The time period “fjord” is of Norwegian origin, particularly from the Outdated Norse phrase “fjrr,” which suggests “a slender inlet of the ocean between excessive cliffs.”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