Explore Höga Kusten

The marine realm of the High Coast

The Marine Realm

The marine realm of the High Coast

The biological character of the High Coast's marine environment is a consequence of several major controlling influences such as: brackish waters of very low salinity; the most sharply contoured submarine topography in the Baltic, extending to depths in excess of 200m close inshore; little tidal influence, with shifting water levels determined mainly by changing weather conditions of air pressure and wind; and seasonal ice cover.

Natural environments have undergone dramatic changes since glacial times, passing through marine, brackish and freshwater conditions. The resultant mosaic of shallow, sheltered embayments and deep, open waters provides a range of habitats for a mix of marine, brackish and freshwater species, low in species diversity but high in population numbers for some macrofauna species. Some species are relics of earlier periods, and others are at the extremes of their latitudinal and environmental limits. For the most part, however, the marine biota are described as being typical and representative of that found throughout the Baltic, rather than special or unique.

 

The special feature of the marine realm, imparting the greatest scientific significance, is that it represents the submarine extension of the topographical continuum of landscapes undergoing isostatic uplift.

Continual elevation of the land results in inlets becoming progressively cut off from the sea, transforming them into estuaries and ultimately lakes (some of which retain their name as bays). Meanwhile, shorelines are constantly reshaped, new islands are born offshore, and others become peninsulas as they unite with the mainland. The terrestrial influence progressively extends seawards into the Bothnian Sea. This process has major effects for the associated plants and animals that must constantly adapt to the changing environments. Thus, the nearshore marine area constitutes an integral part of the ongoing geological evolution of the High Coast and, as such, it is an important natural component of the entire property.

Although the 56% of the size of the High Coast site is marine, only 2% of it is protected: only 15 km2 of the 800 km2 marine component of the area is under protective status.
(Font: UNESCO - World Heritage Nomination - The High Coast (Sweden) - Addendum to 1999 IUCN Technical Evaluation)

The marine realm of the High Coast

The High Coast's terrestrial fauna is typical for the region, but the range of marine habitats provides for a mix of marine, brackish and freshwater species. These are low in diversity but high in populations for some of the macrofauna, some of which are relicts of earlier periods, others at the extremes of their latitudinal and environmental distribution (Dingwall, 2000). All are tolerant of the varying salinity of the brackish water, which off the High Coast ranges between 3 and 6 ‰. There is a major sill across the bottom of the Kvarken Straits at about 25m. Species numbers decline abruptly at the Gulf’s entrance from the Baltic and continue to decrease northwards - from 41 fish species in the Baltic to 20 species in the Gulf and only 6 in the Bay of Bothnia. The consequence is that the northern part of the site is near the northern limit of several species. Two northeastern Atlantic seals are present in the waters off the High Coast, the ringed seal Phoca hispida and the grey seal Halichoerus grypus. The latter occurs in greater numbers, although there are no suitable haul-out areas for the large gatherings of grey seals which are found in the Northern Quark Archipelago and south of the High Coast.

The marine realm of the High Coast

Saltwater and fresh water fish species regularly occur and reproduce along the High Coast within shallow and deep-water areas of the Archipelago. Warm-water species found in shallow waters include perch Perca fluviatilis and roach Rutilus rutilus. Cold-water species of fresh and salt-water origin are the white fish Baltic herring Clupea harengus, salmon Salmo salar, four-horned sculpin and eel pout Zoarces viviparus. Immigrant species include sprat Sprattus sprattus, cod Gadus morhua (VU) and European flounder Platichthys flesus.  Fish are only found in deeper waters in the summer. Shoreline fauna species include the acorn barnacle Balanus improvisus, the common mussel Mytilus edulis, the coralline Electra crustukenta and thefreshwater snail Theodoxus fluviatilis. Shallow water crustaceans include the amphiopods Gammarus zaddachi, G. oceanicus at its northern limit, G. salinus, Pallaseaquadrispinosa, a relict species primarily found in fresh water and Corophium volutator. Several snail species are foundin the mid-archipelago zone: Paludestrina jenkinsi, Theodoxus fluviatilis, Lymnaea peregra and Bithynia tentaculata. The benthic fauna of the deeper waters is dominated by a small number of species. These include the isopod Saduria entomon, the amphipod Monoporeia affinis, the Baltic mussel Macoma bathica, a few semi-pelagic opossum shrimp species (Mysidae) and the common sea snail Liparis liparis. (Font: UNEP-WCMC)

Explore the High Coast with your boat - link back to the main post

Explore the High Coast on your boat

The Höga Kusten is World Heritage also for sailing

The High Coast (Höga Kusten) / Kvarken Archipelago world heritage site

View of the Norrfjärden from the top of Skuleberget

2000: The whole High Coast area was inscribed on the World Heritage List and granted World Heritage status. The area has the largest land uplift of its kind in the world, which was a key reason for the designation of the High Coast as a World Heritage Site.

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The High Coast (Sweden) is located on the west shore of the Gulf of Bothnia, a northern extension of the Baltic Sea.
The area covers 142,500 ha including a marine component of 80,000 ha, which includes a number of offshore islands.
The irregular topography of the region - a series of lakes, inlets and flat hills rising to 350 m - has been largely shaped by the combined processes of glaciation, glacial retreat and the emergence of new land from the sea. Since the last retreat of the ice from the High Coast 9,600 years ago, the uplift has been in the order of 285 m which is the highest known 'rebound'. The High Coast site affords outstanding opportunities for the understanding of the important processes that formed the glaciated and land uplift areas of the Earth's surface. (Font: UNESCO - More info at http://whc.unesco.org/en/list/898) 
 

 
In July 2006, the Kvarken Archipelago was inscribed on the World Heritage List, as an extension to the Sweden's High Coast (Höga Kusten). It is the first UNESCO's Natural Heritage Site in Finland. Together, these two areas form a complementary geological complex featuring land uplift unlike anything found elsewhere in the world.

 
 
The Kvarken Archipelago, the finnish side extension of the High Coast World Heritage

The Kvarken Archipelago (Finland) numbers 5,600 islands and islets and covers a total of 194,400 ha (15% land and 85% sea). It features unusual ridged washboard moraines, "De Geer moraines", formed by the melting of the continental ice sheet, 10,000 to 24,000 years ago. The Archipelago is continuously rising from the sea in a process of rapid glacio-isostatic uplift, whereby the land, previously weighed down under the weight of a glacier, lifts at rates that are among the highest in the world. As a consequence of the advancing shoreline, islands appear and unite, peninsulas expand, lakes evolve from bays and develop into marshes and peat fens. This property is essentially a "type area" for research on isostasy; the phenomenon having been first recognized and studied here. We congratulate Finland with the inscription of Kvarken on the World Heritage List! (from: Nordic World Heritage Foundation - Newsletter August 2006)
Photo on the left: Tuukka Pahtamaa ©

Land uplift in the Kvarken is very intense and the archipelago is constantly changing shape. New islands emerge from the sea, bays are transformed into lakes and shipping lanes become shallower. Since the land surface increases by a hundred hectares a year, these changes can be noticed during one generation. See more about "The Kvarken Archipelago - a World Heritage" at the Finnish Ministry of the Environment website. And here is the link to The Kvarken region picture gallery. But don't miss to visit The Kvarken Nature Guide!
 
Both High Coast and Kvarken Archipelago are inscribed on the World Heritage List under Natural Criterion viii: "to be outstanding examples representing major stages of earth's history, including the record of life, significant on-going geological processes in the development of landforms, or significant geomorphic or physiographic features".

They are also legally gazetted as "protected landscape/seascape" of IUCN management categories.

The distance between the areas is 150 kilometres.

See also: The Kvarken Archipelago and The High Coast World Heritage Site at www.kvarken.fi.

Explore the High Coast with your boat - link back to the main post

Explore the High Coast on your boat

The Höga Kusten is World Heritage also for sailing