Kings Trough is a significant underwater geological feature located in the northern part of the Atlantic Ocean, specifically in the North Atlantic Ocean. It is a deep-sea trough that separates the King Charles Rise to the south from the Greenland continental margin to the north. The feature is known for its depth and is often studied in the context of oceanography, marine geology, and tectonics. It is also of interest for understanding ocean currents, marine ecosystems, and the interaction between tectonic plates.
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