Restronguet Creek
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Restronguet Creek
Restronguet Creek is a tidal ria in south Cornwall, United Kingdom. It is a tributary of Carrick Roads, the estuary of the River Fal, and is situated approximately four miles (6.5 km) south of Truro and three miles (5 km) north of Falmouth. Ordnance Survey: Landranger map sheet 204 ''Truro & Falmouth'' The creek is approximately two miles (3 km) long from its Normal Tidal Limit (NTL) to its mouth and half-a-mile (800 metres) across at its widest point. It discharges into Carrick Roads at Restronguet Point through a narrow channel known locally as 'the gut'.
Restronguet Creek Society website. Retrieved May 2010
Restronguet Creek forms the boundary between the es of
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Restronguet Creek - Geograph
Restronguet is in south Cornwall in the United Kingdom and gives its name to: * Restronguet Creek, a tidal ria * Restronguet Passage, a waterside hamlet * Restronguet Point, a small headland and coastal settlement * Restronguet Sailing Club, a club at Mylor Churchtown Mylor Churchtown is a coastal village in Cornwall, England. It is the church town of the ecclesiastical parish of Mylor and is situated at the mouth of Mylor Creek, approximately three miles north of Falmouth.Ordnance Survey: Landranger map ...
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River Kennall
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, a ...
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Mylor Harbour
Mylor Churchtown is a coastal village in Cornwall, England. It is the church town of the ecclesiastical parish of Mylor and is situated at the mouth of Mylor Creek, approximately three miles north of Falmouth.Ordnance Survey: Landranger map sheet 204 ''Truro & Falmouth'' Mylor Yacht Harbour is a large yacht marina immediately north of Mylor Churchtown. It has been owned by the Graffy family since 1997. The marina is at the mouth of Mylor Creek at its confluence with Carrick Roads and is the home of Restronguet Sailing Club. Parish church Mylor parish church (Anglican) is in Mylor Churchtown and is dedicated to St Melorus. The church has Norman origins and is built on a cruciform plan, with a south aisle was added in the 15th century. There is a small west tower but the bells (three in number, the earliest dated 1637) are in a detached campanile. One of these bells bears the Latin inscription EGO ME PRECO SE CLAMANDO CONTERIMUS AUDITE VENITE (i.e. ''Ego me, praeco se clama ...
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Dinghy Racing
Dinghy racing is a competitive sport using dinghies, which are small boats which may be rowboats, have an outboard motor, or be sailing dinghies. Dinghy racing has affected aspects of the modern sailing dinghy, including hull design, sail materials and sailplan, and techniques such as planing and trapezing. Organization of competitive dinghy sailing Dinghy racing comes under the auspices of World Sailing. Organisations such as the Royal Yachting Association, National School Sailing Association (UK) and Canadian Yachting Association (Canada) organise and regulate the sport at a national level. Sailing dinghies compete on an international, national, state, association, club and class basis, using the ISAF International Racing Rules of Sailing, which are revised every four years. There are several courses used, such as the Olympic triangle. The International Association for Disabled Sailing (IFDS)] is the body authorized by ISAF to be responsible for disabled sailing worldwide. ...
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Yacht
A yacht is a sailing or power vessel used for pleasure, cruising, or racing. There is no standard definition, though the term generally applies to vessels with a cabin intended for overnight use. To be termed a , as opposed to a , such a pleasure vessel is likely to be at least in length and may have been judged to have good aesthetic qualities. The Commercial Yacht Code classifies yachts and over as . Such yachts typically require a hired crew and have higher construction standards. Further classifications for large yachts are: —carrying no more than 12 passengers, —solely for the pleasure of the owner and guests, or by flag, the country under which it is registered. A superyacht (sometimes ) generally refers to any yacht (sail or power) longer than . Racing yachts are designed to emphasize performance over comfort. Charter yachts are run as a business for profit. As of 2020 there were more than 15,000 yachts of sufficient size to require a professional crew. Etymology ...
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English Channel
The English Channel, "The Sleeve"; nrf, la Maunche, "The Sleeve" (Cotentinais) or ( Jèrriais), (Guernésiais), "The Channel"; br, Mor Breizh, "Sea of Brittany"; cy, Môr Udd, "Lord's Sea"; kw, Mor Bretannek, "British Sea"; nl, Het Kanaal, "The Channel"; german: Ärmelkanal, "Sleeve Channel" ( French: ''la Manche;'' also called the British Channel or simply the Channel) is an arm of the Atlantic Ocean that separates Southern England from northern France. It links to the southern part of the North Sea by the Strait of Dover at its northeastern end. It is the busiest shipping area in the world. It is about long and varies in width from at its widest to at its narrowest in the Strait of Dover."English Channel". ''The Columbia Encyclopedia'', 2004. It is the smallest of the shallow seas around the continental shelf of Europe, covering an area of some . The Channel was a key factor in Britain becoming a naval superpower and has been utilised by Britain as a natural def ...
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Mudflat
Mudflats or mud flats, also known as tidal flats or, in Ireland, slob or slobs, are coastal wetlands that form in intertidal areas where sediments have been deposited by tides or rivers. A global analysis published in 2019 suggested that tidal flat ecosystems are as extensive globally as mangroves, covering at least of the Earth's surface. / They are found in sheltered areas such as bays, bayous, lagoons, and estuaries; they are also seen in freshwater lakes and salty lakes (or inland seas) alike, wherein many rivers and creeks end. Mudflats may be viewed geologically as exposed layers of bay mud, resulting from deposition of estuarine silts, clays and aquatic animal detritus. Most of the sediment within a mudflat is within the intertidal zone, and thus the flat is submerged and exposed approximately twice daily. A recent global remote sensing analysis estimated that approximately 50% of the global extent of tidal flats occurs within eight countries (Indonesia, China, Austral ...
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Intertidal
The intertidal zone, also known as the foreshore, is the area above water level at low tide and underwater at high tide (in other words, the area within the tidal range). This area can include several types of Marine habitat, habitats with various species of Marine life, life, such as seastars, Sea urchin, sea urchins, and many species of coral with regional differences in biodiversity. Sometimes it is referred to as the ''littoral zone'' or ''shore, seashore'', although those can be defined as a wider region. The well-known area also includes steep rocky Cliff, cliffs, sandy Beach, beaches, Bog, bogs or wetlands (e.g., vast Mudflat, mudflats). The area can be a narrow strip, as in Pacific island, Pacific islands that have only a narrow tidal range, or can include many meters of shoreline where shallow beach slopes interact with high tidal excursion. The peritidal zone is similar but somewhat wider, extending from above the highest tide level to below the lowest. Organisms in t ...
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Redruth And Chasewater Railway
The Redruth and Chasewater Railway, (otherwise called the ''Redruth and Chacewater Railway'' using modern spelling), was an early mineral railway line in Cornwall, England, UK. It opened in 1825 and was built to convey the output from copper mines in the Gwennap area to wharves on Restronguet Creek (off the Fal Estuary) around Devoran, and to bring in coal to fuel mine engines; later it carried timber for pit props and also house coal. A little over long, it was built to a narrow gauge and used horse traction at first, later using steam locomotives. Solely dependent on the economy of the mines it served, it prospered when they did, and when they declined, the railway declined too; it finally closed in 1915. It never carried passengers. Much of its route can still be traced, and part of it forms the course of the Redruth and Chasewater Railway Trail, an outdoor leisure facility. History Antecedents Prior to the nineteenth century, much mineral extraction had taken place in t ...
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Mining In Cornwall
Mining in Cornwall and Devon, in the southwest of England, began in the early Bronze Age, around 2150 BC. Tin, and later copper, were the most commonly extracted metals. Some tin mining continued long after the mining of other metals had become unprofitable, but ended in the late 20th century. In 2021, it was announced that a new mine was extracting battery-grade lithium carbonate, more than 20 years after the closure of the last South Crofty tin mine in Cornwall in 1998. Historically, tin and copper as well as a few other metals (e.g. arsenic, silver, and zinc) have been mined in Cornwall and Devon. Tin deposits still exist in Cornwall, and there has been talk of reopening the South Crofty tin mine. In addition, work has begun on re-opening the Hemerdon tungsten and tin mine in south-west Devon. In view of the economic importance of mines and quarries, geological studies have been conducted; about forty distinct minerals have been identified from type localities in Cornwa ...
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Copper
Copper is a chemical element with the symbol Cu (from la, cuprum) and atomic number 29. It is a soft, malleable, and ductile metal with very high thermal and electrical conductivity. A freshly exposed surface of pure copper has a pinkish-orange color. Copper is used as a conductor of heat and electricity, as a building material, and as a constituent of various metal alloys, such as sterling silver used in jewelry, cupronickel used to make marine hardware and coins, and constantan used in strain gauges and thermocouples for temperature measurement. Copper is one of the few metals that can occur in nature in a directly usable metallic form ( native metals). This led to very early human use in several regions, from circa 8000 BC. Thousands of years later, it was the first metal to be smelted from sulfide ores, circa 5000 BC; the first metal to be cast into a shape in a mold, c. 4000 BC; and the first metal to be purposely alloyed with another metal, tin, to create ...
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Chycoose
Chycoose ( kw, Chy'n Coos, meaning ''house of the wood''), Point and Penpol ( kw, Pen Pol, meaning ''head of a creek'') form a coastal settlement around Penpol Creek in Cornwall, England, United Kingdom. The creek is a ria, a tidal inlet on the north side of Restronguet Creek. It is situated approximately three-quarters of a mile (1 km) west of Feock village which is four miles (6.5 km) south of Truro. Chycoose is on the west bank of Penpol Creek and Penpol hamlet is at the north end of the creek. Point is on a small promontory where Penpol Creek joins Restronguet Creek. Trolver, a small coastal settlement, extends along the east side of the Penpol Creek south from Penpol. Today, all four settlements are residential in character with many of the houses having river frontages and all four are in the civil parish of Feock. Cornwall Council online mapping. Retrieved May 2010 However, until the beginning of the 20th century, Restronguet Creek was a busy commercial wa ...
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