Oceanic mountains are formed from the rocks of sea-bed that rises above the sea-level to its peak height.
We are given that the base of the mountain or the depth underneath the sea-level from where the mountain was formed as:
The total height/rise of the mountain is given to us as:
We are to determine the portion of the height that is visible above the sea-level! We know that the mountain base formation starts from below the sea-level at a certain depth ( d ) and the total height ( H ) of the mountain. We can express the portion of height ( h ) that is above sea-level mathematically as follows:
We will plug in the respective values given to us and solve for ( h ):
The elevation of mountain above sea-level to its peak height is given as: