Its peak lies at the depth of  and it rises  above the surrounding seafloor, which is located at the depth of up to  and is a part of the Herodotus Abyssal Plain. It is one of the largest features on the Eastern Mediterranean seafloor.
This feature's highest point is situated at a depth of  and it protrudes  above the surrounding seafloor, which extends down to depths of up to  and is part of the larger Herodotus Abyssal Plain. It is a notable characteristic on the Eastern Mediterranean seafloor.