Want this question answered?
They increase in age and density, and decrease in temperature.
Ocean ridges is somewhat vague. Mid-ocean mountains are more precisely called mid-ocean ridges, so it seems like someone is trying to trip you up. The best evidence of seafloor spreading among the choices would be mid-ocean mountains. They are the buoyant, hot, new crust that is formed at the divergent plates of the world's oceans.
The oldest rocks on the continents would be much older than the rocks on the sea floor because the rocks on the continents are not being removed unlike the rocks on the sea floor that are made by the mid-ocean ridge are being removed by deep ocean trenches. this prossess that is occuring on the sea floor is called sea floor spreading. evidence of this is the Pacific ocean shrinking and the Atlantic ocean growing.
Magnetic Reversal
sediment cores
Drilling.
Age of seafloor rock and sediment increases with distance from the oceanic ridges.
age increases
They increase in age and density, and decrease in temperature.
Through geomagnetic reversal whee they studying the magnetic properties of the seafloor.
The further from the ridge, the older the oceanic crustal rock.
age increases
seafloor spreading, age of the sea floor and ocean trenches.
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.
Rocks in the seafloor are moving one place to another
The Atlantic Ocean seafloor has what appear to be "stretch marks" or creases branching out horizontally from the center of the ocean. The seafloor deepens (generally) from both sides up to 20,000 ft. until a central upward ridge is formed (Mid-Atlantic Ridge), running up the middle of the ocean between the western and eastern continents. In some places this ridge is only a few thousand feet deep. The Atlantic also has a few deep basins scattered throughout that are substantially deeper than the surrounding ocean. Some researchers report core samples taken of the seafloor crust show the age of the seafloor increasing as you travel away from the coastline, suggesting the seafloor has expanded outward from the central ridge over time.
the ocean basins are relatively young: no sea floor with the excess of age of 180mllion years