The Darling Scarp, also referred to as the Darling Range or Darling Ranges, is a low escarpment running north–south to the east of the Swan Coastal Plain and Perth, Western Australia. The escarpment extends generally north of Bindoon, to the south of Pemberton. The adjacent Darling Plateau goes easterly to include Mount Bakewell near York and Mount Saddleback near Boddington. It was named after the Governor of New South Wales, Lieutenant-General Ralph Darling.
Bluestone is a cultural or commercial name for a number of dimension or building stone varieties, including:
Wintour's Leap is a noted rock climbing location and viewpoint. It is located near the village of Woodcroft in Gloucestershire, on the English side of the Wye Valley, north of Chepstow.
Fair Head or Benmore is a 5-kilometre long mountain cliff, close to the sea, at the north-eastern corner of County Antrim, Northern Ireland, whose rock face is formed into distinctive vertical columns like organ pipes. Fair Head is regarded as one of the best outdoor rock-climbing locations in Ireland, and its long cliff, up to 100 metres high in places, is considered one of the biggest expanses of climbable rock in Northwest Europe.
Shropshire's Geology is very diverse and most geological periods of time, and most rock types, can be found within the county. There is also a large amount of mineral wealth in the county, including lead, barytes, limestone, coal and iron, which helped the area develop the industrial revolution west of Clee Hill and, later, in the Ironbridge Gorge area. Quarrying is still active, with limestone for cement manufacture and concrete aggregate, sandstone, greywacke and dolerite for road aggregate, and sand and gravel for aggregate and drainage filters. Groundwater is an equally important economic resource.
Blaenavon Industrial Landscape, in and around Blaenavon, Torfaen, Wales, was inscribed a World Heritage Site by UNESCO in 2000. The Blaenavon Ironworks, now a museum, was a major centre of iron production using locally mined or quarried iron ore, coal and limestone. Raw materials and products were transported via horse-drawn tramroads, canals and steam railways. The Landscape includes protected or listed monuments of the industrial processes, transport infrastructure, workers' housing and other aspects of early industrialisation in South Wales.
Dinas Rock is a high promontory of Carboniferous Limestone which rises between the Afon Mellte and its left-bank tributary, the Afon Sychryd on the border between the county of Powys and the county borough of Neath Port Talbot in south Wales. It can be found near the village of Pontneddfechan near Glyn Neath at the head of the Vale of Neath. It derives its name from the presence of Iron Age earthworks on its summit, dinas in Welsh signifying a defensive site or "city".
Pentre Halkyn is a small village in Flintshire, Wales. It is situated approximately two miles from Holywell, and is off Junction 32 of the A55 North Wales Expressway. It has a quarry, a small hotel, and a local shop. The village borders on the Halkyn Mountain Site of Special Scientific Interest and Special Area of Conservation.
Carboniferous Limestone is a collective term for the succession of limestones occurring widely throughout Great Britain and Ireland that were deposited during the Dinantian Epoch of the Carboniferous Period. These rocks formed between 363 and 325 million years ago. Within England and Wales, the entire limestone succession, which includes subordinate mudstones and some thin sandstones, is known as the Carboniferous Limestone Supergroup.
Bwlchgwyn is a village in Wrexham County Borough, Wales, on the A525 road, 5 miles (8 km) west of the town of Wrexham and 10 miles (16 km) south-east of the town of Ruthin. Bwlchgwyn is part of the community of Brymbo. In the 2011 Census the population of the village was 855.
The Eglwyseg valley is an area to the north east of Llangollen in Denbighshire, Wales; it is within the boundaries of Llantysilio Community. The name also refers to a widely scattered hamlet in the valley.
Dalkey Quarry is a long disused 19th century granite quarry located on Dalkey Hill in the Dublin suburb of Dalkey, which has become one of the most popular rock climbing locations in Ireland, with over 350 routes, some of which are amongst the hardest single-pitch rock climbs in Ireland.
Pot Hole quarry is a former limestone quarry close to Llanferres, near Mold, in Denbighshire, North Wales. The quarry is popular with rock climbers due to its rural setting, ease of access and selection of routes on good quality limestone. The average height of the quarried rock is approximately 12 metres (39 ft).
Penwyllt is a hamlet located in the upper Swansea Valley in Powys, Wales.
Adelaide Brighton Cement (ABC) is an Australian manufacturer of cement, lime and dry blended products.
Fforest Fawr Geopark was the first Geopark to be designated in Wales having gained membership of both the European Geoparks Network and the UNESCO-assisted Global Network of National Geoparks in October 2005. The Geopark aims to promote and support sustainable tourism and other opportunities to improve the economy of the area whilst safeguarding the natural environment. Its aims largely coincide with the statutory duties and purpose of the National Park within which it sits.
The Wyndcliff or Wynd Cliff is a steep limestone cliff rising above the western bank of the River Wye in Monmouthshire, Wales, some 1 mile (1.6 km) north-east of the village of St Arvans, 2.5 miles (4.0 km) south of Tintern, and 3.5 miles (5.6 km) north of the town of Chepstow, within the Wye Valley Area of Outstanding Natural Beauty. The cliff rises to 771 feet (235 m) at its summit, the highest point on the Monmouthshire bank of the Wye. The area is traversed by the Wye Valley Walk, and is also a popular venue for rock climbing. Access is provided by the A466 road which passes along the valley immediately below the cliff face.
Bungonia National Park is a protected national park that is located in the Australian state of New South Wales, roughly 40 kilometres (25 mi) east of the city of Goulburn and 122 km (76 mi) south-west of Sydney. The approximately 15 square kilometres (5.8 sq mi) park borders the Bungonia State Conservation Area to the South, Morton National Park to the East, and Bungonia Creek to the North. Only a relatively recent addition to the national parks registry, Bungonia was originally protected as a water reserve to prevent contamination of the Shoalhaven River in the mid-late 19th century.
This article describes the geology of the Brecon Beacons National Park in mid/south Wales. The area gained national park status in 1957 with the designated area of 1,344 km2 (519 sq mi) including mountain massifs to both the east and west of the Brecon Beacons proper. The geology of the national park consists of a thick succession of sedimentary rocks laid down from the late Ordovician through the Silurian and Devonian to the late Carboniferous period. The rock sequence most closely associated with the park is the Old Red Sandstone from which most of its mountains are formed. The older parts of the succession, in the northwest, were folded and faulted during the Caledonian orogeny. Further faulting and folding, particularly in the south of the park is associated with the Variscan orogeny.
The bedrock geology of Carmarthenshire in west Wales consists largely of Palaeozoic age sedimentary rocks. Unconsolidated deposits of Quaternary age in Carmarthenshire include a dissected cover of glacial till, valley floor alluvium and some scattered peat deposits in both upland and lowland settings. There are extensive beach and tidal flat deposits along the Carmarthenshire coast. The exploitation of the county's mineral riches, particularly coal and limestone, was a key part of the local economy through much of the nineteenth and twentieth centuries.
