The Mariana Trench is a deep sea trench just off the East coast of the Phillipines and it is the deepest trench in the oceans of the world. The deepest part of the Mariana Trench is the Challenger Deep, so named after the exploratory vessel HMS Challenger II; a fishing boat converted into a sea lab by the Swiss scientist Jacques Piccard. At this point, the Mariana Trench is 6033.5 fathoms deep, which is 11 033 meters, or 36 201 feet deep.
To be able to imagine the actual depth of the Mariana Trench, consider this; if Mount Everest, which is the tallest point on Earth at 8 850 meters (29 035 feet), picked up and put down inside the Mariana Trench, there would still be 2 183 meters (7 166 feet) of water left above it.
The Mariana Trench was formed when the oceanic crust, a heavy dense crust, collided with the continental crust, which is lighter. At the collision, the heavier oceanic plate, moves downwards towards the molten mantle of the Earth and the ocean trench is formed at the bottom of the trench created by the subducting ocean crust.
To be able to imagine the actual depth of the Mariana Trench, consider this; if Mount Everest, which is the tallest point on Earth at 8 850 meters (29 035 feet), picked up and put down inside the Mariana Trench, there would still be 2 183 meters (7 166 feet) of water left above it.
The Mariana Trench was formed when the oceanic crust, a heavy dense crust, collided with the continental crust, which is lighter. At the collision, the heavier oceanic plate, moves downwards towards the molten mantle of the Earth and the ocean trench is formed at the bottom of the trench created by the subducting ocean crust.