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Stover, Teigngrace
Stover is a historic estate in the parish of Teigngrace, about half way between the towns of Newton Abbot and Bovey Tracey in South Devon, England. It was bought by James Templer (1722–1782) in 1765 and passed through three generations of that family before being bought by Edward St Maur, 11th Duke of Somerset in 1829. The Georgian mansion house known as Stover House was built by the first James Templer. It is a Grade II* listed building. Since 1932 the house and part of the former estate have been occupied by a private school. 114 acres of the former estate situated south of the A38 now forms Stover Country Park, a nature reserve owned and managed by Devon County Council and open to the public. History Templer family James Templer (1722–1782) was born in Exeter, the son of a tradesman. He made a fortune in India and married Mary Parlby, the sister of his business partner Thomas Parlby in 1747.Ewans, p. 13 In 1765 he purchased the estate of Stover which included a r ...
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James Templer (canal Builder)
James Templer (1748–1813) of Stover House, Teigngrace, Devon, was a Devon landowner and the builder of the Stover Canal. Biography He was the eldest son and heir of James Templer (1722–1782), of Stover House, Teigngrace, Devon, a self-made magnate who had made his fortune building dockyards. Templer was a Master in the Crown Office at London. He inherited the Stover estate in 1782, and began construction of a new church at Teigngrace, built in the local granite from quarries at Hay Tor. This was completed in 1787, and his brother Rev. John Templer (1751–1832) of Lindridge House was the first rector of the church. The mining of ball clay in the area had begun to rapidly expand, and from 1790 Templer built the Stover Canal at his own expense to transport clay to cellars on the banks of the River Teign, for onward transportation by barge down the river estuary to the port of Teignmouth on the coast. In 1776 he married Mary Buller (1749–1829), third daughter of James ...
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Neoclassical Architecture
Neoclassical architecture is an architectural style produced by the Neoclassical movement that began in the mid-18th century in Italy and France. It became one of the most prominent architectural styles in the Western world. The prevailing styles of architecture in most of Europe for the previous two centuries, Renaissance architecture and Baroque architecture, already represented partial revivals of the Classical architecture of ancient Rome and (much less) ancient Greek architecture, but the Neoclassical movement aimed to strip away the excesses of Late Baroque and return to a purer and more authentic classical style, adapted to modern purposes. The development of archaeology and published accurate records of surviving classical buildings was crucial in the emergence of Neoclassical architecture. In many countries, there was an initial wave essentially drawing on Roman architecture, followed, from about the start of the 19th century, by a second wave of Greek Revival architec ...
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Portico
A portico is a porch leading to the entrance of a building, or extended as a colonnade, with a roof structure over a walkway, supported by columns or enclosed by walls. This idea was widely used in ancient Greece and has influenced many cultures, including most Western cultures. Some noteworthy examples of porticos are the East Portico of the United States Capitol, the portico adorning the Pantheon in Rome and the portico of University College London. Porticos are sometimes topped with pediments. Palladio was a pioneer of using temple-fronts for secular buildings. In the UK, the temple-front applied to The Vyne, Hampshire, was the first portico applied to an English country house. A pronaos ( or ) is the inner area of the portico of a Greek or Roman temple, situated between the portico's colonnade or walls and the entrance to the ''cella'', or shrine. Roman temples commonly had an open pronaos, usually with only columns and no walls, and the pronaos could be as long as th ...
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Portland Stone
Portland stone is a limestone from the Tithonian stage of the Jurassic period quarried on the Isle of Portland, Dorset. The quarries are cut in beds of white-grey limestone separated by chert beds. It has been used extensively as a building stone throughout the British Isles, notably in major public buildings in London such as St Paul's Cathedral and Buckingham Palace. Portland Stone is also exported to many countries—being used for example in the United Nations headquarters in New York City. Geology Portland Stone formed in a marine environment, on the floor of a shallow, warm, sub-tropical sea probably near land (as evidenced by fossilized driftwood, which is not uncommon). When seawater is warmed by the sun, its capacity to hold dissolved gas is reduced; consequently, dissolved carbon dioxide (CO2) is released into the atmosphere as a gas. Calcium and bicarbonate ions within the water are then able to combine, to form calcium carbonate (CaCO3) as a precipitate. The proces ...
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Berry Pomeroy Castle
Berry Pomeroy Castle, a Tudor mansion within the walls of an earlier castle, is near the village of Berry Pomeroy, in South Devon, England. It was built in the late 15th century by the Pomeroy family which had held the land since the 11th century. By 1547 the family was in financial difficulties and sold the lands to Edward Seymour, 1st Duke of Somerset. Apart from a short period of forfeit to the Crown after Edward's execution, the castle has remained in the Seymour family ever since, although it was abandoned in the late 17th century when the fourth baronet moved to Wiltshire. After lying in ruins for a hundred years, in the 19th century the castle became celebrated as an example of the "picturesque", and it became a popular tourist attraction, a status which it retains today—aided by its reputation of being haunted. Between 1980 and 1996 the castle was subjected to extensive archaeological excavations that clarified much of its history and overturned beliefs regarding its a ...
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Feudal Barony Of Berry Pomeroy
The Feudal Barony of Berry Pomeroy was one of eight feudal baronies in Devonshire, England, which existed during the mediaeval era. It had its ''caput'' at the manor of Berry Pomeroy, 20 miles south of the City of Exeter and 2 miles east of the town of Totnes, where was situated Totnes Castle, the ''caput'' of the feudal barony of Totnes. The exact location of the 11th-century baron's residence is unclear; perhaps it was next to the parish church on the site of the former rectory known as Berry House, as it is now believed that the nearby ruined Berry Pomeroy Castle was not built until the 15th century. The manor and barony was owned by the Pomeroy family from before 1086 until 1547, when it was purchased by Edward Seymour, 1st Duke of Somerset, in whose family it has since remained. Today the manor and much of the former estate belongs to his descendant the Duke of Somerset, seated at Maiden Bradley House in Wiltshire. Descent Pomeroy ; Ralph de la Pomeroy (died before 1100 ...
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Lord Edward Seymour (died 1593)
Lord Edward Seymour ( 1528 – 2 May 1593), knight, of Berry Pomeroy, Devon, was Sheriff of Devon in 1583. He was knighted by his father the Duke of Somerset on the battlefield of Pinkie on 10 September 1547. Biography Lord Edward Seymour was the second son of Edward Seymour, 1st Duke of Somerset (c. 1500 – 1552) by his first wife Catherine Fillol.Vivian, Heraldic Visitations of Devon, 1895, p. 702 The paternity of Catherine's two sons was questioned by her husband after it was alleged that she had had an affair. This resulted in both her sons being excluded in 1540 from their inheritances and their claims to their father's dignities in favour of his children by his second wife, Ann Stanhope; her eldest son succeeding his father as Duke of Somerset. In June 1553 he received the manor of Berry Pomeroy, Devon, including Berry Pomeroy Castle. Seymour married Margaret Walshe, a daughter and co-heiress of John Walshe (c. 1517 – 1572) of Cathanger, Fivehead, Somerset, Just ...
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Granite Lodge, Stover Country Park (3243)
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly always m ...
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Haytor Granite Tramway
The Haytor Granite Tramway (also called Heytor) was a tramway built to convey granite from Haytor Down, Dartmoor, Devon to the Stover Canal. It was very unusual in that the track was formed of granite sections, shaped to guide the wheels of wagonway, horse-drawn wagons. It was built in 1820; the granite was in demand in the developing cities of England as masonry to construct public buildings and bridges. In 1850 the quarries employed about 100 men but by 1858 they had closed due to the availability of cheaper Cornwall, Cornish granite. The Haytor rocks and quarries are protected from development and disturbance as a Site of Special Scientific Interest. Operation and purpose The granite from the quarries near Haytor Rock was much in demand for construction work in the cities of England, but in an era when railways and reliable roads had not yet been developed, the transport of this heavy and bulky commodity was a significant problem. Coastal shipping was a practicable transport ...
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