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Geological Formation

Firth

Landform Concepts

A firth is a term in English and Scots used for various coastal waters in the United Kingdom, mostly in Scotland, generally referring to a broad estuary; it is linguistically related to the Scandinavian words fjord and fjard, both descending from a Proto-Germanic root meaning sailable waterway. Firths are more common on Scotland's east coast and in the southwest, with the Firth of Clyde as a western exception, while the similar inlets of the west Highland coast are usually called sea lochs instead. A firth typically forms from ice age glaciation acting on a river valley, with tidal seawater pushing upriver and eroding the riverbed wider into the estuary seen today.

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Caused By

Glaciation, Processes
Source Firth (Wikipedia)

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Source Firth (Wikipedia)
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Sources
Firth (Wikipedia)
  • In Discipline: Oceanography, Lead paragraph
    Firth is a word in the English and Scots languages used to denote various coastal waters in the United Kingdom, predominantly within Scotland
  • Caused By: Glaciation, Lead paragraph
    A firth is generally the result of ice age glaciation and is very often associated with a large river, where erosion caused by the tidal effects of incoming sea water passing upriver has widened the riverbed into an estuary
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