Showery Tor
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Showery Tor
Showery Tor is a rocky outcrop on a ridge-top approximately north of the Rough Tor summit, near Camelford on Bodmin Moor in Cornwall. It is notable for its rock formations and prehistoric monuments. The Tor is a prominent landmark for a wide area. It consists of a natural outcrop of weathered granite enveloped by a giant man-made ring cairn of stones, each up to in diameter and high. Christopher Tilley has estimated the height of the cairn on which the outcrop stands to be . The site was thought to have been a religious focal point, possibly from the Neolithic or Bronze Age period. No excavations have been recorded at the site, and it is not known if any burials were made there. The granite outcrop is reminiscent of the Cheesewring The Cheesewring ( kw, Keuswask) is a granite tor in Cornwall, United Kingdom, situated on the eastern flank of Bodmin Moor on Stowe's Hill in the parish of Linkinhorne approximately one mile northwest of the village of Minions and f ...
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Cornwall
Cornwall (; kw, Kernow ) is a historic county and ceremonial county in South West England. It is recognised as one of the Celtic nations, and is the homeland of the Cornish people. Cornwall is bordered to the north and west by the Atlantic Ocean, to the south by the English Channel, and to the east by the county of Devon, with the River Tamar forming the border between them. Cornwall forms the westernmost part of the South West Peninsula of the island of Great Britain. The southwesternmost point is Land's End and the southernmost Lizard Point. Cornwall has a population of and an area of . The county has been administered since 2009 by the unitary authority, Cornwall Council. The ceremonial county of Cornwall also includes the Isles of Scilly, which are administered separately. The administrative centre of Cornwall is Truro, its only city. Cornwall was formerly a Brythonic kingdom and subsequently a royal duchy. It is the cultural and ethnic origin of the Cornish dias ...
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Granite
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 alway ...
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Buildings And Structures In Cornwall
A building, or edifice, is an enclosed structure with a roof and walls standing more or less permanently in one place, such as a house or factory (although there's also portable buildings). Buildings come in a variety of sizes, shapes, and functions, and have been adapted throughout history for a wide number of factors, from building materials available, to weather conditions, land prices, ground conditions, specific uses, prestige, and aesthetic reasons. To better understand the term ''building'' compare the list of nonbuilding structures. Buildings serve several societal needs – primarily as shelter from weather, security, living space, privacy, to store belongings, and to comfortably live and work. A building as a shelter represents a physical division of the human habitat (a place of comfort and safety) and the ''outside'' (a place that at times may be harsh and harmful). Ever since the first cave paintings, buildings have also become objects or canvasses of much artis ...
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Archaeological Sites In Cornwall
Archaeology or archeology is the scientific study of human activity through the recovery and analysis of material culture. The archaeological record consists of artifacts, architecture, biofacts or ecofacts, sites, and cultural landscapes. Archaeology can be considered both a social science and a branch of the humanities. It is usually considered an independent academic discipline, but may also be classified as part of anthropology (in North America – the four-field approach), history or geography. Archaeologists study human prehistory and history, from the development of the first stone tools at Lomekwi in East Africa 3.3 million years ago up until recent decades. Archaeology is distinct from palaeontology, which is the study of fossil remains. Archaeology is particularly important for learning about prehistoric societies, for which, by definition, there are no written records. Prehistory includes over 99% of the human past, from the Paleolithic until the adve ...
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History Of Cornwall
The history of Cornwall goes back to the Paleolithic, but in this period Cornwall only had sporadic visits by groups of humans. Continuous occupation started around 10,000 years ago after the end of the last ice age. When recorded history started in the first century BCE, the spoken language was Common Brittonic, and that would develop into Southwestern Brittonic and then the Cornish language. Cornwall was part of the territory of the tribe of the Dumnonii that included modern-day Devon and parts of Somerset. After a period of Roman rule, Cornwall reverted to rule by independent Romano-British leaders and continued to have a close relationship with Brittany and Wales as well as southern Ireland, which neighboured across the Celtic Sea. After the collapse of Dumnonia, the remaining territory of Cornwall came into conflict with neighbouring Wessex. By the middle of the ninth century, Cornwall had fallen under the control of Wessex, but it kept its own culture. In 1337, th ...
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Stone Age Sites In Cornwall
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 composition, and the way in which it is formed. Rocks form the Earth's outer solid layer, the crust, and most of its interior, except for the liquid 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 weathering, transport, and deposition of existing rocks. ...
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Megalithic Monuments In England
A megalith is a large stone that has been used to construct a prehistoric structure or monument, either alone or together with other stones. There are over 35,000 in Europe alone, located widely from Sweden to the Mediterranean sea. The word was first used in 1849 by the British antiquarian Algernon Herbert in reference to Stonehenge and derives from the Ancient Greek words "mega" for great and "lithos" for stone. Most extant megaliths were erected between the Neolithic period (although earlier Mesolithic examples are known) through the Chalcolithic period and into the Bronze Age. At that time, the beliefs that developed were dynamism and animism, because Indonesia experienced the megalithic age or the great stone age in 2100 to 4000 BC. So that humans ancient tribe worship certain objects that are considered to have supernatural powers. Some relics of the megalithic era are menhirs (stone monuments) and dolmens (stone tables). Types and definitions While "megalith" is ...
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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 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 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 a surface is eroded. Typically, physical erosion procee ...
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Cheesewring
The Cheesewring ( kw, Keuswask) is a granite tor in Cornwall, United Kingdom, situated on the eastern flank of Bodmin Moor on Stowe's Hill in the parish of Linkinhorne approximately one mile northwest of the village of Minions and four miles (6 km) north of Liskeard. It is a natural geological formation, a rock outcrop of granite slabs formed by weathering. The name derives from the resemblance of the piled slabs to a "cheesewring", a press-like device that was once used to make cheese. Wilkie Collins described the Cheesewring in 1861 in his book ''Rambles Beyond Railways'': Located adjacent to the Cheesewring Quarry (which supplied the granite cladding for the structure of Tower Bridge, London) and surrounded by other granite formations, this landmark was threatened with destruction in the late nineteenth century by the proximity of blasting operations, but was saved as a result of local activism. Legend A local legend says that the Cheesewring is the result of a ...
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Bronze Age
The Bronze Age is a historic period, lasting approximately from 3300 BC to 1200 BC, characterized by the use of bronze, the presence of writing in some areas, and other early features of urban civilization. The Bronze Age is the second principal period of the three-age system proposed in 1836 by Christian Jürgensen Thomsen for classifying and studying ancient societies and history. An ancient civilization is deemed to be part of the Bronze Age because it either produced bronze by smelting its own copper and alloying it with tin, arsenic, or other metals, or traded other items for bronze from production areas elsewhere. Bronze is harder and more durable than the other metals available at the time, allowing Bronze Age civilizations to gain a technological advantage. While terrestrial iron is naturally abundant, the higher temperature required for smelting, , in addition to the greater difficulty of working with the metal, placed it out of reach of common use until the end o ...
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Camelford
Camelford ( kw, Reskammel) is a town and civil parish in north Cornwall, England, United Kingdom, situated in the River Camel valley northwest of Bodmin Moor. The town is approximately ten miles (16 km) north of Bodmin and is governed by Camelford Town Council. Lanteglos-by-Camelford is the ecclesiastical parish in which the town is situated (''not to be confused with'' Lanteglos-by-Fowey). The ward population at the 2011 Census was 4,001. The town population at the same census was 865. Camelford is in the North Cornwall parliamentary constituency represented by Scott Mann MP since 2015. Until 1974, the town was the administrative headquarters of Camelford Rural District. From 2009 to 2021, the town was represented on Cornwall Council by the Camelford division. From the 2021 local elections, it will be represented by the Camelford and Boscastle division. The two main industrial enterprises in the area are the slate quarry at Delabole and the cheese factory at Davids ...
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Neolithic
The Neolithic period, or New Stone Age, is an Old World archaeological period and the final division of the Stone Age. It saw the Neolithic Revolution, a wide-ranging set of developments that appear to have arisen independently in several parts of the world. This "Neolithic package" included the introduction of farming, domestication of animals, and change from a hunter-gatherer lifestyle to one of settlement. It began about 12,000 years ago when farming appeared in the Epipalaeolithic Near East, and later in other parts of the world. The Neolithic lasted in the Near East until the transitional period of the Chalcolithic (Copper Age) from about 6,500 years ago (4500 BC), marked by the development of metallurgy, leading up to the Bronze Age and Iron Age. In other places the Neolithic followed the Mesolithic (Middle Stone Age) and then lasted until later. In Ancient Egypt, the Neolithic lasted until the Protodynastic period, 3150 BC.Karin Sowada and Peter Grave. Egypt in th ...
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