117-525: St Andrews Links in the town of St Andrews , Fife , Scotland , is regarded as the "Home of Golf ". It has one of the oldest courses in the world, where the game has been played since the 15th century. Today there are seven public golf courses : the Balgove, Eden, Jubilee, Strathtyrum, New, and the Old Course all on the links, and The Castle Course, a mile to the east of the town. The famous Old Course
234-429: A glacial armor . Ice can not only erode mountains but also protect them from erosion. Depending on glacier regime, even steep alpine lands can be preserved through time with the help of ice. Scientists have proved this theory by sampling eight summits of northwestern Svalbard using Be10 and Al26, showing that northwestern Svalbard transformed from a glacier-erosion state under relatively mild glacial maxima temperature, to
351-466: A cliff-top to the north of the town. The castle was first erected around 1200 as the residence, prison and fortress of the bishops of the diocese. Several reconstructions occurred in subsequent centuries, most notably due to damage incurred in the Wars of Scottish Independence . The castle was occupied, besieged and stormed during The Rough Wooing and was severely damaged in the process. The majority of
468-538: A community based station which broadcast from the University of St Andrews . The St Andrews Citizen is the town's local newspaper including student newspapers which are published from the University of St Andrews , The Saint and The Stand. St Andrews was once bounded by several "ports" (the Lowland Scots word for a town gate). Two are still extant: So'gait port (South Street, now called West Port) and
585-426: A considerable depth. A gully is distinguished from a rill based on a critical cross-sectional area of at least one square foot, i.e. the size of a channel that can no longer be erased via normal tillage operations. Extreme gully erosion can progress to formation of badlands . These form under conditions of high relief on easily eroded bedrock in climates favorable to erosion. Conditions or disturbances that limit
702-408: A fall in sea level, can produce a distinctive landform called a raised beach . Chemical erosion is the loss of matter in a landscape in the form of solutes . Chemical erosion is usually calculated from the solutes found in streams. Anders Rapp pioneered the study of chemical erosion in his work about Kärkevagge published in 1960. Formation of sinkholes and other features of karst topography
819-409: A few millimetres, or for thousands of kilometres. Agents of erosion include rainfall ; bedrock wear in rivers ; coastal erosion by the sea and waves ; glacial plucking , abrasion , and scour; areal flooding; wind abrasion; groundwater processes; and mass movement processes in steep landscapes like landslides and debris flows . The rates at which such processes act control how fast
936-485: A glacier-armor state occupied by cold-based, protective ice during much colder glacial maxima temperatures as the Quaternary ice age progressed. These processes, combined with erosion and transport by the water network beneath the glacier, leave behind glacial landforms such as moraines , drumlins , ground moraine (till), glaciokarst , kames, kame deltas, moulins, and glacial erratics in their wake, typically at
1053-464: A homogeneous bedrock erosion pattern, curved channel cross-section beneath the ice is created. Though the glacier continues to incise vertically, the shape of the channel beneath the ice eventually remain constant, reaching a U-shaped parabolic steady-state shape as we now see in glaciated valleys . Scientists also provide a numerical estimate of the time required for the ultimate formation of a steady-shaped U-shaped valley —approximately 100,000 years. In
1170-423: A large river can remove enough sediments to produce a river anticline , as isostatic rebound raises rock beds unburdened by erosion of overlying beds. Shoreline erosion, which occurs on both exposed and sheltered coasts, primarily occurs through the action of currents and waves but sea level (tidal) change can also play a role. Hydraulic action takes place when the air in a joint is suddenly compressed by
1287-492: A mountain mass similar to the Himalaya into an almost-flat peneplain if there are no significant sea-level changes . Erosion of mountains massifs can create a pattern of equally high summits called summit accordance . It has been argued that extension during post-orogenic collapse is a more effective mechanism of lowering the height of orogenic mountains than erosion. Examples of heavily eroded mountain ranges include
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#17327873967831404-481: A move to St Leonards House was made. The school is now spread across thirty acres between Pends Road and Kinnesburn. A private school for boys was also set up in 1933 as New Park . The operations of the school merged with the middle and junior sections of St Leonards to become St Leonards-New Park in 2005. Erosion Erosion is the action of surface processes (such as water flow or wind ) that removes soil , rock , or dissolved material from one location on
1521-464: A replacement for Madras College on a single site have been ongoing since 2006. Originally, the school was in negotiations with the University of St Andrews for a joint new build at Lang Lands on land owned by the university. The plans, which were scrapped in August 2011, would have seen the school share the university's playing fields. In October 2011, a scoring exercise drawn up by the council to decide
1638-468: A scheduled monument administered by Historic Environment Scotland . The apse of the Dominican friary , Blackfriars , can still be seen on South Street (between Madras College and Bell Street). Other defunct religious houses that existed in the medieval town, though less visible, have left traces, as for instance the leper hospital at St Nicholas farmhouse (The Steading) between Albany Park and
1755-515: A school which was able to teach both poor and privileged children on one site. The high reputation of the school meant that many children came from throughout Britain to be taught there, often lodging with masters or residents in the town. The school was located on two campuses – Kilrymont, (which opened in 1967) and South Street (incorporating the original 1833 building). Pupils in S1-S3 are served by Kilrymont and S4-S6 by South Street. Plans to build
1872-432: A surface is eroded. Typically, physical erosion proceeds the fastest on steeply sloping surfaces, and rates may also be sensitive to some climatically controlled properties including amounts of water supplied (e.g., by rain), storminess, wind speed, wave fetch , or atmospheric temperature (especially for some ice-related processes). Feedbacks are also possible between rates of erosion and the amount of eroded material that
1989-501: A wave closing the entrance of the joint. This then cracks it. Wave pounding is when the sheer energy of the wave hitting the cliff or rock breaks pieces off. Abrasion or corrasion is caused by waves launching sea load at the cliff. It is the most effective and rapid form of shoreline erosion (not to be confused with corrosion ). Corrosion is the dissolving of rock by carbonic acid in sea water. Limestone cliffs are particularly vulnerable to this kind of erosion. Attrition
2106-412: A weak bedrock (containing material more erodible than the surrounding rocks) erosion pattern, on the contrary, the amount of over deepening is limited because ice velocities and erosion rates are reduced. Glaciers can also cause pieces of bedrock to crack off in the process of plucking. In ice thrusting, the glacier freezes to its bed, then as it surges forward, it moves large sheets of frozen sediment at
2223-625: Is 31.3 °C (88.3 °F), recorded in July 2022. In a typical year, the warmest day should reach 26.1 °C (79.0 °F) and a total of 2 days should record a temperature of 25.1 °C (77.2 °F) or above. The warmest calendar month (since 1960) was July 2006, with a mean temperature of 16.8 °C (62.2 °F) (mean maximum of 21.6 °C (70.9 °F), mean minimum of 11.9 °C (53.4 °F)) The absolute minimum temperature (since 1960) stands at −14.5 °C (5.9 °F) recorded during February 1972, although in an 'average' year,
2340-544: Is a town on the east coast of Fife in Scotland, 10 miles (16 kilometres) southeast of Dundee and 30 miles (50 kilometres) northeast of Edinburgh . St Andrews had a recorded population of 16,800 as of 2011 , making it Fife's fourth-largest settlement and 45th most populous settlement in Scotland . The town is home to the University of St Andrews , the third oldest university in the English-speaking world and
2457-546: Is already carried by, for example, a river or glacier. The transport of eroded materials from their original location is followed by deposition, which is arrival and emplacement of material at a new location. While erosion is a natural process, human activities have increased by 10–40 times the rate at which soil erosion is occurring globally. At agriculture sites in the Appalachian Mountains , intensive farming practices have caused erosion at up to 100 times
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#17327873967832574-494: Is also more prone to mudslides, landslides, and other forms of gravitational erosion processes. Tectonic processes control rates and distributions of erosion at the Earth's surface. If the tectonic action causes part of the Earth's surface (e.g., a mountain range) to be raised or lowered relative to surrounding areas, this must necessarily change the gradient of the land surface. Because erosion rates are almost always sensitive to
2691-484: Is an example of extreme chemical erosion. Glaciers erode predominantly by three different processes: abrasion/scouring, plucking , and ice thrusting. In an abrasion process, debris in the basal ice scrapes along the bed, polishing and gouging the underlying rocks, similar to sandpaper on wood. Scientists have shown that, in addition to the role of temperature played in valley-deepening, other glaciological processes, such as erosion also control cross-valley variations. In
2808-409: Is distinguished from changes on the bed of the watercourse, which is referred to as scour . Erosion and changes in the form of river banks may be measured by inserting metal rods into the bank and marking the position of the bank surface along the rods at different times. Thermal erosion is the result of melting and weakening permafrost due to moving water. It can occur both along rivers and at
2925-405: Is of two primary varieties: deflation , where the wind picks up and carries away loose particles; and abrasion , where surfaces are worn down as they are struck by airborne particles carried by wind. Deflation is divided into three categories: (1) surface creep , where larger, heavier particles slide or roll along the ground; (2) saltation , where particles are lifted a short height into
3042-507: Is related to tourism. St Andrews is often considered as an expensive destination. In 2016, St Andrews was reported to be home to the "Most Expensive Street in Scotland", with average house prices in The Scores in excess of 2 million pounds. St Andrews has a temperate maritime climate , which is relatively mild despite its northerly latitude . Winters are not as cold as one might expect, considering that Moscow and Labrador lie on
3159-758: Is represented by Wendy Chamberlain , MP of the Scottish Liberal Democrats . For the purposes of the Scottish Parliament , St Andrews forms part of the North East Fife constituency. The North East Fife Scottish Parliament (or Holyrood ) constituency created in 1999 is one of nine within the Mid Scotland and Fife electoral region. Each constituency elects one Member of the Scottish Parliament (MSP) by
3276-404: Is sparse and soil is dry (and so is more erodible). Other climatic factors such as average temperature and temperature range may also affect erosion, via their effects on vegetation and soil properties. In general, given similar vegetation and ecosystems, areas with more precipitation (especially high-intensity rainfall), more wind, or more storms are expected to have more erosion. In some areas of
3393-478: Is the Stagecoach bus station located near the town centre. Stagecoach's Route 99 (and its alternate routes 99A, 99B, 99C, 99D) connects St Andrews to Dundee via Leuchars with buses up to every ten minutes. Moffat & Williamson operates Route 92 (and 92A, 92B, 92C) on a lesser frequency from Balmullo via Leuchars station to St Andrews before looping the town. There are also some local bus service that links
3510-457: Is the main climatic factor governing soil erosion by water. The relationship is particularly strong if heavy rainfall occurs at times when, or in locations where, the soil's surface is not well protected by vegetation . This might be during periods when agricultural activities leave the soil bare, or in semi-arid regions where vegetation is naturally sparse. Wind erosion requires strong winds, particularly during times of drought when vegetation
3627-400: Is where particles/sea load carried by the waves are worn down as they hit each other and the cliffs. This then makes the material easier to wash away. The material ends up as shingle and sand. Another significant source of erosion, particularly on carbonate coastlines, is boring, scraping and grinding of organisms, a process termed bioerosion . Sediment is transported along the coast in
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3744-452: Is widely considered one of the finest courses in the world. The courses of St Andrews Links are owned by the local authorities and operated by St Andrews Links Trust, a charitable organization. In general, St Andrews is a popular hub for golf tourism, as there is a high density of links and heathland courses in the area. In addition to the public courses there are two courses at the privately owned Fairmont Hotel (Torrance and Kittocks) to
3861-472: The Earth's crust and then transports it to another location where it is deposited . Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as physical or mechanical erosion; this contrasts with chemical erosion, where soil or rock material is removed from an area by dissolution . Eroded sediment or solutes may be transported just
3978-664: The Great Plains , it is estimated that soil loss due to wind erosion can be as much as 6100 times greater in drought years than in wet years. Mass wasting or mass movement is the downward and outward movement of rock and sediments on a sloped surface, mainly due to the force of gravity . Mass wasting is an important part of the erosional process and is often the first stage in the breakdown and transport of weathered materials in mountainous areas. It moves material from higher elevations to lower elevations where other eroding agents such as streams and glaciers can then pick up
4095-652: The Redistribution of Seats Act 1885 , there was one MP sitting for St Andrews Burgh (which would include Anstruther Easter, Anstruther Wester, Crail , Cupar, Kilrenny and Pittenweem). St Andrews now forms part of the North East Fife constituency, electing one Member of Parliament (MP) to the House of Commons of the Parliament of the United Kingdom by the first past the post system. The constituency
4212-533: The St Andrews Links Trophy . Initially a 12-hole course, it was expanded to 18 holes in 1905. The course has seen considerable developments under the management of Willie Auchterlonie, Donald Steel, David Wilson and Graeme Taylor. It now plays at around 6,745 yards, and is host to the St Andrews Links Trophy . The Jubilee is one of several courses in Scotland that are under threat from erosion . The Strathtyrum Course, opened in July 1993, became
4329-737: The Timanides of Northern Russia. Erosion of this orogen has produced sediments that are now found in the East European Platform , including the Cambrian Sablya Formation near Lake Ladoga . Studies of these sediments indicate that it is likely that the erosion of the orogen began in the Cambrian and then intensified in the Ordovician . If the erosion rate exceeds soil formation , erosion destroys
4446-416: The accumulation zone above the glacial equilibrium line altitude), which causes increased rates of erosion of the mountain, decreasing mass faster than isostatic rebound can add to the mountain. This provides a good example of a negative feedback loop . Ongoing research is showing that while glaciers tend to decrease mountain size, in some areas, glaciers can actually reduce the rate of erosion, acting as
4563-405: The impact of a falling raindrop creates a small crater in the soil , ejecting soil particles. The distance these soil particles travel can be as much as 0.6 m (2.0 ft) vertically and 1.5 m (4.9 ft) horizontally on level ground. If the soil is saturated , or if the rainfall rate is greater than the rate at which water can infiltrate into the soil, surface runoff occurs. If
4680-530: The links were subsequently confirmed in local and royal charters. The land was acquired by James Cheape, owner of the adjacent Strathtyrum estate, in 1821 and sold by his brother's grandson, also named James Cheape, to the Royal and Ancient Golf Club of St Andrews in 1893. Control of St Andrews Links was regulated by the St. Andrews Links Act 1894 and St. Andrews Links Order Confirmation Act 1974 which resulted in
4797-455: The lower crust and mantle . Because tectonic processes are driven by gradients in the stress field developed in the crust, this unloading can in turn cause tectonic or isostatic uplift in the region. In some cases, it has been hypothesised that these twin feedbacks can act to localize and enhance zones of very rapid exhumation of deep crustal rocks beneath places on the Earth's surface with extremely high erosion rates, for example, beneath
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4914-407: The surface runoff which may result from rainfall, produces four main types of soil erosion : splash erosion , sheet erosion , rill erosion , and gully erosion . Splash erosion is generally seen as the first and least severe stage in the soil erosion process, which is followed by sheet erosion, then rill erosion and finally gully erosion (the most severe of the four). In splash erosion ,
5031-445: The 18th century, the town was still in decline, but despite this the town was becoming known for having links 'well known to golfers'. By the 19th century, the town began to expand beyond the original medieval boundaries with streets of new houses and town villas being built. Today, St Andrews is served by education, golf and the tourist and conference industry. In 1951, The Masque of St. Andrews , which dramatised important events in
5148-556: The 1971–2000 observation period. The St Andrews Railway provided a connection to the main Edinburgh to Aberdeen Line at Leuchars railway station . This service was ended in 1969. The St Andrews Rail Link project aims at realising a new high-speed twin-cord mainline rail link via Cupar to the south and west and via Leuchars to the north. Nowadays, the only public transport to reach trains at Leuchars or to connect other towns in Fife
5265-499: The 21st century, a strong link has been drawn between the increase in storm frequency with an increase in sediment load in rivers and reservoirs, highlighting the impacts climate change can have on erosion. Vegetation acts as an interface between the atmosphere and the soil. It increases the permeability of the soil to rainwater, thus decreasing runoff. It shelters the soil from winds, which results in decreased wind erosion, as well as advantageous changes in microclimate. The roots of
5382-650: The East Sands leisure centre. Today, St Andrews is home to one secondary school, one private school and three primary schools. Canongate Primary School, which opened in 1972 is located off the Canongate, beside the St Andrews Botanic Garden . The school roll was recorded in February 2008 as 215. Lawhead Primary School, which opened in 1974 is on the western edge of the town. The school roll
5499-642: The Scores to the north and the Kinness Burn to the south. The burgh soon became the ecclesiastical capital of Scotland, a position which was held until the Scottish Reformation . The famous cathedral , the largest in Scotland, now lies in ruins. St Andrews is also known globally as the " home of golf ". This is in part because of The Royal and Ancient Golf Club of St Andrews , founded in 1754, which until 2004 exercised legislative authority over
5616-539: The Sea Yett (as The Pends terminates to the harbour). The West Port is one of few surviving town "Ports" in Scotland and is a scheduled monument . The towers were influenced by those seen at the base of the Netherbow Port in Edinburgh . The central archway which displays semi-octagonal "rownds" and "battling" is supported by corbelling and neatly moulded passageways. Side arches and relief panels were added to
5733-652: The St Andrews economy. The Jubilee Course is the third championship golf course at the Home of Golf. It was named after Queen Victoria 's Diamond Jubilee celebration in 1897. Originally intended for Victorian dressed ladies, and other golf beginners, it has evolved into one of the hardest courses at St Andrews Links. The course is commonly used to test junior and amateur golfers for the British Mid-Amateur Golf Championship, as well as
5850-433: The air, and bounce and saltate across the surface of the soil; and (3) suspension , where very small and light particles are lifted into the air by the wind, and are often carried for long distances. Saltation is responsible for the majority (50–70%) of wind erosion, followed by suspension (30–40%), and then surface creep (5–25%). Wind erosion is much more severe in arid areas and during times of drought. For example, in
5967-401: The architecture feature of the church was lost in the re-building by Robert Balfour between 1798 and 1800. The church was later restored to a (more elaborately decorated) approximation of its medieval appearance between 1907 and 1909 by MacGregor Chambers. To the east of the town centre, lie the ruins of St Andrews Cathedral . This was at one time Scotland's largest building, originated in
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#17327873967836084-470: The base along with the glacier. This method produced some of the many thousands of lake basins that dot the edge of the Canadian Shield . Differences in the height of mountain ranges are not only being the result tectonic forces, such as rock uplift, but also local climate variations. Scientists use global analysis of topography to show that glacial erosion controls the maximum height of mountains, as
6201-525: The best location for the new Madras College was put before parents, staff and the local community to ask for their views. A £40-million redevelopment of the Kilrymont building proved to be most popular and was officially given the go-ahead in November 2011. This decision was met with controversy from parents, staff and the local community. Following a decision from a group of senior councillors to analyse
6318-463: The castle seen today dates to between 1549 and 1571. The work was commissioned by John Hamilton (archbishop of St Andrews) in a renaissance style which made the building a comfortable, palatial residence while still remaining well-fortified. After the Reformation, the castle passed to several owners, who could not maintain its structure and the building deteriorated into a ruin. The castle is now
6435-522: The coast. Rapid river channel migration observed in the Lena River of Siberia is due to thermal erosion, as these portions of the banks are composed of permafrost-cemented non-cohesive materials. Much of this erosion occurs as the weakened banks fail in large slumps. Thermal erosion also affects the Arctic coast , where wave action and near-shore temperatures combine to undercut permafrost bluffs along
6552-409: The coastline. Where there is a bend in the coastline, quite often a buildup of eroded material occurs forming a long narrow bank (a spit ). Armoured beaches and submerged offshore sandbanks may also protect parts of a coastline from erosion. Over the years, as the shoals gradually shift, the erosion may be redirected to attack different parts of the shore. Erosion of a coastal surface, followed by
6669-416: The coldest night should only fall to −8.3 °C (17.1 °F). Typically, just short of 60 nights a year will experience an air frost. The coldest calendar month (since 1960) was December 2010, with a mean temperature of −0.8 °C (30.6 °F) (mean maximum 1.9 °C (35.4 °F), mean minimum −3.5 °C (25.7 °F) ) Rainfall, at little more than 650 mm per year makes St Andrews one of
6786-530: The creation of the St Andrews Links Trust. The Balgove Course, named after the farm on which it was built, is a 1,520 yard, par 30, nine-hole course. It was originally opened in 1972 and remodeled in 1993. The Castle Course opened in June 2008, becoming the seventh public course at St Andrews. It is set on a rugged-cliff top a mile to the east of St Andrews with extensive views over the town, and
6903-411: The direction of the prevailing current ( longshore drift ). When the upcurrent supply of sediment is less than the amount being carried away, erosion occurs. When the upcurrent amount of sediment is greater, sand or gravel banks will tend to form as a result of deposition . These banks may slowly migrate along the coast in the direction of the longshore drift, alternately protecting and exposing parts of
7020-424: The driest parts of Scotland, shielded from Atlantic weather systems by several mountain ranges. Over 1 mm of rain is recorded on just under 117 days of the year. Sunshine, averaging in excess of 1,500 hours a year is amongst the highest for Scotland, and comparable to inland parts of Southern England. St Andrews is about the furthest north annual levels of above 1500 hours are encountered. All averages refer to
7137-484: The ecclesiastical capital of Scotland, the town now had vast economic and political influence within Europe as a cosmopolitan town. The Scottish Parliament met in the town in 1304, when King Edward I , in his capacity as overlord of Scotland, came to be received by Bishop William de Lamberton . As many as 130 landowners turned up to witness the event ranging from Sir John of Cambo to Sir William Murray of Fort. In 1559,
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#17327873967837254-405: The extremely steep terrain of Nanga Parbat in the western Himalayas . Such a place has been called a " tectonic aneurysm ". Human land development, in forms including agricultural and urban development, is considered a significant factor in erosion and sediment transport , which aggravate food insecurity . In Taiwan, increases in sediment load in the northern, central, and southern regions of
7371-477: The first Monday of the month in the Council Chamber of St Andrews Town Hall , forms the lowest tier of governance whose statutory role is to communicate local opinion to local and central government. The current chair is Mrs Penelope Fraser. The chair uses the honorary title of Provost of St Andrews on official and ceremonial occasions, this ancient title having been revived to mark the 400th Anniversary of
7488-787: The first new 18 hole layout at St Andrews in nearly 80 years. It was built on land that was previously part of the Strathtyrum estate and sold to the St Andrews Links Trust by Mrs Gladys Cheape in 1986. The Old Course, believed to be the oldest golf course in the world, dates back more than 600 years. The New Course, located adjacent to the Old Course, was paid for and commissioned by the Royal and Ancient Golf Club who asked Old Tom Morris to be designer. The New Course opened for play in 1895. St Andrews St Andrews ( Latin : S. Andrea(s) ; Scots : Saunt Aundraes ; Scottish Gaelic : Cill Rìmhinn , pronounced [kʰʲɪʎˈrˠiː.ɪɲ])
7605-436: The first past the post system of election, and the region elects seven additional members to produce a form of proportional representation. The seat was won at the 2016 Scottish Parliament Election by Willie Rennie , for the Scottish Liberal Democrats . According to the 2001 census, St Andrews had a total population of 14,209. The population increased to around 16,680 in 2008 and 16,800 in 2012 The demographic make-up of
7722-582: The flood regions result from glacial Lake Missoula , which created the channeled scablands in the Columbia Basin region of eastern Washington . Wind erosion is a major geomorphological force, especially in arid and semi-arid regions. It is also a major source of land degradation, evaporation, desertification, harmful airborne dust, and crop damage—especially after being increased far above natural rates by human activities such as deforestation , urbanization , and agriculture . Wind erosion
7839-502: The game worldwide (except in the United States and Mexico). It is also because the famous Old Course of St Andrews Links (acquired by the town in 1894) is the most frequent venue for The Open Championship , the oldest of golf 's four major championships . Visitors travel to St Andrews in great numbers for several courses ranked amongst the finest in the world, as well as for the sandy beaches. The Martyrs Memorial, erected to
7956-592: The granting of Royal Burgh status to St Andrews in 1620 by King James VI & I. In the early days of the United Kingdom, following implementation of the union of 1707 , St Andrews elected one Member of Parliament (MP) to the United Kingdom Parliament. Following the implementation of the Reform Act 1832 St Andrews Burgh merged with Anstruther for the purposes of electing one MP to the United Kingdom Parliament. Following implementation of
8073-417: The growth of protective vegetation ( rhexistasy ) are a key element of badland formation. Valley or stream erosion occurs with continued water flow along a linear feature. The erosion is both downward , deepening the valley , and headward , extending the valley into the hillside, creating head cuts and steep banks. In the earliest stage of stream erosion, the erosive activity is dominantly vertical,
8190-595: The honour of Patrick Hamilton , George Wishart , and other martyrs of the Reformation epoch, stands at the west end of the Scores on a cliff overlooking the sea. The civil parish has a population of 18,421 (in 2011). The town also contains numerous museums, a botanic garden and an aquarium. The earliest recorded name of the area is Cennrígmonaid . This is Old Gaelic and composed of the elements cenn (head, peninsula), ríg (king) and monaid (moor). This became Cell Rígmonaid ( cell meaning church) and
8307-411: The island can be tracked with the timeline of development for each region throughout the 20th century. The intentional removal of soil and rock by humans is a form of erosion that has been named lisasion . Mountain ranges take millions of years to erode to the degree they effectively cease to exist. Scholars Pitman and Golovchenko estimate that it takes probably more than 450 million years to erode
8424-537: The lay-out may have led to the creation of two new streets (North Street and South Street) from the foundations of the new St Andrews Cathedral filling the area inside a two-sided triangle at its apex. The northern boundary of the burgh was the southern side of the Scores (the street between North Street and the sea) with the southern by the Kinness Burn and the western by the West Port. The burgh of St Andrews
8541-409: The local slope (see above), this will change the rates of erosion in the uplifted area. Active tectonics also brings fresh, unweathered rock towards the surface, where it is exposed to the action of erosion. However, erosion can also affect tectonic processes. The removal by erosion of large amounts of rock from a particular region, and its deposition elsewhere, can result in a lightening of the load on
8658-418: The material and move it to even lower elevations. Mass-wasting processes are always occurring continuously on all slopes; some mass-wasting processes act very slowly; others occur very suddenly, often with disastrous results. Any perceptible down-slope movement of rock or sediment is often referred to in general terms as a landslide . However, landslides can be classified in a much more detailed way that reflects
8775-407: The material has begun to slide downhill. In some cases, the slump is caused by water beneath the slope weakening it. In many cases it is simply the result of poor engineering along highways where it is a regular occurrence. Surface creep is the slow movement of soil and rock debris by gravity which is usually not perceptible except through extended observation. However, the term can also describe
8892-438: The mechanisms responsible for the movement and the velocity at which the movement occurs. One of the visible topographical manifestations of a very slow form of such activity is a scree slope. Slumping happens on steep hillsides, occurring along distinct fracture zones, often within materials like clay that, once released, may move quite rapidly downhill. They will often show a spoon-shaped isostatic depression , in which
9009-539: The mesolithic (middle Stone Age) came from the plains in Northern Europe between 10,000 and 5,000 BCE. This was followed by the nomadic people who settled around the modern town around 4,500 BCE as farmers clearing the area of woodland and building monuments. During the Iron Age/Early Middle ages, a fortified enclosure, potentially a hillfort, was established on East Balrymonth hill, a mile to
9126-484: The morphologic impact of glaciations on active orogens, by both influencing their height, and by altering the patterns of erosion during subsequent glacial periods via a link between rock uplift and valley cross-sectional shape. At extremely high flows, kolks , or vortices are formed by large volumes of rapidly rushing water. Kolks cause extreme local erosion, plucking bedrock and creating pothole-type geographical features called rock-cut basins . Examples can be seen in
9243-404: The most erosion occurs during times of flood when more and faster-moving water is available to carry a larger sediment load. In such processes, it is not the water alone that erodes: suspended abrasive particles, pebbles , and boulders can also act erosively as they traverse a surface, in a process known as traction . Bank erosion is the wearing away of the banks of a stream or river. This
9360-422: The most prestigious golf clubs and, until 2004, one of the two rule-making authorities of golf. The history of St Andrews Links goes back to 1552 when John Hamilton was granted a charter to establish a rabbit warren to the north of the links. The St Andrews Links Charter refers to the public ownership of the links and the right of the people of St Andrews to play golf and other games. The right to play golf on
9477-531: The natural rate of erosion in the region. Excessive (or accelerated) erosion causes both "on-site" and "off-site" problems. On-site impacts include decreases in agricultural productivity and (on natural landscapes ) ecological collapse , both because of loss of the nutrient-rich upper soil layers . In some cases, this leads to desertification . Off-site effects include sedimentation of waterways and eutrophication of water bodies , as well as sediment-related damage to roads and houses. Water and wind erosion are
9594-434: The nutrient-rich upper soil layers . In some cases, the eventual result is desertification . Off-site effects include sedimentation of waterways and eutrophication of water bodies, as well as sediment-related damage to roads and houses. Water and wind erosion are the two primary causes of land degradation ; combined, they are responsible for about 84% of the global extent of degraded land , making excessive erosion one of
9711-512: The oldest in Scotland. It was ranked as the best university in the UK by the 2022 Good University Guide, which is published by The Times and The Sunday Times . According to other rankings, it is ranked as one of the best universities in the United Kingdom. The town is named after Saint Andrew the Apostle . The settlement grew to the west of St Andrews Cathedral , with the southern side of
9828-411: The order of a few centimetres (about an inch) or less and along-channel slopes may be quite steep. This means that rills exhibit hydraulic physics very different from water flowing through the deeper, wider channels of streams and rivers. Gully erosion occurs when runoff water accumulates and rapidly flows in narrow channels during or immediately after heavy rains or melting snow, removing soil to
9945-481: The other potential sites than push ahead with the controversial redevelopment, The new Building was finished in 2021. In August 2020, it was reported that the college will sell its Kilrymont site and built a replacement school at Langlands. The private school known as St Leonards School was initially established as the St Andrews School for girls company in 1877. The present name was taken in 1882 when
10062-556: The plants bind the soil together, and interweave with other roots, forming a more solid mass that is less susceptible to both water and wind erosion. The removal of vegetation increases the rate of surface erosion. The topography of the land determines the velocity at which surface runoff will flow, which in turn determines the erosivity of the runoff. Longer, steeper slopes (especially those without adequate vegetative cover) are more susceptible to very high rates of erosion during heavy rains than shorter, less steep slopes. Steeper terrain
10179-496: The population is much in line with the rest of Scotland. The age group from 16 to 29 forms the largest portion of the population (37%). The median age of males and females living in St Andrews was 29 and 34 years respectively, compared to 37 and 39 years for those in the whole of Scotland. The place of birth of the town's residents was 87.78% United Kingdom (including 61.80% from Scotland), 0.63% Republic of Ireland, 4.18% from other European Union countries, and 7.42% from elsewhere in
10296-556: The port, during the reconstruction between 1843 and 1845. The Category A listed Holy Trinity (also known as the Holy Trinity Parish Church or "town kirk") is the most historic church in St Andrews. The church was initially built on land, close to the south-east gable of the cathedral, around 1144, and was dedicated in 1234 by Bishop David de Bernham . It then moved to a new site on the north side of South Street between 1410 and 1412 by bishop Warlock. Much of
10413-456: The position of abbot of the monastery of St Andrews. The establishment of the present town began around 1140 by Bishop Robert on an L-shaped hill, possibly on the site of the ruined St Andrews Castle . According to a charter of 1170, the new burgh was built to the west of the Cathedral precinct, along Castle Street and possibly as far as what is now known as North Street. This means that
10530-408: The priory of Canons Regular founded by Bishop Robert Kennedy. St Rule's Church, to the south-east of the medieval cathedral is said to date from around 1120 and 1150, being the predecessor of the cathedral. The tall square tower, part of the church, was built to hold the relics of St Andrew and became known as the first cathedral in the town. After the death of Bishop Robert Kennedy, a new cathedral
10647-413: The relief between mountain peaks and the snow line are generally confined to altitudes less than 1500 m. The erosion caused by glaciers worldwide erodes mountains so effectively that the term glacial buzzsaw has become widely used, which describes the limiting effect of glaciers on the height of mountain ranges. As mountains grow higher, they generally allow for more glacial activity (especially in
10764-828: The rolling of dislodged soil particles 0.5 to 1.0 mm (0.02 to 0.04 in) in diameter by wind along the soil surface. On the continental slope , erosion of the ocean floor to create channels and submarine canyons can result from the rapid downslope flow of sediment gravity flows , bodies of sediment-laden water that move rapidly downslope as turbidity currents . Where erosion by turbidity currents creates oversteepened slopes it can also trigger underwater landslides and debris flows . Turbidity currents can erode channels and canyons into substrates ranging from recently deposited unconsolidated sediments to hard crystalline bedrock. Almost all continental slopes and deep ocean basins display such channels and canyons resulting from sediment gravity flows and submarine canyons act as conduits for
10881-515: The runoff has sufficient flow energy , it will transport loosened soil particles ( sediment ) down the slope. Sheet erosion is the transport of loosened soil particles by overland flow. Rill erosion refers to the development of small, ephemeral concentrated flow paths which function as both sediment source and sediment delivery systems for erosion on hillslopes. Generally, where water erosion rates on disturbed upland areas are greatest, rills are active. Flow depths in rills are typically of
10998-429: The same latitude. Daytime temperatures can fall below freezing and average around 4 °C (39 °F). However, the town is subject to strong winds. Night-time frosts are common; however, snowfall is more rare. The nearest official Met Office weather station for which data are available is at Leuchars, about 3 + 1 ⁄ 4 miles (5.2 kilometres) northwest of St Andrews town centre. The absolute maximum temperature
11115-538: The shoreline and cause them to fail. Annual erosion rates along a 100-kilometre (62-mile) segment of the Beaufort Sea shoreline averaged 5.6 metres (18 feet) per year from 1955 to 2002. Most river erosion happens nearer to the mouth of a river. On a river bend, the longest least sharp side has slower moving water. Here deposits build up. On the narrowest sharpest side of the bend, there is faster moving water so this side tends to erode away mostly. Rapid erosion by
11232-593: The soil. Lower rates of erosion can prevent the formation of soil features that take time to develop. Inceptisols develop on eroded landscapes that, if stable, would have supported the formation of more developed Alfisols . While erosion of soils is a natural process, human activities have increased by 10-40 times the rate at which erosion occurs globally. Excessive (or accelerated) erosion causes both "on-site" and "off-site" problems. On-site impacts include decreases in agricultural productivity and (on natural landscapes ) ecological collapse , both because of loss of
11349-471: The south of the town. Today, the outline of the defences are visible on some aerial images. It marks the oldest still extant structure in St Andrews. In the mid-eighth century a monastery was established by the Pictish king Oengus I , traditionally associated with the relics of Saint Andrew , a number of bones supposed to be the saint's arm, kneecap, three fingers and a tooth believed to have been brought to
11466-499: The south of the town; and the Duke's and Drumoig, both inland parkland courses to the west. A few miles further South are the modern links of Kingsbarns and the traditional Balcomie links at Crail . Also nearby are the courses at Elie , Lundin , Leven , Scotscraig and Anstruther . Within 45 minutes drive are Monifieth , Carnoustie and Panmure . St Andrews is also home to The Royal and Ancient Golf Club of St Andrews , one of
11583-433: The terminus or during glacier retreat . The best-developed glacial valley morphology appears to be restricted to landscapes with low rock uplift rates (less than or equal to 2mm per year) and high relief, leading to long-turnover times. Where rock uplift rates exceed 2mm per year, glacial valley morphology has generally been significantly modified in postglacial time. Interplay of glacial erosion and tectonic forcing governs
11700-576: The town by St Regulus. In AD 877, king Causantín mac Cináeda (Constantine I) built a new church for the Culdees at St Andrews and later the same year was captured and executed (or perhaps killed in battle) after defending against Viking raiders. In AD 906, the town became the seat of the bishop of Alba, with the boundaries of the see being extended to include land between the River Forth and River Tweed . In 943 Constantine II abdicated and took
11817-513: The town centre to St Andrews Community Hospital in the south. St Andrews Bus Station provides frequent bus services to most towns in Fife and the nearby city of Dundee via Leuchars, and less frequent services to further destinations like Edinburgh and Stirling . Travellers from Edinburgh Airport may take Route 747 to Halbeath Park & Ride then take X59/X24 to St Andrews. Otherwise, they have to travel to central Edinburgh for train or bus services. Dundee Airport , about 15 miles north of
11934-555: The town fell into decay after the violent Scottish Reformation and the Wars of the Three Kingdoms losing the status of ecclesiastical capital of Scotland. Even the University of St Andrews was considering relocating to Perth around 1697 and 1698. Under the authorisation of the bishop of St Andrews , the town was made a burgh of barony in 1614. Royal Burgh was then granted as a charter by King James VI in 1620. In
12051-479: The town's history, was staged in the Cathedral grounds as part of the Festival of Britain . St Andrews is represented by several tiers of elected government. Prior to 1975 the town was governed by a burgh council, a provost and baillies . From 1975, St Andrews was administered by North East Fife District Council and Fife Regional Council . North East Fife District was abolished in 1996 when Fife Council became
12168-569: The town, has flights that connect with London-City and Belfast-City provided by Loganair . Roads A91 , A915 , A917 , A918 and B939 traverse the town at different locations. Local news and television programmes are provided by BBC Scotland and STV North . Television signals are received from either the Angus or Durris TV transmitters. Local radio stations are BBC Radio Scotland , Kingdom FM , Forth 1 , Greatest Hits Radio Edinburgh, Lothians, Fife and Falkirk , and St Andrews Radio,
12285-409: The transfer of sediment from the continents and shallow marine environments to the deep sea. Turbidites , which are the sedimentary deposits resulting from turbidity currents, comprise some of the thickest and largest sedimentary sequences on Earth, indicating that the associated erosional processes must also have played a prominent role in Earth's history. The amount and intensity of precipitation
12402-563: The two primary causes of land degradation ; combined, they are responsible for about 84% of the global extent of degraded land, making excessive erosion one of the most significant environmental problems worldwide. Intensive agriculture , deforestation , roads , anthropogenic climate change and urban sprawl are amongst the most significant human activities in regard to their effect on stimulating erosion. However, there are many prevention and remediation practices that can curtail or limit erosion of vulnerable soils. Rainfall , and
12519-566: The unitary authority. Fife Council, based in Glenrothes , is now the executive , deliberative and legislative body responsible for local governance . The Scottish Parliament is responsible for devolved matters such as education , health and justice while reserved matters are dealt with by the Parliament of the United Kingdom of Great Britain and Northern Ireland . The Royal Burgh of St Andrews Community Council, meeting on
12636-427: The valleys have a typical V-shaped cross-section and the stream gradient is relatively steep. When some base level is reached, the erosive activity switches to lateral erosion, which widens the valley floor and creates a narrow floodplain. The stream gradient becomes nearly flat, and lateral deposition of sediments becomes important as the stream meanders across the valley floor. In all stages of stream erosion, by far
12753-501: The world (e.g. western Europe ), runoff and erosion result from relatively low intensities of stratiform rainfall falling onto the previously saturated soil. In such situations, rainfall amount rather than intensity is the main factor determining the severity of soil erosion by water. According to the climate change projections, erosivity will increase significantly in Europe and soil erosion may increase by 13–22.5% by 2050 In Taiwan , where typhoon frequency increased significantly in
12870-491: The world (e.g. the mid-western US ), rainfall intensity is the primary determinant of erosivity (for a definition of erosivity check, ) with higher intensity rainfall generally resulting in more soil erosion by water. The size and velocity of rain drops is also an important factor. Larger and higher-velocity rain drops have greater kinetic energy , and thus their impact will displace soil particles by larger distances than smaller, slower-moving rain drops. In other regions of
12987-502: The world. The economic activity of residents aged 16–74 was 23.94% in full-time employment, 8.52% in part-time employment, 4.73% self-employed, 1.94% unemployed, 31.14% students with jobs, 9.08% students without jobs, 13.24% retired, 2.91% looking after home or family, 2.84% permanently sick or disabled, and 1.67% economically inactive for other reasons. St Andrews, whose economy stands at £660 million, relies heavily on tourism and education. In 2016, one out of every five jobs in St Andrews
13104-495: Was Scoticised to Kilrymont . The modern Gaelic spelling is Cill Rìmhinn . It is likely that the Gaelic name represents an adaptation of a Pictish form *Penrimond . The name St Andrews derives from the town's claim to be the resting place of bones of the apostle Andrew . According to legend, St Regulus (or Rule) brought the relics to Kilrymont, where a shrine was established for their safekeeping and veneration while Kilrymont
13221-465: Was begun in 1160 by Bishop Arnold (his successor) on a site adjacent to St Rule's Church. Work on the cathedral was finally completed and consecrated in 1318 by Bishop William de Lamberton with Robert the Bruce (1306–29) present at the ceremony. The cathedral and associated buildings, including St Rule's Church, are protected as a scheduled monument. The ruins of St Andrews Castle are situated on
13338-530: Was designed by the architect David McLay Kidd. The course is a par 71 and measures 6,759 yards from the back tees. The Eden Course opened in 1914 after demand on the existing courses grew. It was designed by Harry Colt , and alterations in 1989 by Donald Steel maintain Colt's standards. It was named after the Eden estuary by which it resides, as the profits from mussels collected there once made up an important part of
13455-468: Was first represented at the great council at Scone Palace in 1357. St Andrews, in particular the large cathedral built in 1160, was the most important centre of pilgrimage in medieval Scotland and one of the most important in Europe. Pilgrims from all over Scotland came in large numbers hoping to be blessed, and in many cases to be cured, at the shrine of Saint Andrew. The presence of the pilgrims brought about increased trade and development. Recognised as
13572-458: Was recorded in September 2009 as 181. Greyfriars Primary School is a Roman Catholic school located in the southern part of the town. Madras College is the sole secondary school in the town. The school which opened to pupils in 1833 was based on a Madras system – founded and endowed by Andrew Bell (1755–1832), a native of the town. Prior to the opening, Bell was interested in the demand for
13689-462: Was renamed in honour of the saint. This is the origin of a third name for the town Kilrule . Its name may also be notable for the lack of apostrophe ; this is due to the fact that the name of the town predates the introduction of the apostrophe into the English language from French in the 16th century. The first inhabitants who settled on the estuary fringes of the rivers Tay and Eden during
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