South Stack

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South Stack
Ynys Lawd (Welsh)
South Stack lighthouse aerial.jpg
Isle of Anglesey UK location map.svg
Red pog.svg
South Stack
Location with Anglesey
Geography
Location Irish Sea near Holyhead, Anglesey
Coordinates 53°18′24.40″N4°41′56.91″W / 53.3067778°N 4.6991417°W / 53.3067778; -4.6991417
Length0.15 mi (0.24 km)
Width0.1 mi (0.2 km)
Highest point134 ft (41 m)

South Stack (Welsh : Ynys Lawd) is an island situated just off Holy Island on the northwest coast of Anglesey, Wales.

Contents

Geology

Folding in the South Stack Formation can be seen in the rocks of the mainland's sea cliffs. South Stack3.JPG
Folding in the South Stack Formation can be seen in the rocks of the mainland's sea cliffs.

South Stack is an island known as a sea stack. It was formed by the wave erosion of sedimentary rocks that once connected the island to the mainland. [1]

The area is known geologically as the South Stack Formation. Its strata includes sandstones and interbedded shales which have been contorted by large folds and crumples. The folds can be seen in the seacliffs (best viewed from the steps leading down to the lighthouse). Thick beds of pure Holyhead Quartzite, which forms the bulk of Holyhead Mountain, lie above these folded sedimentary rocks. Recent studies suggests the rocks appearance was caused by large scale earth movements which is not a part of the normal sedimentary process; however, this theory remains controversial. Similar evidence of upthrusts can be seen in the cliffs to the south of South Stack. [2]

The geology of South Stack has been chosen as one of the top 100 geosites in the United Kingdom by Geological Society of London, for its display of small-scale folding. [3]

Lighthouse

South Stack Lighthouse, which was first built in the early 19th century, is connected to the mainland via a footbridge. South Stack Lighthouse - geograph.org.uk - 870858.jpg
South Stack Lighthouse, which was first built in the early 19th century, is connected to the mainland via a footbridge.

South Stack Lighthouse, which was completed in 1809, is sited 41 metres (135 ft) above the sea on South Stack. Its lamp tower is 28 m (92 ft)-tall and the lighthouse complex covers seven acres (2.8 ha). There are over 390 stone steps and 10 metal steps down to the footbridge.

Originally the only way to cross to the island was in a basket suspended from a hemp cable. In 1828, an iron suspension bridge was built; it was replaced in 1964 with a steel cable truss bridge. However, in 1983 it had to be closed to the public due to safety concerns. After a new aluminium bridge was built, the lighthouse was reopened to the public in 1997. It is now a popular destination, attracting thousands of visitors every year.

Nature reserve

The island's cliffs are part of the South Stack Cliffs RSPB reserve which are home to an estimated 8,000 nesting birds during the breeding season. An RSPB visitor centre (with bird hide) is located at Elin's Tower on the mainland. Birds and marine life seen from the centre include choughs, peregrine falcons, and kestrels as well as harbour porpoises, grey seals, Risso's dolphins and bottlenose dolphins.

Tidal energy project

In 2019, proposals to develop a 35 km2 (14 sq mi) 'West Anglesey Demonstration Zone' tidal energy project at South Stack were submitted under the Transport and Works Act 1992 to the Welsh Government for planning consent. [4] Consent for the project, called Morlais was awarded in December 2021 and construction of the onshore grid connection works took place in 2023. [5] [6]

As the development will come within 500 metres (1,600 ft) of the South Stack SSSI, concerns have been expressed about the visual impact on the Anglesey Area of Outstanding Natural Beauty and the Holyhead Mountain Heritage Coast, along with the resultant impact on the tourism, recreation and fishing sectors. The developers have identified that seabird and mammal populations would be affected within the Holy Island Coast Special Area of Conservation and Special Protection Area along with the North Anglesey Marine Special Area of Conservation. Most notably bottlenose dolphin and harbour porpoise would likely be affected, whilst razorbill and common guillemot will be severely impacted. The RSPB is concerned that the razorbill colony on South Stack could be wiped out. [7]

Walking trails

Part of the Anglesey Coastal Path, which is a 200-kilometre (124 mi) long-distance footpath around the island of Anglesey, passes South Stack. [8] The Cybi Circular Walk around Holyhead Mountain has long and short variants; the short walk is four miles (6.4 km) long and takes around two hours to complete. Travelling from the Breakwater Country Park, other sites along the way are the North Stack Fog Signal station, Caer y Tŵr, and Tŷ Mawr Hut Circles.

Media

South Stack's natural beauty has been used in photography and literature. The cover photo for Roxy Music's Siren album was taken directly below the central span of the bridge on a slope on the south side, by Graham Hughes in August 1975. [9] In 2010, a French comic entitled Les Gardiens des Enfers (The Guardians of Hell) was published. Its story is mainly set in South Stack lighthouse in 1859. The cover and the first pages can be seen on the publisher's website. [10]

See also

Related Research Articles

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Holyhead is the largest town and a community in the county of Isle of Anglesey, Wales, with a population of 13,659 at the 2011 census.. Holyhead is on Holy Island, bounded by the Irish Sea to the north, and is separated from Anglesey island by the narrow Cymyran Strait and was originally connected to Anglesey via the Four Mile Bridge.

<span class="mw-page-title-main">Holy Island, Anglesey</span> Island, part of Wales, United Kingdom

Holy Island is an island on the western side of the larger Isle of Anglesey, Wales, from which it is separated by the Cymyran Strait. It is called "Holy" because of the high concentration of standing stones, burial chambers, and other religious sites on the small island. The alternative English name of the island is Holyhead Island. According to the 2011 UK Census, the population was 13,659, of whom 11,431 (84%) lived in the largest town, Holyhead.

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<span class="mw-page-title-main">Ramsey Island</span> Island in Pembrokeshire, Wales

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<span class="mw-page-title-main">Godrevy</span> Area on the eastern side of St Ives Bay, west Cornwall, England

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

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<span class="mw-page-title-main">South Stack Cliffs RSPB reserve</span> RSPB nature reserve in Anglesey, UK

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<span class="mw-page-title-main">North Stack</span> Island in Anglesey, Wales, United Kingdom

North Stack is a small island situated just off Holy Island on the north-west coast of Anglesey. The area has been an important location in the development of traditional climbing in Britain and has several notable classic, and also extreme, climbing routes.

<span class="mw-page-title-main">South Stack Lighthouse</span> Lighthouse in Anglesey, Wales

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<span class="mw-page-title-main">South Stack Formation</span> Cambro-Ordovician geologic formation in Wales

The South Stack Formation is a sequence of Cambro-Ordovician metasedimentary rocks exposed in northwestern Anglesey, North Wales. The outcrop of this formation at South Stack was chosen as one of the top 100 geosites in the United Kingdom by the Geological Society of London, for its display of small-scale folding.

<span class="mw-page-title-main">Cymyran Strait</span> Strait in Wales

Cymyran Strait is a strait that runs from Beddmanarch Bay in the north to Cymyran Bay in the south between the islands of Anglesey and Holy Island. At either end it opens up into the Irish Sea.

The geology of Anglesey, the largest (714 km2) island in Wales is some of the most complex in the country. Anglesey has relatively low relief, the 'grain' of which runs northeast–southwest, i.e. ridge and valley features extend in that direction reflecting not only the trend of the late Precambrian and Palaeozoic age bedrock geology but also the direction in which glacial ice traversed and scoured the island during the last ice age. It was realised in the 1980s that the island is composed of multiple terranes, recognition of which is key to understanding its Precambrian and lower Palaeozoic evolution. The interpretation of the island's geological complexity has been debated amongst geologists for decades and recent research continues in that vein.

<span class="mw-page-title-main">Coastline of Wales</span> Sea-bounded areas of Wales

The coastline of Wales extends from the English border at Chepstow westwards to Pembrokeshire then north to Anglesey and back eastwards to the English border once again near Flint. Its character is determined by multiple factors, including the local geology and geological processes active during and subsequent to the last ice age, its relative exposure to or shelter from waves, tidal variation and the history of human settlement and development which varies considerably from one place to another. The majority of the coast east of Cardiff in the south, and of Llandudno in the north, is flat whilst that to the west is more typically backed by cliffs. The cliffs are a mix of sandstones, shales and limestones, the erosion of which provides material for beach deposits. Of the twenty-two principal areas which deliver local government in Wales, sixteen have a coastline, though that of Powys consists only of a short section of tidal river some distance from the open sea. Its length has been estimated at 1,680 miles (2,700 km).

The geology of Pembrokeshire in Wales inevitably includes the geology of the Pembrokeshire Coast National Park which extends around the larger part of the county's coastline and where the majority of rock outcrops are to be seen. Pembrokeshire's bedrock geology is largely formed from a sequence of sedimentary and igneous rocks originating during the late Precambrian and the Palaeozoic era, namely the Ediacaran, Cambrian, Ordovician, Silurian, Devonian and Carboniferous periods, i.e. between 635 and 299 Ma. The older rocks in the north of the county display patterns of faulting and folding associated with the Caledonian Orogeny. On the other hand, the late Palaeozoic rocks to the south owe their fold patterns and deformation to the later Variscan Orogeny.

Morlais is a grid connected tidal stream energy project located in the Irish Sea just off the west coast of Holy Island, Anglesey, Wales. It is being developed by the social enterprise agency Menter Môn. The site has the potential for up to 240 MW of renewable energy to be harnessed from the tides, using a mixture of seabed mounted and floating tidal energy devices from different companies.

References

  1. Stacks are formed over time by wind and water, processes of coastal geomorphology. "Sea stacks" britannica.com Archived 14 April 2009 at the Wayback Machine
  2. "South Stack Geology". angleseynature.co.uk. Retrieved 24 August 2020.
  3. "The Geological Society's 100 Great Geosites". The Geological Society. 2014. Retrieved 14 October 2014.
  4. "What is Morlais". Menter Môn . Retrieved 26 October 2019.
  5. "Jones Bros completes onshore works for Morlais". reNEWS.biz. 23 June 2023.
  6. "Official opening of Wales' first tidal stream energy site on Anglesey". North Wales Chronicle. 20 October 2023. Retrieved 1 December 2023.
  7. "Update on Morlais". rspb.org.uk. 15 April 2020.
  8. "Circular walks - Holyhead: St Cybi". walkingnorthwales.co.uk. Retrieved 24 January 2013.
  9. "Roxy Music - Albums - on VivaRoxyMusic.com". vivaroxymusic.com. Retrieved 18 February 2016.
  10. Les Gardiens des Enfers

53°18′24.5″N4°41′55.5″W / 53.306806°N 4.698750°W / 53.306806; -4.698750