Constituting the deepest points in the Atlantic Ocean, the trench is 810 kilometres (503 mi) long[7] and has a maximum documented depth between 8,376 metres (27,480 ft)[8] and 8,740 metres (28,675 ft).[7][9] The deepest point is commonly referred to as the Milwaukee Deep, with the Brownson Deep naming the seabed surrounding it.[10] However, more recently, the latter term has also been used interchangeably with the former to refer to this point.[11][12][13] The exact point was identified by the DSSV Pressure Drop using a state-of-the-art Kongsberg EM124 multibeam sonar in 2018, and then directly visited and its depth verified by the crewed submersible Deep-Submergence Vehicle DSV Limiting Factor (a Triton 36000/2 model submersible) piloted by Victor Vescovo.[14][15][16]
Scientific studies have concluded that an earthquake occurring along this fault zone could generate a significant tsunami.[17] The island of Puerto Rico, which lies immediately to the south of the fault zone and the trench, suffered a destructive tsunami soon after the 1918 San Fermín earthquake.
^Lidiak, Edward G.; Anderson, Thomas H. (2015). "Evolution of the Caribbean plate and origin of the Gulf of Mexico in light of plate motions accommodated by strike-slip faulting". GeoScienceWorld. Geological Society of America Special Papers. 513. Geological Society of America: 1–88. doi:10.1130/2015.2513(01). ISBN978-0-8137-2513-0. S2CID131933179.