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'The '''Eighty Five East Ridge''' is a near-linear, aseismic, age-progressive ridge in the northeastern Indian Ocean. It is named for its near-parallel strike along the [[85th meridian east|85th meridian]]. Seismic studies have shown that the morphology of the ridge including its depth of occurrence varies along the ridge track and that in general the ridge has been buried beneath sediments deposited since the [[Oligocene]]. The ridge is associated with complicated gravity and magnetic signatures. The northern part of the ridge is buried beneath thick sediments of the [[Bengal Fan]] and shows a negative gravity anomaly. Ridge structures in the south occasionally rise above the sea floor and are associated with a positive gravity anomaly. The magnetic signatures associated with the ridge are complex, with alternate stripes of strong positive and negative anomalies. Magnetic modelling of the ridge suggests that it was emplaced over a period of rapid [[geomagnetic reversal]]s whereas the underlying oceanic crust was formed in a normal magnetic field of the [[Cretaceous Normal Superchron]] or "Cretaceous Quiet Period". The correlation of the magnetization pattern of the ridge and the geomagnetic polarity timescale suggests that the volcanism that created the ridge started ~80 Ma (magnetic chron time 33r ) in the [[Mahanadi Basin]] the process continued southwards, ending at ~55 Ma near the [[Afanasy Nikitin Seamount]]. The volcanism is thought to have been caused by a short-lived hotspot. ==References== {{reflist}} ==Further reading== {{coord missing}} [[Category:Underwater ridges of the Indian Ocean]]'