Skerry

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Skerry outside Krottoy in Harstad municipality, Norway Skerry in shallow water.jpg
Skerry outside Krøttøy in Harstad municipality, Norway
Skerries which are part of Aland, Finland Archipelago062009.jpg
Skerries which are part of Åland, Finland
Passing a skerry off Garibaldi, Oregon, United States

A skerry is a small rocky island, or islet, usually too small for human habitation. It may simply be a rocky reef. A skerry can also be called a low sea stack. [1]

Contents

A skerry may have vegetative life such as moss and small, hardy grasses. They are often used as resting places by animals such as seals and birds.

Etymology

The term skerry is derived from the Old Norse sker, which means a rock in the sea (which in turn derives from the Proto-Indo-European root *sker-, "cut", in the sense of a rock cut off from the land). [2] The Old Norse term sker was brought into the English language via the Scots language word spelled skerrie or skerry. It is a cognate of the Scandinavian languages' words for skerryIcelandic, Faroese : sker, Danish : skær, Swedish : skär, Norwegian : skjær / skjer, found also in German : Schäre, Finnish : kari, Estonian : skäär, Latvian : šēra, Lithuanian : Šcheras and Russian : шхеры (shkhery). In Scottish Gaelic, it appears as sgeir, e.g. Sula Sgeir, in Irish as sceir, in Welsh as sgeri, and in Manx as skeyr.

Formation

Skerries are most commonly formed at the outlet of fjords where submerged glacially formed valleys at right angles to the coast join with other cross valleys in a complex array. In some places near the seaward margins of fjorded areas, the ice-scoured channels are so numerous and varied in direction that the rocky coast is divided into thousands of island blocks, some large and mountainous, while others are merely rocky points or rock reefs that menace navigation.

Examples

Islets and skerries in Loch Uisgebhagh, east of Benbecula, Outer Hebrides Loch Uisgebhagh.jpg
Islets and skerries in Loch Uisgebhagh, east of Benbecula, Outer Hebrides

The island fringe of Norway is such a group of glacially formed skerries, called a skjærgård (sometimes translated into English as archipelago, but specifically one near the coast of the mainland). Many of the cross fjords are so arranged that they parallel the coast and provide a protected channel behind an almost unbroken succession of rocky islands and skerries. By this channel one can travel through a protected passage almost the entire 1,600 km (1,000 mi) route from Stavanger to North Cape, Norway. The Blindleia is a skerry-protected waterway that starts near Kristiansand in southern Norway and continues past Lillesand.

The Inside Passage provides a similar route from Seattle, Washington, to Skagway, Alaska, United States. Another such skerry-protected passage extends from the Straits of Magellan north for 800 km (500 mi) along the west coast of the South American continent.

The Swedish coast along Bohuslän is likewise guarded by skerries. Even the east coast of Sweden, in the Baltic Sea, has many big skärgårdar (archipelagos), notably Stockholm Archipelago.

The southwestern coast of Finland also has a great many skerries; so many, in fact, that they form an archipelago. This area is experiencing post-glacial rebound that connects the rising islands as they break sea level, revealing till deposits and eventually clay bottoms. The skerries exist as small rocky islands before uplift of adjacent terrain changes the classification of this landform into a tombolo. [3]

In the Russian Federation, the best examples are the Minina Skerries, located in the Kara Sea, in the western shores of the Taymyr Peninsula, and the Sumsky Skerries, located in the White Sea.

The United Kingdom has a large number of skerries including Staple Island (an outer Farne Island) in England; a small rocky outcrop near the Fowlsheugh in northeast Scotland; numerous reefs in the Hebrides such as Dubh Artach and Skerryvore; and The Skerries, located off the Antrim coast of Northern Ireland.

Skerries is the name of a coastal area of Dublin, Ireland, with many skerries offshore, including Rockabill, Shenick Island, Colt Island and St Patrick's Island.

Related Research Articles

<span class="mw-page-title-main">Kattegat</span> Sea area between Denmark and Sweden

The Kattegat is a 30,000 km2 (12,000 sq mi) sea area bounded by the Jutlandic peninsula in the west, the Danish Straits islands of Denmark and the Baltic Sea to the south and the provinces of Bohuslän, Västergötland, Halland and Skåne in Sweden in the east. The Baltic Sea drains into the Kattegat through the Danish Straits. The sea area is a continuation of the Skagerrak and may be seen as a bay of the North Sea, but in traditional Scandinavian usage, this is not the case.

<span class="mw-page-title-main">Vänern</span> Largest lake in Sweden

Vänern is the largest lake in Sweden, the largest lake in the European Union and the third-largest lake in Europe after Ladoga and Onega in Russia. It is located in the provinces of Västergötland, Dalsland, and Värmland in the southwest of the country. With its surface located at 44 metres (144 ft) with a maximum depth of 106 metres (348 ft), the lowest point of the Vänern basin is at 62 metres (203 ft) below sea level. The average depth is at a more modest 28 metres (92 ft), which means that the average point of the lake floor remains above sea level.

<span class="mw-page-title-main">Fjord</span> Long, narrow inlet with steep sides or cliffs, created by glacial activity

In physical geography, a fjord or fiord is a long, narrow sea inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Antarctica, British Columbia (Canada), Chile, Denmark, Germany, Greenland (Denmark), the Faroe Islands (Denmark), Montenegro, Iceland, Ireland, Kamchatka (Russia), the Kerguelen Islands (France), Newfoundland and Labrador (Canada), New Zealand, Norway, Novaya Zemlya (Russia), Nunavut (Canada), Quebec (Canada), Argentina, Russia, South Georgia Island, Tasmania (Australia), Scotland and the states of Washington, Maine, and Alaska. Norway's coastline is estimated to be 29,000 km (18,000 mi) long with its nearly 1,200 fjords, but only 2,500 km (1,600 mi) long excluding the fjords.

<span class="mw-page-title-main">Nordland</span> County of Norway

Nordland is a county in Norway in the Northern Norway region, the least populous of all 11 counties, bordering Troms og Finnmark in the north, Trøndelag in the south, Norrbotten County in Sweden to the east, Västerbotten County to the south-east, and the Atlantic Ocean to the west. The county was formerly known as Nordlandene amt. The county administration is in the town of Bodø. The remote Arctic island of Jan Mayen has been administered from Nordland since 1995. In the southern part of the county is Vega, listed on the UNESCO World Heritage Site list.

<span class="mw-page-title-main">Bohuslän</span> Historical province of Sweden

Bohuslän is a Swedish province in Götaland, on the northernmost part of the country's west coast. It is bordered by Dalsland to the northeast, Västergötland to the southeast, the Skagerrak arm of the North Sea to the west, and the county of Østfold, in Norway, to the north. In English it literally means Bohus County, although it shared counties with the city of Gothenburg prior to the 1998 county merger and thus was not an administrative unit in its own right.

<span class="mw-page-title-main">Skagerrak</span> Sea between Denmark, Norway and Sweden

The Skagerrak is a strait running between the Jutland peninsula of Denmark, the east coast of Norway and the west coast of Sweden, connecting the North Sea and the Kattegat sea.

<span class="mw-page-title-main">Sound (geography)</span> A long, relatively wide body of water, connecting two larger bodies of water

In geography, a sound is a smaller body of water usually connected to a sea or an ocean. A sound may be an inlet that is deeper than a bight and wider than a fjord; or a narrow sea channel or an ocean channel between two land masses, such as a strait; or also a lagoon between a barrier island and the mainland.

The Out Skerries are an archipelago of islets, some inhabited, in Shetland, Scotland, and are the easternmost part of Shetland. Locally, they are usually called Da Skerries or just Skerries.

Torsa is one of the Slate Islands in Argyll and Bute, Scotland. Lying east of Luing and south of Seil, this tidal island was inhabited until the 1960s. There is now only one house there, which is used for holiday lets. The underlying bedrock is slate but unlike Torsa's immediate island neighbours this has never been worked commercially. The island's name is of Norse origin but the most prominent historical structure on the island is the ruined Caisteal nan Con on the northeast shore, once held by Clan Campbell. The abundant sea life in the waters surrounding the island are protected by the Loch Sunart to the Sound of Jura Marine Protected Area.

<span class="mw-page-title-main">Hyskeir</span> Islet in Scotland

Hyskeir or Heyskeir is a low-lying rocky islet in the Inner Hebrides, Scotland. The Hyskeir Lighthouse marks the southern entrance to the Minch.

<span class="mw-page-title-main">Archipelago Sea</span> Part of the Baltic Sea

The Archipelago Sea is a part of the Baltic Sea between the Gulf of Bothnia, the Gulf of Finland and the Sea of Åland, within Finnish territorial waters. By some definitions it contains the largest archipelago in the world by the number of islands, although many of the islands are very small and tightly clustered.

<span class="mw-page-title-main">The Skerries, Isle of Anglesey</span> Group of rocky islets in Wales

The Skerries, coming from the Old Norse word sker, are a group of sparsely vegetated rocky islets (skerries), with a total area of about 17 hectares lying 3 kilometres (1.9 mi) offshore from Carmel Head at the northwest corner of Anglesey, Wales. The islands are important as a breeding site for seabirds, and they attract divers, who come to visit the numerous shipwrecks. The Skerries Lighthouse sits atop the highest point in the islands.

<span class="mw-page-title-main">Sula Sgeir</span> Island in Outer Hebrides, Scotland, UK

Sula Sgeir is a small, uninhabited Scottish islet in the North Atlantic, 18 kilometres west of Rona. One of the most remote islands of the British Isles, it lies approximately forty nautical miles north of Lewis and is best known for its population of gannets. It has a narrow elongated shape running north-northeast to south-southwest, and is approximately 900 m long by typically 100 m wide.

<span class="mw-page-title-main">Archipelago National Park</span>

Archipelago National Park is a national park in Southwest Finland. It was established in 1983 and includes 500 km2 (190 sq mi) of land area. Most of the land is on islands smaller than 1 km2 (0.39 sq mi). The park encompasses about 2,000 of the 8,400 islets and skerries within the cooperative area. The larger islands are mainly owned by their inhabitants. Archipelago National Park is part of the UNESCO biosphere reserves and received a PAN Parks certificate in 2007.

<span class="mw-page-title-main">Yell Sound</span>

Yell Sound is the strait running between Yell and Mainland, Shetland, Scotland. It is the boundary between the Mainland and the North Isles and it contains many small islands. Sullom Voe, on the shores of which is a substantial oil terminal, is an arm of Yell Sound.

<span class="mw-page-title-main">Fjard</span> Glacially formed, broad, shallow inlet

A fjard 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 rivers. Fjard and fjord were originally the same word with the general meaning of sailable waterway. In Scandinavia, fjords dominate along the North Sea coast while fjards dominate the Baltic Sea coast.

The Torran Rocks are a group of small islands and skerries located between the islands of Mull and Colonsay in Scotland.

<span class="mw-page-title-main">Strandflat</span> Type of landform found in high-latitude areas

Strandflat is a landform typical of the Norwegian coast consisting of a flattish erosion surface on the coast and near-coast seabed. In Norway, strandflats provide room for settlements and agriculture, constituting important cultural landscapes. The shallow and protected waters of strandflats are valued fishing grounds that provide sustenance to traditional fishing settlements. Outside Norway proper, strandflats can be found in other high-latitude areas, such as Antarctica, Alaska, the Canadian Arctic, the Russian Far North, Greenland, Svalbard, Sweden and Scotland.

<i>Skärgårdsnamn</i> 1989 book on place names by Kurt Zilliacus

Skärgårdsnamn, is a Finnish Swedish-language book on around one hundred thousand Swedish place names in Finland's archipelagos, written by toponymy researcher Kurt Zilliacus, published in 1989.

References

  1. Johnson, Markes E.; Webb, Gregory E. (1 September 2007). "Outer Rocky Shores of the Mowanbini Archipelago, Devonian Reef Complex, Canning Basin, Western Australia" (PDF). The Journal of Geology. 115 (5): 583–600. Bibcode:2007JG....115..583J. doi:10.1086/519779. S2CID   129190899.
  2. "Indo-European root sker-".
  3. Tolvanen, Harri; Numminen, Samu; Kalliola, Risto (1 January 2004). "Spatial Distribution and Dynamics of Special Shore-Forms (Tombolos, Flads and Glo-lakes) in an Uplifting Archipelago of the Baltic Sea". Journal of Coastal Research. 20 (1): 234–243. doi:10.2112/1551-5036(2004)20[234:SDADOS]2.0.CO;2. JSTOR   4299279. S2CID   130519270.