The time period “fjord” is of Norwegian origin, particularly from the Previous Norse phrase “fjrr,” which implies “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 may also be present in different components of the world, corresponding 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.
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