Linked from
The 12 pages that link to Continental slope, each with the reason it gives.
Continental shelfRelated: It marks the seaward boundary of the shelf.
Abyssal plainRelated: Its canyons and slopes channel sediment flows that can reach the plain.
Bathyal zoneRelated: Its descent forms much of the bathyal zone’s seafloor.
Continental riseRelated: The rise begins at the base of this steep descent.
Neritic zoneRelated: It begins beyond the shelf edge, where the neritic zone ends.
Spotted ratfishRelated: Spotted ratfish inhabit deep waters along this seabed zone.
Cusk-eelRelated: This habitat supports many deep-water cusk-eels.
Sea toadRelated: This seafloor setting includes habitats occupied by many chaunacids.