Age Of Sea Floor Map

An international scientific team recently published a new map of the ocean floor based on earth s gravity field and it is a particularly useful tool.

Age of sea floor map.

This map builds on the tectonic plates map by adding seafloor age data. The data are described in a data and analysis note in the journal of geophysical research 1997 entitled digital isochrons of the world s ocean floor. A marine gravity map of the north atlantic ocean red dots show locations of earthquakes with magnitude 5 5 and they highlight the present day location of the seafloor spreading ridges and. Most new crus t forms at these mid ocean spreading ridges.

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. New sea floor map for google earth january 13 2016 in late 2014 we had a look at a map of the ocean floor published by the scripps institution of oceanography university of california san diego. Note that the youngest seafloor ages are found at the mid ocean spreading ridges where new rock is constantly coming up from under the crust to heal the rifts formed as tectonic plates move away from one another. The following features are shown at example depths to scale though each feature has a considerable range at which it may occur.

The maps were created through computer analysis and modeling of new satellite data from esa s cryosat 2 and from the nasa cnes jason 1 as well as older data from missions flown in the 1980s and 90s. Measurements of the thickness of marine sediments and absolute age determinations of such bottom material have provided additional evidence for seafloor spreading. Therefore seafloor dating isn t that useful for studying plate motions beyond the cretaceous. A digital age map of the ocean floor.

Very little of the sea floor is older than 150 million years. Sio reference series 93 30 scripps institution of oceanography. The data is from four companion digital models of the age age uncertainty spreading rates and spreading asymmetries of the world s ocean basins. For that geologists date and study continental crust.

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. This graphic shows several ocean floor features on a scale from 0 35 000 feet below sea level. The age spreading rate and asymmetry at each grid node is determined by linear interpolation between adjacent seafloor isochrons in the direction of spreading.