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Gower Peninsula
The Gower Peninsula (Welsh: Penrhyn Gŵyr), or simply Gower (Gŵyr), is a peninsula in the south-west of Wales. It is the most westerly part of the historic county of Glamorgan, and is now within the City and County of Swansea. It projects towards the Bristol Channel. In 1956, the majority of Gower became the first area in the United Kingdom to be designated an Area of Outstanding Natural Beauty.
Until 1974, Gower was administered as a rural district. It was then merged with the county borough of Swansea. From 1974 to 1996, it formed the Swansea district. Since 1996, Gower has been administered as part of the unitary authority of the City and County of Swansea.
Since its establishment in 1999, the Gower Senedd constituency has only elected Labour members. The Gower constituency in Westminster had previously also elected only Labour Members of Parliament (MPs) since 1908; the longest run (with Normanton and Makerfield) of any UK constituency. This ended in 2015 when the Conservatives took the seat. In 2017, it returned to Labour. The area of both constituencies covers the peninsula and the outer Gower areas of Clydach, Gowerton, Gorseinon, Felindre, Garnswllt and encompasses the area of the historic Lordship of Gower apart from the city of Swansea.
About 70 square miles (180 km2) in area, Gower is known for its coastline, popular with walkers and outdoor enthusiasts, especially surfers. Gower has many caves, including Paviland Cave and Minchin Hole Cave. The peninsula is bounded by the Loughor Estuary to the north and Swansea Bay to the east. Gower Area of Outstanding Natural Beauty covers 188 km2, including most of the peninsula west of Crofty, Three Crosses, Upper Killay, Blackpill and Bishopston. The highest point of Gower is The Beacon at Rhossili Down at 193 metres (633 feet) overlooking Rhossili Bay. Pwll Du and the Bishopton Valley form a statutory Local Nature Reserve.
The southern coast consists of a series of small, rocky or sandy bays, such as Langland and Three Cliffs, and larger beaches such as Port Eynon, Rhossili and Oxwich Bay. The north of the peninsula has fewer beaches, and is home to the cockle-beds of Penclawdd.
The northern coast is mainly salt marsh, and is used for raising Gower salt marsh lamb which was registered as a Protected Designation of Origin in 2021 under UK law and in 2023 under EU law.
The interior is mainly farmland and common land. The population mainly resides in small villages and communities with some suburban development in eastern Gower; part of the Swansea Urban Area.
In the caves of Bacon Hole and Minchin Hole on the southern coast of the Gower, remains of Pleistocene aged animals have been found, primarily animals present in the area during the Last Interglacial and the beginning of the Last Glacial Period (around 130-87,000 years ago) when the area had a similar climate to today, including animals such as straight-tusked elephants, the narrow-nosed rhinoceros, bison, cave lions, wolves, cave hyenas (who at times used the caves as dens), red foxes, red deer, roe deer, and fallow deer, as well as woolly mammoths in younger layers, with later layers in the caves dating to cooler phases of the Last Glacial having cold adapted species like reindeer and wolverines.
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Gower Peninsula AI simulator
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Gower Peninsula
The Gower Peninsula (Welsh: Penrhyn Gŵyr), or simply Gower (Gŵyr), is a peninsula in the south-west of Wales. It is the most westerly part of the historic county of Glamorgan, and is now within the City and County of Swansea. It projects towards the Bristol Channel. In 1956, the majority of Gower became the first area in the United Kingdom to be designated an Area of Outstanding Natural Beauty.
Until 1974, Gower was administered as a rural district. It was then merged with the county borough of Swansea. From 1974 to 1996, it formed the Swansea district. Since 1996, Gower has been administered as part of the unitary authority of the City and County of Swansea.
Since its establishment in 1999, the Gower Senedd constituency has only elected Labour members. The Gower constituency in Westminster had previously also elected only Labour Members of Parliament (MPs) since 1908; the longest run (with Normanton and Makerfield) of any UK constituency. This ended in 2015 when the Conservatives took the seat. In 2017, it returned to Labour. The area of both constituencies covers the peninsula and the outer Gower areas of Clydach, Gowerton, Gorseinon, Felindre, Garnswllt and encompasses the area of the historic Lordship of Gower apart from the city of Swansea.
About 70 square miles (180 km2) in area, Gower is known for its coastline, popular with walkers and outdoor enthusiasts, especially surfers. Gower has many caves, including Paviland Cave and Minchin Hole Cave. The peninsula is bounded by the Loughor Estuary to the north and Swansea Bay to the east. Gower Area of Outstanding Natural Beauty covers 188 km2, including most of the peninsula west of Crofty, Three Crosses, Upper Killay, Blackpill and Bishopston. The highest point of Gower is The Beacon at Rhossili Down at 193 metres (633 feet) overlooking Rhossili Bay. Pwll Du and the Bishopton Valley form a statutory Local Nature Reserve.
The southern coast consists of a series of small, rocky or sandy bays, such as Langland and Three Cliffs, and larger beaches such as Port Eynon, Rhossili and Oxwich Bay. The north of the peninsula has fewer beaches, and is home to the cockle-beds of Penclawdd.
The northern coast is mainly salt marsh, and is used for raising Gower salt marsh lamb which was registered as a Protected Designation of Origin in 2021 under UK law and in 2023 under EU law.
The interior is mainly farmland and common land. The population mainly resides in small villages and communities with some suburban development in eastern Gower; part of the Swansea Urban Area.
In the caves of Bacon Hole and Minchin Hole on the southern coast of the Gower, remains of Pleistocene aged animals have been found, primarily animals present in the area during the Last Interglacial and the beginning of the Last Glacial Period (around 130-87,000 years ago) when the area had a similar climate to today, including animals such as straight-tusked elephants, the narrow-nosed rhinoceros, bison, cave lions, wolves, cave hyenas (who at times used the caves as dens), red foxes, red deer, roe deer, and fallow deer, as well as woolly mammoths in younger layers, with later layers in the caves dating to cooler phases of the Last Glacial having cold adapted species like reindeer and wolverines.