How Long Does It Take to Get to the Bottom of the Mariana Trench?

The time required to reach the Challenger Deep, the deepest point on Earth, depends entirely on the technology used for the journey. Reaching this remote location at the bottom of the Mariana Trench requires a submersible designed to withstand conditions far more extreme than those found in any other part of the ocean. The duration of the journey is determined by a careful balance of engineering limitations, safety protocols, and the sheer distance involved in this unique underwater voyage.

Defining the Journey’s Endpoint

The destination of this journey is the Challenger Deep, a slot-shaped valley within the southern part of the Mariana Trench in the Western Pacific Ocean. This spot represents the deepest known point in the world’s oceans, plunging to an estimated 10,935 meters, or roughly 35,876 feet, below the surface of the sea.

The most significant factor making this environment challenging is the crushing hydrostatic pressure exerted by the water column above. At the bottom of the trench, the pressure exceeds 1,000 standard atmospheres, which translates to approximately 8 tons per square inch. Any vessel designed to transport humans or delicate equipment to this depth must contend with this physical reality, which dictates every aspect of the descent.

Factors Governing Descent Speed

The speed of a deep-sea submersible is not set by powerful engines but by the need for a controlled descent. Deep-diving vehicles are designed to be slightly heavier than the water they displace, overcoming the natural buoyancy of the ocean. They rely on heavy weights, ballast, to initiate and sustain the downward journey.

The descent is essentially a controlled fall, where speed must be limited to prevent structural failure and allow for necessary monitoring. Submersibles must descend slowly to continuously monitor the pressure hull for any signs of stress, material deformation, or leaks caused by the increasing external pressure. High-speed travel is not the priority; rather, the focus is on maintaining the structural integrity of the specialized steel or titanium sphere that protects the occupants.

Deep-sea submersibles are not equipped with high-powered vertical thrusters because the energy required to actively push against the immense water column at a high rate would be prohibitive. Instead, the small thrusters that are included are primarily used for minor adjustments to pitch and yaw, along with lateral movement once the vehicle reaches the seafloor. The speed of the dive is therefore a function of safety protocols and the amount of ballast used, which determines the rate of acceleration.

Actual Descent Timeframes

The time it takes to reach the bottom of the Mariana Trench is highly variable and depends on the specific technology and mission profile of the submersible. The first crewed descent in 1960, by the bathyscaphe Trieste, took nearly five hours to complete its journey to the seafloor, reaching a maximum depth of 35,814 feet. The slow rate was a necessity of the pioneering technology and the extreme caution required for a first-of-its-kind dive.

Modern, highly optimized manned vehicles have drastically reduced this time. For example, James Cameron’s solo dive in the Deepsea Challenger in 2012 was able to achieve the descent in approximately two and a half hours. This significantly faster time was due to the submersible’s lighter weight, advanced materials like specialized foam for buoyancy, and a more streamlined design built for a rapid, controlled drop.

Unmanned scientific probes and robotic landers are often designed with speed in mind and can sometimes reach the bottom in a time frame comparable to the Deepsea Challenger, often between three and four hours. These robotic platforms can sometimes tolerate higher descent rates since there is no human life at risk, but they still require time for data transmission and navigational adjustments. The return trip, or ascent, typically takes a similar amount of time to the descent, as the vehicle must release its ballast and rely on its natural buoyancy to rise at a controlled rate.