Sea Floor Age Data

The data is from four companion digital models of the age age uncertainty spreading rates and spreading asymmetries of the world s ocean basins.

Sea floor age data.

Scientists can determine the age of the seafloor by examining the changing magnetic field of our planet. Shortly after the conclusion of world war ii sonar equipped vessels crisscrossed the oceans collecting ocean depth profiles of the seafloor beneath them. This graphic shows several ocean floor features on a scale from 0 35 000 feet below sea level. Scientists use the magnetic polarity of the sea floor to determine the age.

This has happened many times throughout earth s history. Age of oceanic lithosphere. The age spreading rate and asymmetry at each grid node is determined by linear interpolation between adjacent seafloor isochrons in the direction of spreading. Seafloor spreading is a process that occurs at mid ocean ridges where new oceanic crust is formed through volcanic activity and then gradually moves away from the ridge.

Sio reference series 93 30 scripps institution of oceanography. The following features are shown at example depths to scale though each feature has a considerable range at which it may occur. Youngest red is along spreading centers. Switch to construct mode choose the geology data library and add the plate boundary types layer to your layer list.

It is called a geomagnetic reversal. Notice that the age will appear on the sea floor age m y legend located below the map. When scientists studied the magnetic properties of the. 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.

The ocean plates spread and grow in opposite directions so rocks that are equidistance from the center have the same magnetic polarity and age. The grids include data from all the major ocean basins as well as detailed reconstructions of back arc basins. Click and drag the layer above the sea floor age layer. Use the pointer tool to identify the age of the ocean floor moving away from the plate boundaries.

Very little of the sea floor is older than 150 million years. Continental shelf 300 feet continental slope 300 10 000 feet abyssal plain 10 000 feet abyssal hill 3 000 feet up from the abyssal plain seamount 6 000 feet. As the magma and lava cool at seafloor spreading centers whatever magnetic field is present get ingrained into the rock. The survey data was used to create three dimensional relief maps of the ocean floor and by 1953 american oceanic cartographer marie tharp had created the first of several maps that revealed the presence of an underwater mountain range.

Every so often it has occurred over 170 times over the past 100 million years the poles will suddenly switch. The age at each grid node was determined by linear interpolation between adjacent isochrons in the direction of spreading.