The challenger deep was formed when the Philippine plate and the pacific plate had a collision forced the heavier pacific plate down toward the mantle, and the edge of the Philippine plate was dragged down creating a steep walled trench.
The challenger deep was formed when the Philippine plate and the pacific plate had a collision forced the heavier pacific plate down toward the mantle, and the edge of the Philippine plate was dragged down creating a steep walled trench.
Challenger deep.
The challenger was able to protect the challenger deep by sleeping in the ground so far down.
The Challenger Deep is in the north Pacific, southwest of Guam.
Challenger deep is in the ocean, it was never explored by spacecraft.
Challenger Deep is a very deep spot on Mariana's Trench. Mariana's Trench is very long and Challenger Deep is just a tiny part of it, considered the deepest part.
the average temperature of challenger deep is 25 to 27 degrees Celsius (85 to 86 degrees Fahrenheit).
The Challenger Deep is the deepest known part of the seabed in the world. It is between 35,755 to 35,814 feet deep. It is at the southern end of the Mariana Trench in the Pacific Ocean.
Challenger Deep.
Challenger deep
It is in the Mariana Trench!
Marianas Trench