|
Perranporth Village Centre From Boscawen Road
Perranporth ( kw, Porthperan) is a seaside resort town on the north coast of Cornwall, England, United Kingdom. It is 1 mile east of the St Agnes Heritage Coastline, and around 8 miles south-west of Newquay. Perranporth and its long beach face the Atlantic Ocean.Ordnance Survey: Landranger map sheet 204 ''Truro & Falmouth'' It has a population of 3,066, and is the largest settlement in the civil parish of Perranzabuloe. It has an electoral ward in its own name, whose population was 4,270 in the 2011 census. The town's modern name comes from ''Porth Peran'', the Cornish for the cove of Saint Piran, the patron saint of Cornwall. He founded St Piran's Oratory on Penhale Sands near Perranporth in the 7th century. Buried under sand for many centuries, it was unearthed in the 19th century. History The ''Voorspoed'' ran ashore in a northerly gale in Perran Bay on 7 March 1901, while travelling from Cardiff to Bahia. The wreck was one of the last to be looted. Perranporth Airfi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Perranzabuloe
Perranzabuloe (; kw, Pyran yn Treth) is a coastal civil parish and a hamlet in Cornwall, England, United Kingdom. Perranzabuloe parish is bordered to the west by the Atlantic coast and St Agnes parish, to the north by Cubert parish, to the east by St Newlyn East and St Allen parishes and to the south by Kenwyn parish. The hamlet (containing the parish church) is situated just over a mile (2 km) south of the principal settlement of the parish, Perranporth; the hamlet is also seven miles (11 km) south-southwest of Newquay. Other settlements in the parish include Perrancoombe, Goonhavern, Mount and Callestick. The parish population was 5,382 in the 2001 census, increasing to 5,486 at the 2011 census. The name of the parish derives from the medieval Latin ''Perranus in Sabulo'' meaning Piran in the sand. It refers to Saint Piran (the patron saint of Cornwall) who founded an oratory church in the seventh century near the coast north of Perranporth. In medieval times the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chacewater
Chacewater ( kw, Dowr an Chas) is a village and civil parish in Cornwall, England, UK. It is situated approximately east of Redruth. The hamlets of Carnhot, Cox Hill, Creegbrawse, Hale Mills, Jolly's Bottom, Salem, Saveock, Scorrier, Todpool, Twelveheads and Wheal Busy are in the parish. The electoral ward is called Chacewater & Kenwyn. At the 2011 census a population of 3,870 was quoted. Village Chacewater sits in a valley between hills separating it from the villages of Threemilestone, Scorrier and St Day. Nearby is Wheal Busy, the Poldice Valley and the Coast to Coast cycle route. The village has a pub and a club, the Chacewater Literary Institute. There are also a health centre, primary school, village hall and small selection of shops. A free monthly magazine ''What's on in Chacewater'' reached its 200th issue in July 2007. It lists events and activities, such as the Football Club, a Cricket Club, a Bowling Club, the Chacewater Old Cornwall Society, the Chacewater Playe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Orienteering
Orienteering is a group of sports that require navigational skills using a map and compass to navigate from point to point in diverse and usually unfamiliar terrain whilst moving at speed. Participants are given a topographical map, usually a specially prepared orienteering map, which they use to find control points. Originally a training exercise in land navigation for military officers, orienteering has developed many variations. Among these, the oldest and the most popular is foot orienteering. For the purposes of this article, foot orienteering serves as a point of departure for discussion of all other variations, but almost any sport that involves racing against a clock and requires navigation with a map is a type of orienteering. Orienteering is included in the programs of world sporting events including the World Games (see Orienteering at the World Games) and World Police and Fire Games. History The history of orienteering begins in the late 19th century in Swede ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Penhale Sands
Penhale Sands ( kw, Peran Treth, meaning ''St Piran's sands''), or Penhale Dunes, is a complex of sand dunes and a protected area for its wildlife, on the north Cornwall coast in England, UK. It is the most extensive system of sand dunes in Cornwall and is believed to be the landing site of Saint Piran. Dating from the 6th century, St Piran's Oratory is thought to be one of the oldest Christian sites in Britain. The remains were discovered in the late 18th century, and in 2014 the covering sand was removed to reveal a building more than a thousand years old, in a reasonable state of preservation. A restricted military area dating from 1939, Penhale Camp, is found on the northern part of the dunes. The area has been designated as a Site of Special Scientific Interest (SSSI) since 1953 and became a Special Area of Conservation (SAC) in 2004. The South West Coast Path runs through the dunes. Geography The sands are located south-west of the town of Newquay, in the civil parish of P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sand Dunes
A dune is a landform composed of wind- or water-driven sand. It typically takes the form of a mound, ridge, or hill. An area with dunes is called a dune system or a dune complex. A large dune complex is called a dune field, while broad, flat regions covered with wind-swept sand or dunes with little or no vegetation are called ''ergs'' or ''sand seas''. Dunes occur in different shapes and sizes, but most kinds of dunes are longer on the stoss (upflow) side, where the sand is pushed up the dune, and have a shorter ''slip face'' in the lee side. The valley or trough between dunes is called a ''dune slack''. Dunes are most common in desert environments, where the lack of moisture hinders the growth of vegetation that would otherwise interfere with the development of dunes. However, sand deposits are not restricted to deserts, and dunes are also found along sea shores, along streams in semiarid climates, in areas of glacial outwash, and in other areas where poorly cemented san ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Youth Hostels Association (England & Wales)
The Youth Hostels Association (England & Wales) is a charitable organisation, registered with the Charity Commission, providing youth hostel accommodation in England and Wales. It is a member of the Hostelling International federation. History Formation The concept of youth hostels originated in Germany in 1909 with Richard Schirrmann and it took 20 years for the ideas to reach fruition in the United Kingdom. In 1929/30, several groups almost simultaneously formed to investigate establishing youth hostels in the UK. Foremost among these was the Merseyside Centre of the British Youth Hostels Association. On 10 April 1930, representatives of these bodies met and agreed to form the British Youth Hostels Association. Shortly afterwards, it became YHA (England & Wales), with separate associations for Scotland ( Hostelling Scotland) and Northern Ireland (Hostelling International Northern Ireland). YHA's charitable objective is stated as: To help all, especially young people ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Adit
An adit (from Latin ''aditus'', entrance) is an entrance to an underground mine which is horizontal or nearly horizontal, by which the mine can be entered, drained of water, ventilated, and minerals extracted at the lowest convenient level. Adits are also used to explore for mineral veins. Construction Adits are driven into the side of a hill or mountain, and are often used when an ore body is located inside the mountain but above the adjacent valley floor or coastal plain. In cases where the mineral vein outcrops at the surface, the adit may follow the lode or vein until it is worked out, in which case the adit is rarely straight. The use of adits for the extraction of ore is generally called drift mining. Adits can only be driven into a mine where the local topography permits. There will be no opportunity to drive an adit to a mine situated on a large flat plain, for instance. Also if the ground is weak, the cost of shoring up a long adit may outweigh its possible advantage ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stack (geology)
A stack or sea stack is a geological landform consisting of a steep and often vertical column or columns of rock in the sea near a coast, formed by wave erosion. Stacks are formed over time by wind and water, processes of coastal geomorphology. britannica.com They are formed when part of a headland is by , which is the force of the sea or water crashing against the rock. The force of the water weakens cracks in the headland, causing them to later collapse, formi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Natural Arch
A natural arch, natural bridge, or (less commonly) rock arch is a natural landform where an arch has formed with an opening underneath. Natural arches commonly form where inland cliffs, coastal cliffs, fins or stacks are subject to erosion from the sea, rivers or weathering ( subaerial processes). Most natural arches are formed from narrow fins and sea stacks composed of sandstone or limestone with steep, often vertical, cliff faces. The formations become narrower due to erosion over geologic time scales. The softer rock stratum erodes away creating rock shelters, or alcoves, on opposite sides of the formation beneath the relatively harder stratum, or caprock, above it. The alcoves erode further into the formation eventually meeting underneath the harder caprock layer, thus creating an arch. The erosional processes exploit weaknesses in the softer rock layers making cracks larger and removing material more quickly than the caprock; however, the caprock itself continues to er ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ebb Tide
Tides are the rise and fall of sea levels caused by the combined effects of the gravitational forces exerted by the Moon (and to a much lesser extent, the Sun) and are also caused by the Earth and Moon orbiting one another. Tide tables can be used for any given locale to find the predicted times and amplitude (or "tidal range"). The predictions are influenced by many factors including the alignment of the Sun and Moon, the phase and amplitude of the tide (pattern of tides in the deep ocean), the amphidromic systems of the oceans, and the shape of the coastline and near-shore bathymetry (see '' Timing''). They are however only predictions, the actual time and height of the tide is affected by wind and atmospheric pressure. Many shorelines experience semi-diurnal tides—two nearly equal high and low tides each day. Other locations have a diurnal tide—one high and low tide each day. A "mixed tide"—two uneven magnitude tides a day—is a third regular category. Tides va ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rip Current
A rip current, often simply called a rip (or misleadingly a ''rip tide''), is a specific kind of water current that can occur near beaches with breaking waves. A rip is a strong, localized, and narrow current of water which moves directly away from the shore, cutting through the lines of breaking waves like a river running out to sea. The current in a rip is strongest and fastest next to the surface of the water. Rip currents can be hazardous to people in the water. Swimmers who are caught in a rip current and who do not understand what is happening, or who may not have the necessary water skills, may panic, or they may exhaust themselves by trying to swim directly against the flow of water. Because of these factors, rip currents are the leading cause of rescues by lifeguards at beaches, and in the United States, they are the cause of an average of 46 deaths by drowning per year. A rip current is not the same thing as undertow, although some people use the term incorrectly whe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Surfing
Surfing is a surface water sport in which an individual, a surfer (or two in tandem surfing), uses a board to ride on the forward section, or face, of a moving wave of water, which usually carries the surfer towards the shore. Waves suitable for surfing are primarily found on ocean shores, but can also be found in standing waves in the open ocean, in lakes, in rivers in the form of a tidal bore, or in wave pools. The term ''surfing'' refers to a person riding a wave using a board, regardless of the stance. There are several types of boards. The Moche of Peru would often surf on reed craft, while the native peoples of the Pacific surfed waves on alaia, paipo, and other such water craft. Ancient cultures often surfed on their belly and knees, while the modern-day definition of surfing most often refers to a surfer riding a wave standing on a surfboard; this is also referred to as stand-up surfing. Another prominent form of surfing is body boarding, where a surfer rides ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpg "Click for more on -> Adit")
.jpg "Click for more on -> Stack (geology)")
