[go: up one dir, main page]
Wikipedia

Fjard

A fjard (Swedish: fjärd, IPA: [ˈfjæːɖ]) is a large open space of water between groups of islands or mainland in archipelagos. Fjards can be found along sea coasts, in freshwater lakes or in rivers. Fjard and fjord were originally the same word, and they generally meant sailable waterway. In Scandinavia, fjords dominate along the North Sea coast while fjards dominate the Baltic Sea coast.

The fjard of Somes Sound, Maine, USA.

Fjards vs. fjords vs. förden vs. rias

edit

Although fjards and fjords are similar in that they are a glacially-formed topography, they still differ in some key ways:

  • Fjords are characterized by steep high relief cliffs carved by glacial activity and often have split or branching channels.
  • Fjards are glacial depressions or valleys that have much lower reliefs than fjords. Fjards fill with eroded local materials which assist in "filling", along with rising sea levels since the last ice age contributing as well. Other low relief landforms that are only associated with fjards, such as mud flats, salt marshes, and flood plains,[1] further characterize the difference between fjords and fjards.
  • "Förden" of the German coast and the fjords of Danish eastern Jutland together form a third type of glacial inlet. They tend to occur along older 'beheaded' river channels and open into the tideless Baltic sea.
  • Rias are drowned valleys, such as the estuaries of Thames, Severn and Humber and the firths of Tay and Forth.

Examples

edit

Denmark

edit

Finland

edit
  • Airisto in the Turku Archipelago
  • Kihti between the Turku Archipelago and Åland
  • Porkkalanselkä west from Porkkala peninsula
  • Seurasaarenselkä and Kruunuvuorenselkä in Helsinki

Republic of Ireland

edit

Sweden

edit

United Kingdom

edit

Scotland

edit

Wales

edit

United States

edit

References

edit
  1. ^ ABPmer and HR Wallingford. 2007. Understanding and Managing Morphological Change in Estuaries, Ch. 3 of The Estuary-Guide: A website based overview of how to identify and predict morphological change within estuaries., Joint Defra/EA Flood and Coastal Erosion Risk Management R&D Programme. UK Department for Environment, Food, and Public Affairs.
  2. ^ a b c d e f Development_and_Demonstration_of_Systems_Based_Estuary_Simulators_-technical_Report.pdf (PDF). Department for Environment, Food and Rural Affairs. June 2009.
  3. ^ Bird, E.C.F., 2008, Coastal Geomorphology: An Introduction, 2nd ed. John Wiley and Sons Ltd. West Sussex, England. ISBN 978-0-470-51729-1
  4. ^ Cooper, J. A. G. (2006). "Geomorphology of Irish estuaries: inherited and dynamic controls". Journal of Coastal Research: 176–180. JSTOR 25741557.
  5. ^ Jackson, J.A., 1997, Glossary of Geology. American Geological Institute. Alexandria, Virginia. ISBN 0-922152-34-9
  6. ^ Goudie, A., 2004, Encyclopedia of Geomorphology. Routledge. London, England. ISBN 0-415-27298-X
Retrieved from "https://en.wikipedia.org/w/index.php?title=Fjard&oldid=1253985458"