean ridges are younger than rocks at deep sea trenches
Alvin, Sonar , and underwater vessels
ocean technologies are used from like scientist objects to go into the ocean
minisubmarines
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the darkness and the weather condition
While studying the ocean floor, scientists found alternating bands of magnetism. Each band is magnetized with a polarity that is opposite the surrounding bands.
Ocean-floor spreading.
Through geomagnetic reversal whee they studying the magnetic properties of the seafloor.
Pictures, or scattered debris on the floor of the ocean appeared.
Pictures, or scattered debris on the floor of the ocean appeared.
They measure how far away the rock is from the mid-ocean ridge. The farther, the older.
Pictures, or scattered debris on the floor of the ocean appeared.