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A sea loch is a tidal inlet of the sea which may range in size from a few hundred metres across to a major body of seawater several tens of kilometres in length and more than 2 or 3 kilometres wide. Other tidal inlets include firths , voes and bays.
Ria – Coastal inlet formed by the partial submergence of an unglaciated river valley; River delta – Silt deposition landform at the mouth of a river; Salt marsh – Coastal ecosystem between land and open saltwater that is regularly flooded; Sea cave – Cave formed by the wave action of the sea and located along present or former coastlines
These are long narrow inlets with steep sides or cliffs, created in a valley carved by glacial activity. In the 21st century, however, the preferred usage of ria by geologists and geomorphologists is to refer solely to drowned unglaciated river valleys. It therefore excludes fjords by definition, since fjords are products of glaciation. [2] [3] [4]
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Taiari / Chalky Inlet, and its arms: Moana-whenua-pōuri / Edwardson Sound; Te Korowhakaunu / Kanáris Sound [1] Rakituma / Preservation Inlet, and its arms: Isthmus Sound; Useless Bay; Te Awaroa / Long Sound; Lake Hakapoua (divided from sea by a landslide in 1915) [2] Many of the sounds and inlets were given dual names in 2019. [3]
Firth is a word in the English and Scots languages used to denote various coastal waters in the United Kingdom, predominantly within Scotland. In the Northern Isles, it more often refers to a smaller inlet. It is linguistically cognate to Scandinavian fjord and fjard (all from Proto-Germanic *ferþuz), with the original meaning of "sailable ...
The fiords of New Zealand (Māori: tai matapari "bluff sea" [1] [2]) are all located in the southwest of the South Island, in a mountainous area known as Fiordland. A fiord is a narrow inlet of the sea between cliffs or steep slopes, which results from marine inundation of a glaciated valley .