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Frosterley Marble Detail
Frosterley is a village in the civil parish of Stanhope, in County Durham, England. It is situated in Weardale, on the River Wear close to its confluence with Bollihope Burn; between Wolsingham and Stanhope; west of Durham City and southwest of Newcastle upon Tyne. In the 2001 census Frosterley had a population of 705. Frosterley is on the Weardale Railway. Heritage trains currently run to Stanhope, Wolsingham and Witton-le-Wear. History The area has been inhabited since Mesolithic times: Mesolithic flints and Neolithic stones axes have been found in the vicinity. A bronze spearhead was found in a local quarry dating to the late Bronze Age . The village itself has medieval origins, and although the original houses have long been replaced, the village still retains its medieval pattern. On the north of the village are the remains of St Botolph’s Chapel. What remains is an earthwork mound surrounded by a modern housing estate (Kirk Rise). The site was excavated in 1 ...
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Stanhope, County Durham
Stanhope is a market town and civil parish in the County Durham district, in the ceremonial county of Durham, England. It lies on the River Wear between Eastgate and Frosterley, in the north-east of Weardale. The main A689 road over the Pennines is crossed by the B6278 between Barnard Castle and Shotley Bridge. In 2001 Stanhope had a population of 1,633, in 2019 an estimate of 1,627, and a figure of 1,602 in the 2011 census for the ONS built-up-area which includes Crawleyside. In 2011 the parish population was 4,581. Governance Stanhope parish is the largest parish area in England, at It has some land in common with the neighbouring Wolsingham civil parish. If Stanhope was a district it would be the 135th largest in England and would be 94th if only counting districts that are 2 tier thus excluding unitary authorities and similar, 2 ceremonial counties namely the City of London and Bristol cover a smaller area. On 31 December 1894 "Stanhope Urban" parish was formed ...
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Middle Ages
In the history of Europe, the Middle Ages or medieval period lasted approximately from the 5th to the late 15th centuries, similarly to the post-classical period of global history. It began with the fall of the Western Roman Empire and transitioned into the Renaissance and the Age of Discovery. The Middle Ages is the middle period of the three traditional divisions of Western history: classical antiquity, the medieval period, and the modern period. The medieval period is itself subdivided into the Early, High, and Late Middle Ages. Population decline, counterurbanisation, the collapse of centralised authority, invasions, and mass migrations of tribes, which had begun in late antiquity, continued into the Early Middle Ages. The large-scale movements of the Migration Period, including various Germanic peoples, formed new kingdoms in what remained of the Western Roman Empire. In the 7th century, North Africa and the Middle East—once part of the Byzantine Empire� ...
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Mindat
Mindat may refer to: Places * Mindat District, a district in Chin State, Myanmar (Burma), consisting of two townships and many villages ** Mindat Township, Myanmar *** Mindat, Chin State, a town in Chin State, Myanmar, administrative seat of Mindat Township Other uses * Mindat, alternative name for the Kʼchò language in Myanmar * Mindat Min, a Burmese prince * Mindat.org, an online mineralogy database {{dab, geo ...
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North Pennines
The North Pennines are the northernmost section of the Pennines, a range of hills which run north–south through northern England. They run along the border between County Durham and Northumberland in the east and Cumbria in the west, and are bounded to the north by the Tyne Valley and to the south by the Stainmore Gap. Much of the region is moorland, and it contains significant industrial archaeology. The North Pennines have been designated a national landscape and a UNESCO Global Geopark. Several major rivers rise in the North Pennines, including the Tees and Wear. The part of the area in County Durham, including Teesdale and Weardale, is known as the Durham Dales. Geology The North Pennines are formed from a succession largely of sedimentary rocks laid down during the Palaeozoic era, later intruded by the Whin Sill and affected by glaciation during the Quaternary period. Mud and volcanic ash deposited during the Ordovician and Silurian periods were buried and s ...
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Fluorite
Fluorite (also called fluorspar) is the mineral form of calcium fluoride, CaF2. It belongs to the halide minerals. It crystallizes in isometric cubic habit, although octahedral and more complex isometric forms are not uncommon. The Mohs scale of mineral hardness, based on scratch hardness comparison, defines value 4 as fluorite. Pure fluorite is colourless and transparent, both in visible and ultraviolet light, but impurities usually make it a colorful mineral and the stone has ornamental and lapidary uses. Industrially, fluorite is used as a flux for smelting, and in the production of certain glasses and enamels. The purest grades of fluorite are a source of fluoride for hydrofluoric acid manufacture, which is the intermediate source of most fluorine-containing fine chemicals. Optically clear transparent fluorite has anomalous partial dispersion, that is, its refractive index varies with the wavelength of light in a manner that differs from that of commonly used glasses, ...
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Crinoid
Crinoids are marine invertebrates that make up the class Crinoidea. Crinoids that remain attached to the sea floor by a stalk in their adult form are commonly called sea lilies, while the unstalked forms, called feather stars or comatulids, are members of the largest crinoid order, Comatulida. Crinoids are echinoderms in the phylum Echinodermata, which also includes the starfish, brittle stars, sea urchins and sea cucumbers. They live in both shallow water and in depths of over . Adult crinoids are characterised by having the mouth located on the upper surface. This is surrounded by feeding arms, and is linked to a U-shaped gut, with the anus being located on the oral disc near the mouth. Although the basic echinoderm pattern of fivefold symmetry can be recognised, in most crinoids the five arms are subdivided into ten or more. These have feathery pinnules and are spread wide to gather planktonic particles from the water. At some stage in their lives, most crinoids have a sho ...
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Michael (archangel)
Michael, also called Saint Michael the Archangel, Archangel Michael and Saint Michael the Taxiarch is an archangel and the warrior of God in Christianity, Judaism, and Islam. The earliest surviving mentions of his name are in third- and second-century BC Jewish works, often but not always apocalyptic, where he is the chief of the angels and archangels, and he is the guardian prince of Israel and is responsible for the care of the Israelites, people of Biblical Israel, Israel. Christianity conserved nearly all the Jewish traditions concerning him, and he is mentioned explicitly in Revelation 12:7–12, where he does battle with Satan, and in the Epistle of Jude, where the archangel and the devil dispute over the body of Moses. Old Testament and Apocrypha The Book of Enoch lists him as one of seven archangels (the remaining names are Uriel, Raguel (angel), Raguel, Raphael (archangel), Raphael, Sariel, Gabriel, and Remiel), who, in the Book of Tobit, “stand ready and ente ...
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Durham Cathedral
Durham Cathedral, formally the , is a Church of England cathedral in the city of Durham, England. The cathedral is the seat of the bishop of Durham and is the Mother Church#Cathedral, mother church of the diocese of Durham. It also contains the shrines of the Anglo-Saxons, Anglo-Saxon saints Cuthbert and Bede. There are daily Church of England services at the cathedral, and it received 727,367 visitors in 2019. It is a grade I listed building and forms part of the Durham Castle and Cathedral World Heritage Site. The cathedral is the successor to the Anglo-Saxon Lindisfarne Priory, which was established but abandoned in 875 in the face of Viking Age, Viking raids. The monks settled at Chester-le-Street from 882 until 995, when they moved to Durham. The cathedral remained a monastery until it was Dissolution of the monasteries, dissolved in 1541, since when it has been governed by a Dean of Durham, dean and Chapter (religion), chapter. The cathedral precinct formed part of Durham ...
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Carboniferous Period
The Carboniferous ( ) is a geologic period and system of the Paleozoic era that spans 60 million years, from the end of the Devonian Period Ma (million years ago) to the beginning of the Permian Period, Ma. It is the fifth and penultimate period of the Paleozoic era and the fifth period of the Phanerozoic eon. In North America, the Carboniferous is often treated as two separate geological periods, the earlier Mississippian and the later Pennsylvanian. The name ''Carboniferous'' means "coal-bearing", from the Latin ("coal") and ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern "system" names, it was coined by geologists William Conybeare and William Phillips in 1822, based on a study of the British rock succession. Carboniferous is the period during which both terrestrial animal and land plant life was well established. Stegocephalia (four-limbed vertebrates including true tetrapods), whose forerunners (tetrapodomo ...
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Eilert Ekwall
Bror Oscar Eilert Ekwall (8 January 1877 in Vallsjö – 23 November 1964 in Lund) was a Swedish academic, Professor of English at Sweden's Lund University from 1909 to 1942 and one of the outstanding scholars of the English language in the first half of the 20th century. He wrote works on the history of English, but he is best known as the author of numerous important books on English place-names (in the broadest sense) and personal names. Scholarly works His chief works in this area are ''The Place-Names of Lancashire'' (1922), ''English Place-Names in -ing'' (1923, new edition 1961), ''English River Names'' (1928), ''Studies on English Place- and Personal Names'' (1931), ''Studies on English Place-Names'' (1936), ''Street-Names of the City of London'' (1954), ''Studies on the Population of Medieval London'' (1956), and the monumental ''Concise Oxford Dictionary of English Place-Names'' (1936, new editions 1940, 1947/51 and the last in 1960). The ''Dictionary'' remained the st ...
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Boldon Book
The Boldon Book (also known as the Boldon Buke) contains the results of a survey of the bishopric of Durham that was completed on the orders of Hugh du Puiset, Bishop of Durham, in 1183, designed to assist the administration of the vast diocesan estates. The survey was similar to that of the Domesday Book in the previous century, covering the bishop's lands in what was to become County Durham and other parts of the north east of England that, following the Norman Conquest, were liable to tax by the Prince-Bishop of Durham and not taxed directly by the King of England. It is the first survey undertaken north of the River Tees, where the king's authority was never more than nominal. Like the Domesday Book it is a ''custumal account'' listing the labour, money and produce owed by standing custom to the Bishop. The areas of North Durham (Norhamshire) and Bedlingtonshire are included, but not those areas in the possession of other great northern landowners. The Bishop's manor at Bold ...
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Earthworks (archaeology)
In archaeology, earthworks are artificial changes in land level, typically made from piles of artificially placed or sculpted rocks and soil. Earthworks can themselves be archaeological features, or they can show features beneath the surface. Types There are two broad categories of archaeological earthwork: positive features where earth is built up above the previous ground level, and negative features which are cut into the landscape. Beyond this, earthworks of interest to archaeologists include hill forts, henges, mounds, platform mounds, effigy mounds, enclosure (archaeology), enclosures, long barrows, tumulus, tumuli, ridge and furrow, motte-and-bailey castle, mottes, round barrows, and other tombs. * Hill forts, a type of fort made out of mostly earth and other natural materials including sand, straw, and water, were built as early as the late Stone Age and were built more frequently during the Bronze Age and Iron Age as a means of protection. See also Oppidum. * Henge eart ...
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