Cornish Cross (stone)
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Cornish Cross (stone)
Wayside crosses and Celtic inscribed stones are found in Cornwall in large numbers; the inscribed stones (about 40 in number) are thought to be earlier in date than the crosses and are a product of Celtic Christian society. It is likely that the crosses represent a development from the inscribed stones but nothing is certain about the dating of them. In the late Middle Ages it is likely that their erection was very common and they occur in locations of various types, e.g. by the wayside, in churchyards, and in moorlands. Those by roadsides and on moorlands were doubtless intended as route markings. A few may have served as boundary stones, and others like the wayside shrines found in Catholic European countries. Crosses to which inscriptions have been added must have been memorial stones. According to W. G. V. Balchin "The crosses are either plain or ornamented, invariably carved in granite, and the great majority are of the wheel-headed Celtic type." Their distribution shows a ...
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The Victoria History Of The County Of Cornwall (1906) (14777375892)
''The'' () is a grammatical article in English, denoting persons or things already mentioned, under discussion, implied or otherwise presumed familiar to listeners, readers, or speakers. It is the definite article in English. ''The'' is the most frequently used word in the English language; studies and analyses of texts have found it to account for seven percent of all printed English-language words. It is derived from gendered articles in Old English which combined in Middle English and now has a single form used with pronouns of any gender. The word can be used with both singular and plural nouns, and with a noun that starts with any letter. This is different from many other languages, which have different forms of the definite article for different genders or numbers. Pronunciation In most dialects, "the" is pronounced as (with the voiced dental fricative followed by a schwa) when followed by a consonant sound, and as (homophone of pronoun ''thee'') when followed by a v ...
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Millennium
A millennium (plural millennia or millenniums) is a period of one thousand years, sometimes called a kiloannum (ka), or kiloyear (ky). Normally, the word is used specifically for periods of a thousand years that begin at the starting point (initial reference point) of the calendar in consideration (typically the year "1") and at later years that are whole number multiples of a thousand years after the start point. The term can also refer to an interval of time beginning on any date. Millennia sometimes have religious or theological implications (see millenarianism). The word ''millennium'' derives from the Latin ', thousand, and ', year. Debate over millennium celebrations There was a public debate leading up to the celebrations of the year 2000 as to whether the beginning of that year should be understood as the beginning of the “new” millennium. Historically, there has been debate around the turn of previous decades, centuries, and millennia. The issue arises from the ...
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Quethiock Stone Cross And Church 2007 04 21
Quethiock ( kw, Koosek, meaning ''forested place'') is a village and civil parish in Cornwall, England, United Kingdom, roughly five miles east of Liskeard. According to the 2001 census the parish had a population of 429, increasing to 443 at the 2011 census. The ancient parish church of St Hugh is one of the most notable in Cornwall. The placename derives from the Old Cornish ''cuidoc'' meaning ''wooded place''. In 1871 the population was 661 and the area . Formerly part of the Pentillie Estate and owned by Squire Coryton most of the properties passed into owner occupation after a forced sale to meet Estate Duty in the early 1920s. The village has not had a public house since the closure of the Mason's Arms in the 1920s. There was a post office at Ivydene until the 1960s not long before the closure of the village General Supply Stores which not only sold everything from groceries to petrol and organs but also delivered weekly groceries to farms, mills and cottages throughout a r ...
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Trebartha
Trebartha is a hamlet in Cornwall, England, United Kingdom, in the parish of North Hill and in the valley of the River Lynher. History The manor of Trebartha was recorded in the Domesday Book (1086) when it was held by Thurstan from Robert, Count of Mortain. There was half a hide of land and land for four ploughs. There were three and a half ploughs, two villeins and six smallholders. The value of the manor was 15 shillings. In 1193 the manor was described as ″this desirable manor...″ and the property of Walter Reynell who was castellan of Launceston Castle. Trebarth passed from the Reynells to the Carews and then to the Spoures. Henrie Spoure (died 1603) was one of the owners and in circa 1700 when Edmond Spoure (married to Mary née Rodd) died, the estate passed to his daughter Mary. She married Renatus Bellott of Bochym and they had one son, who died at the age of 8 in 1712. Mary outlived her husband and married Charles Grylls of Court and, was widowed a second time. Mar ...
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Menheniot
Menheniot (pronounced Men-en-yut; kw, Mahynyet) is a civil parish and village in Cornwall, England, United Kingdom. The village is southeast of Liskeard. The meaning of the name is "sanctuary of Neot" (from ''minihi'' and ''Neot''). Menheniot had a population of 1,605 in the 2001 census. This increased slightly to 1,655 at the 2011 census, whereas the ward population at the same census was 3,658. The village has a primary school, a pub, a shop and a post office. Geography To the south of the civil parish is Clicker Tor Quarry, a Site of Special Scientific Interest noted for its geological interest, containing one of the best examples of ultramafic rocks in South West England. At Coldrenick was a black and white mansion dated 1870 by the architect C. F. Hayward. At Merrymeet is an Anglican mission church dedicated to St Mary the Virgin. Hendra Cross Parish church The parish church, located in the village, is dedicated to St Lalluwy. It has a buttressed tower and a spire.
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Linkinhorne
Linkinhorne (in Cornish ''Lanngynhorn'') is a civil parish and village in southeast Cornwall, England, United Kingdom. The village itself is situated at and is approximately four miles (6.5 km) northwest of Callington and seven miles (11 km) south of Launceston.Ordnance Survey: Landranger map sheet 201 ''Plymouth & Launceston'' The parish population at the 2011 census including Downgate was 1,541 Geography As well as Linkinhorne village, other settlements in the parish include (in alphabetical order) Bray Shop, Caradon Town, Downgate, Henwood, Ley Mill, Minions, Plushabridge, Rilla Mill and Upton Cross. The area is bordered by the River Inny in the north-east and Bodmin Moor to the west. The valley of the River Lynher runs through the parish. History Linkinhorne parish is within the Deanery and Hundred of East and is bounded on the north by North Hill and Lezant, on the east by Stoke Climsland and South Hill, on the south and west by St Ive and St Cleer. ...
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Lewannick
Lewannick (; kw, Lannwenek) is a civil parish and village in Cornwall, England, United Kingdom. The village is situated approximately five miles (8 km) southwest of Launceston. The civil parish had a population of 973 at the 2011 census. The parish is rural in character and is within the Deanery and Hundred of East. It is bounded on the north by Trewen and South Petherwin, on the east by Lezant, on the south by North Hill and on the west by Altarnun. The parish church is dedicated to St Martin and is located at . History Evidence of early medieval habitation at Lewannick is in the form of two inscribed pillar stones, each having text in both Latin and ogham characters; on the basis of the ogham text, these stones have been dated as having been inscribed between the fifth and sixth centuries. One is located in the village churchyard, and was dedicated to a "Ingenuus"; the other has been moved inside to the church nave, and both texts mention an "Ulcagnus". Two miles sou ...
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Stone Cross, Lewannick - Geograph
In geology, rock (or stone) is any naturally occurring solid mass or aggregate of minerals or mineraloid matter. It is categorized by the minerals included, its Chemical compound, chemical composition, and the way in which it is formed. Rocks form the Earth's outer solid layer, the Earth's crust, crust, and most of its interior, except for the liquid Earth's outer core, outer core and pockets of magma in the asthenosphere. The study of rocks involves multiple subdisciplines of geology, including petrology and mineralogy. It may be limited to rocks found on Earth, or it may include planetary geology that studies the rocks of other celestial objects. Rocks are usually grouped into three main groups: igneous rocks, sedimentary rocks and metamorphic rocks. Igneous rocks are formed when magma cools in the Earth's crust, or lava cools on the ground surface or the seabed. Sedimentary rocks are formed by diagenesis and lithification of sediments, which in turn are formed by the weathe ...
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Lawhitton
Lawhitton ( kw, Nansgwydhenn) is a village in the civil parish of Lawhitton Rural, in east Cornwall, England, United Kingdom. The village is situated two miles (3 km) southwest of Launceston and half-a-mile west of Cornwall's border with Devon at the River Tamar. Governance The civil parish of Lawhitton was abolished in 1894 and the parishes of Lawhitton Urban and Lawhitton Rural were created. On the 1 April 1922 Lawhitton Urban was abolished into Launceston parish. In 1891 the civil parish of Lawhitton had a population of 361. The parish of Lawhitton Rural is in the Launceston registration district. It is a comparatively small parish and Lawhitton village is the principal settlement. The border with Devon forms the parish's eastern boundary; to the north, it is bounded by St Thomas by Launceston parish; to the west by Launceston parish; and to the south by Lezant parish. The population of Lawhitton Rural in the 2001 census was 270, decreasing to 232 at the 2011 census. ...
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Polyphant Stone
Elvan is a name used in Cornwall and Devon for the native varieties of quartz-porphyry. They are dispersed irregularly in the Devonian series of rocks and some of them make very fine building stones (e.g. Pentewan stone, Polyphant stone and Catacleuse stone). Greenstone is another name for this stone and it is often used for parts of buildings such as doorways so they can be finely carved. Most of the elvan quarries are now disused. Others are quarried in bulk for aggregates commonly used for road-building. More precisely there are two types of rock in this category: one is "white elvan" and the other is "blue elvan". "White elvans" are a group of fine-grained, acid igneous rocks, while "blue elvans" or "greenstones" are various unusual basic igneous rocks. "White elvan" comes from various different locations and is often known as Pentewan stone (or by other names based on the location). Some older descriptions of building stones have called "white elvans" limestone, e.g. in st ...
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Laneast
Laneast ( kw, Lanneyst) is a village and civil parish in Cornwall, England, United Kingdom. It lies above the River Inny valley, about six miles (11 km) west of Launceston. The population in the 2001 census was 164, increasing to 209 at the 2011 census. Parish church The parish church at is dedicated to Saint Sidwell and Saint Gulval or to St Michael. The inclusion of St Gulval in the dedication is apparently due to a mistake by Dr. Oliver who understood entries referring to the church of "St Wolvela of Lanestly" as referring to Laneast whereas "Lanestly" is the old name of Gulval. The church and cemetery were dedicated by Edmund Lacy, Bishop of Exeter in 1436; before that time burials were made at the mother church of St Stephen's.''Cornish Church Guide'' (1925) Truro: Blackford; pp. 128–29 The land of the parish was divided between the hundreds of Lesnewth and East Wivelshire, the church being in the latter. It was founded and until the Reformation maintained by th ...
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Stone Cross On Laneast Downs - Geograph
In geology, rock (or stone) is any naturally occurring solid mass or aggregate of minerals or mineraloid matter. It is categorized by the minerals included, its Chemical compound, chemical composition, and the way in which it is formed. Rocks form the Earth's outer solid layer, the Earth's crust, crust, and most of its interior, except for the liquid Earth's outer core, outer core and pockets of magma in the asthenosphere. The study of rocks involves multiple subdisciplines of geology, including petrology and mineralogy. It may be limited to rocks found on Earth, or it may include planetary geology that studies the rocks of other celestial objects. Rocks are usually grouped into three main groups: igneous rocks, sedimentary rocks and metamorphic rocks. Igneous rocks are formed when magma cools in the Earth's crust, or lava cools on the ground surface or the seabed. Sedimentary rocks are formed by diagenesis and lithification of sediments, which in turn are formed by the weathe ...
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