The time period “fjord” is of Norwegian origin, particularly from the Previous Norse phrase “fjrr,” which suggests “a slim inlet of the ocean between excessive cliffs.” Fjords are characterised by their steep, glacially-carved sides and their lengthy, slim form.
Fjords are sometimes present in Norway, however they will also be present in different elements of the world, equivalent to Alaska, Canada, Chile, and New Zealand. They’re fashioned by the erosion of glaciers, which carve out deep channels within the rock. Over time, these channels are flooded by the ocean, creating fjords.
