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Heathstone
Carrstone (or carstone, also known as Silsoe, heathstone, ironstone or gingerbread) is a sedimentary sandstone conglomerate formed during the Cretaceous period. It varies in colour from light to dark rusty ginger. Used as a building stone it can be found in Bedfordshire, Cambridgeshire and extensively in the historic buildings of northwest Norfolk. Carrstone can vary in quality depending on factors such as the degree of iron oxide present, and sufficient pressure to form the matrix. Carrstone can also phase into puddingstone, ferricrete and silver carr. Because of its variations it does not lend itself to carving or finer work. Carrstonework can be seen in forms such as: random carrstone, coursed carrstone, ashlared carrstone, all with, or without, galleting. Other patterns of use are: rough carrstone sipps (slips or brickettes) and cut carrstone sipps, both used in masonry fields between brickwork quoins. Cut carrstone sipps are used extensively at Sandringham House on t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carrstone 006
Carrstone (or carstone, also known as Silsoe, heathstone, ironstone or gingerbread) is a sedimentary sandstone conglomerate formed during the Cretaceous period. It varies in colour from light to dark rusty ginger. Used as a building stone it can be found in Bedfordshire, Cambridgeshire and extensively in the historic buildings of northwest Norfolk. Carrstone can vary in quality depending on factors such as the degree of iron oxide present, and sufficient pressure to form the matrix. Carrstone can also phase into puddingstone, ferricrete and silver carr. Because of its variations it does not lend itself to carving or finer work. Carrstonework can be seen in forms such as: random carrstone, coursed carrstone, ashlared carrstone, all with, or without, galleting. Other patterns of use are: rough carrstone sipps (slips or brickettes) and cut carrstone sipps, both used in masonry fields between brickwork quoins. Cut carrstone sipps are used extensively at Sandringham House on the main ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carrstone At Hunstanton
Carrstone (or carstone, also known as Silsoe, heathstone, ironstone or gingerbread) is a sedimentary sandstone conglomerate formed during the Cretaceous period. It varies in colour from light to dark rusty ginger. Used as a building stone it can be found in Bedfordshire, Cambridgeshire and extensively in the historic buildings of northwest Norfolk. Carrstone can vary in quality depending on factors such as the degree of iron oxide present, and sufficient pressure to form the matrix. Carrstone can also phase into puddingstone, ferricrete and silver carr. Because of its variations it does not lend itself to carving or finer work. Carrstonework can be seen in forms such as: random carrstone, coursed carrstone, ashlared carrstone, all with, or without, galleting. Other patterns of use are: rough carrstone sipps (slips or brickettes) and cut carrstone sipps, both used in masonry fields between brickwork quoins. Cut carrstone sipps are used extensively at Sandringham House on the main ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Bentley
Great Bentley is a village, civil parish and electoral ward in the Tendring district of north Essex, England, located seven miles east of Colchester. The parish includes the hamlets of Aingers Green and South Heath. It is home to the second largest village green in the country, at a size of , behind Duncan Down and has won 'Essex Village of the Year' and 'Daily Telegraph/Calor Gas Village of the Year' awards. Great Bentley railway station provides the village with frequent rail services along the Sunshine Coast Line to London Liverpool Street, Clacton-on-Sea, Colchester and Walton-on-the-Naze. Great Bentley is scattered round an extensive level or common, of , on the eastern side of the vale of a rivulet, east-south-east of Colchester. The parish contains 2500 inhabitants, and of fertile land, including hills and valleys, and extending southward to the Flag Creek, a tidal creek which connects with the Colne, near Brightlingsea. The population of the civil parish reduced to 2,2 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Silver Carrstone 1
Silver is a chemical element with the symbol Ag (from the Latin ', derived from the Proto-Indo-European ''h₂erǵ'': "shiny" or "white") and atomic number 47. A soft, white, lustrous transition metal, it exhibits the highest electrical conductivity, thermal conductivity, and reflectivity of any metal. The metal is found in the Earth's crust in the pure, free elemental form ("native silver"), as an alloy with gold and other metals, and in minerals such as argentite and chlorargyrite. Most silver is produced as a byproduct of copper, gold, lead, and zinc refining. Silver has long been valued as a precious metal. Silver metal is used in many bullion coins, sometimes alongside gold: while it is more abundant than gold, it is much less abundant as a native metal. Its purity is typically measured on a per-mille basis; a 94%-pure alloy is described as "0.940 fine". As one of the seven metals of antiquity, silver has had an enduring role in most human cultures. Other than in cur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Burgh Castle
Burgh Castle is a village and civil parish in the English county of Norfolk. It is situated on the east bank of the River Waveney, some west of Great Yarmouth and within the Norfolk Broads National Park. The parish was part of Suffolk until 1974. History Burgh Castle's name is of Roman origin and derives from Gariannonum which invokes the Latin name for the River Yare. Burgh Castle was likely the site of a Neolithic settlement due to an abundance of flint and bronze axe-heads being discovered in the area. Burgh Castle is the location of a Roman Fortification which dates to the third century; the fort was part of system of coastal defence, the Saxon Shore, against Anglo-Saxon incursions on the East Anglian coast. The site is maintained by the Norfolk Archeological Trust and is open free of charge to the public. It has been suggested by the Elizabethan historian William Camden, that Burgh Castle is the site of Cnobheresburg, the first Irish monastery in southern England foun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flitcham, Norfolk
Flitcham is a village and civil parish in the English county of Norfolk. The village is located north-east of King's Lynn and north-west of Norwich, along the River Babingley. Together with the villages of West Newton, Shernborne and Anmer, Flitcham forms part of the Royal Sandringham Estate. History Flitcham's name is of Anglo-Saxon origin and derives from the Old English for a village or settlement where 'flitches' of Bacon were produced. In 1948, the site of a Roman villa was excavated close to Denbeck Wood, within the parish. After excavation, the villa was found to have glazed windows, a tessellated floor and a small courtyard flanker by other buildings from the same period. Further artefacts, including coins, pottery and metalwork dating from the Third and Forth Centuries, have been discovered close to the site and across the parish. Another possible Roman building has been identified close to the course of the River Babingley. In addition, the Denbeck Wood excavations ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hillington, Norfolk
Hillington is a village and civil parish in the English county of Norfolk. It covers an area of and had a population of 287 in 123 households as of the United Kingdom Census 2001, 2001 census, increasing to 400 at the 2011 Census. For the purposes of local government, it falls within the Non-metropolitan district, district of King's Lynn and West Norfolk. The village straddles the A148 road, A148 King's Lynn to Cromer road. It formerly had a Hillington railway station, railway station, but this closed in 1959. History The settlement was recorded in the Domesday Book as ''Helingetuna'', which is believed to mean ‘the farmstead of the family or followers of a man named Hythla or Hydl'. Archaeological test pits were dug between 2015–2017 and a report was published in 2019. Notable people Hillington is the traditional home of the ffolkes baronets. Francis ffolkes, 5th Baronet was Rector of Hillington from 1912 until his death. His nephew, the intelligence officer and conserva ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Castle Rising
Castle Rising is a village and civil parish in the English county of Norfolk. The village is situated some north-east of the town of King's Lynn and west of the city of Norwich. The River Babingley skirts the north of the village separating Castle Rising from the site of the lost village of Babingley.Ordnance Survey (2002). ''OS Explorer Map 250 - Norfolk Coast West''. . History Castle Rising's name is of Norman and Anglo-Saxon origin, deriving from a mix of the Old English and Norman French for a castle close to the settlement of Risa's people. In the Domesday Book, Rising is listed as a settlement of fourteen households in the hundred of Grimshoe. The village was owned by William de Warenne. Castle Rising Castle was built in the 1140s on the orders of William d'Aubigny and was most famously the residence of Queen Isabella after her role in the murder of King Edward II. The castle was subsequently passed to Edward of Woodstock and is now in the possession of Grevil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Concretion
A concretion is a hard, compact mass of matter formed by the precipitation of mineral cement within the spaces between particles, and is found in sedimentary rock or soil. Concretions are often ovoid or spherical in shape, although irregular shapes also occur. The word 'concretion' is derived from the Latin "(act of) compacting, condensing, congealing, uniting", itself from ''con'' meaning 'together' and ''crescere'' meaning "to grow". Concretions form within layers of sedimentary strata that have already been deposited. They usually form early in the burial history of the sediment, before the rest of the sediment is hardened into rock. This concretionary cement often makes the concretion harder and more resistant to weathering than the host stratum. There is an important distinction to draw between concretions and nodules. Concretions are formed from mineral precipitation around some kind of nucleus while a nodule is a replacement body. Descriptions dating from the 18th ce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glauconite
Glauconite is an iron potassium phyllosilicate ( mica group) mineral of characteristic green color which is very friable and has very low weathering resistance. It crystallizes with a monoclinic geometry. Its name is derived from the Greek () meaning 'bluish green', referring to the common blue-green color of the mineral; its sheen ( mica glimmer) and blue-green color. Its color ranges from olive green, black green to bluish green, and yellowish on exposed surfaces due to oxidation. In the Mohs scale it has hardness of 2. The relative specific gravity range is 2.4 - 2.95. It is normally found in dark green rounded brittle pellets, and with the dimension of a sand grain size. It can be confused with chlorite (also of green color) or with a clay mineral. Glauconite has the chemical formula . Glauconite particles are one of the main components of greensand, glauconitic siltstone and glauconitic sandstone. Glauconite has been called a marl in an old and broad sense of that word. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Feldspar
Feldspars are a group of rock-forming aluminium tectosilicate minerals, also containing other cations such as sodium, calcium, potassium, or barium. The most common members of the feldspar group are the ''plagioclase'' (sodium-calcium) feldspars and the ''alkali'' (potassium-sodium) feldspars. Feldspars make up about 60% of the Earth's crust, and 41% of the Earth's continental crust by weight. Feldspars crystalize from magma as both intrusive and extrusive igneous rocks and are also present in many types of metamorphic rock. Rock formed almost entirely of calcic plagioclase feldspar is known as anorthosite. Feldspars are also found in many types of sedimentary rocks. Compositions The feldspar group of minerals consists of tectosilicates, silicate minerals in which silicon ions are linked by shared oxygen ions to form a three-dimensional network. Compositions of major elements in common feldspars can be expressed in terms of three endmembers: * potassium feldspar (K-spar) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saunders_Quarry-1.jpg "Click for more on -> Sandstone")
