Estimated Age Of Sea Floor

In essence oceanic plates are more susceptible to subductionas they get older.

Estimated age of sea floor.

164 million years years show formulas for calculations with units 622 896 000 cm 3 8 cm yr. Therefore the age of the ocean floor is not an accurate tool to measure the age of the earth. Rate of spreading distance the sea floor moved length of time or r d t generally expressed as cm yr. To determine the age of the ocean basin divide the distance in centimeters separating the continental shelves by the rate of sea floor spreading for the atlantic ocean basin.

The depth predicted by the square root of seafloor age derived above is too deep for seafloor older than 80 million years. The age spreading rate and asymmetry at each grid node is determined by linear interpolation between adjacent seafloor isochrons in the direction of spreading. The oldest seafloor has been radiometrically dated to only about 200 million years duxbury et al. This has happened many times throughout earth s history.

The cooling plate model explains the age depth observations best for seafloor older that 20 million years. The tectonic plates are constantly in motion and new surfaces are always being created. Age of the north atlantic ocean basin. 2005 114 whereas continental rocks have been dated to four billion years and the earth is thought to be about 4 6 billion years old dalrymple 2004.

Every once in a while the currents in the liquid core which create the earth s magnetic field reverse themselves. Very little of the sea floor is older than 150 million years. Depth is better explained by a cooling lithosphere plate model rather than the cooling mantle half space. The cooling mantle model explains the age depth observations for seafloor younger that 80 million years.

Ages for ocean floor between the oldest identified magnetic anomalies and continental crust are interpolated by geological estimates of the ages of passive continental margin segments. The plate has a constant temperature at its base and spreading edge. Ages for ocean floor between the oldest identified magnetic anomalies and continental crust are interpolated by geological estimates of the ages of passive continental margin segments. Scientists can determine the age of the seafloor by examining the changing magnetic field of our planet.

This is because the oldest sea floor is subducted under other plates and replaces by new surfaces. Because of this correlation between age and subduction potential very little ocean floor is older than 125 million years and almost none of it is older than 200 million years. Scientists use the magnetic polarity of the sea floor to determine the age. It is called a geomagnetic reversal.

The age spreading rate and asymmetry at each grid node are determined by linear interpolation between adjacent seafloor isochrons in the direction of spreading.