= J-Anomaly Ridge
{wiki=J-Anomaly_Ridge}
J-Anomaly Ridge is an underwater geological feature located in the central Atlantic Ocean. It is characterized by a significant positive geoid anomaly that is thought to result from a combination of geological factors, including variations in crustal thickness, mantle dynamics, and volcanic activity. The ridge is part of a broader system of underwater features that reflect the geological processes that shape the ocean floor, including seafloor spreading, tectonic activity, and sedimentation.
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