Corndon Hill
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Corndon Hill
Corndon Hill ( cy, Cornatyn) is a hill in Powys, Mid Wales, whose isolated summit rises to 1,683 ft above sea level. It is surrounded on three sides by the English county of Shropshire and forms a prominent landmark in the Wales-England border. Corndon's prominent western edge appears to form a separate hill and is known locally as ''Lan Fawr'' (Welsh: 'Big Hill'). It is frequented by walkers and ramblers from car parks nearby at Mitchell's Fold for example. There are spectacular panoramic views from the summit, and it is itself an important landmark for the surrounding countryside and towns like Montgomery. It is close to villages such as Church Stoke and Hyssington. The hill is geologically part of the Shropshire Hills range of hills lying mainly to the north, east and south of the summit. The immediate area to the west is the Vale of Montgomery and the River Severn. The Cambrian Mountains are visible beyond to the far west. The Stiperstones and Shelve lie to the ...
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Mitchells Fold
Mitchell's Fold (sometimes called Medgel's Fold or Madges Pinfold) is a Bronze Age stone circle in southwest Shropshire, located near the small village of White Grit on dry heathland at the southwest end of Stapeley Hill in the civil parish of Chirbury with Brompton, at a height of 1083 ft (330m) o.d. The stone circle, a standing stone, and a cairn comprise a Scheduled Ancient Monument; the circle is in the guardianship of English Heritage. Description As with most sites of this type, its true history is unknown. The name of the circle may derive from 'micel' or 'mycel', Old English for 'big', referring to the size of this large circle. Its doleritic stones came from nearby Stapeley Hill. Many of them are now missing and others are fallen. One example, reported in pagan magazine ''White Dragon'', is that “This circle was the site of vandalism by a local farmer in the summer of 1995 when several stones were uprooted by a mechanical digger. The stones were promptly rig ...
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Geologically
Geology () is a branch of natural science concerned with Earth and other astronomical objects, the features or rocks of which it is composed, and the processes by which they change over time. Modern geology significantly overlaps all other Earth sciences, including hydrology, and so is treated as one major aspect of integrated Earth system science and planetary science. Geology describes the structure of the Earth on and beneath its surface, and the processes that have shaped that structure. It also provides tools to determine the relative and absolute ages of rocks found in a given location, and also to describe the histories of those rocks. By combining these tools, geologists are able to chronicle the geological history of the Earth as a whole, and also to demonstrate the age of the Earth. Geology provides the primary evidence for plate tectonics, the evolutionary history of life, and the Earth's past climates. Geologists broadly study the properties and processes of Earth ...
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Cremation Urn
An urn is a vase, often with a cover, with a typically narrowed neck above a rounded body and a footed pedestal. Describing a vessel as an "urn", as opposed to a vase or other terms, generally reflects its use rather than any particular shape or origin. The term is especially often used for funerary urns, vessels used in burials, either to hold the cremated ashes or as grave goods, but is used in many other contexts. Large sculpted vases are often called urns, whether placed outdoors, in gardens or as architectural ornaments on buildings, or kept inside. In catering, large vessels for serving tea or coffee are often called "tea-urns", even when they are metal cylinders of purely functional design. Urns are also a common reference in thought experiments in probability wherein marbles or balls of different colors are used to represent different results and the urn represents the "container" of the whole set of possible states. Funerary Funerary urns (also called cinerary urns a ...
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Bronze
Bronze is an alloy consisting primarily of copper, commonly with about 12–12.5% tin and often with the addition of other metals (including aluminium, manganese, nickel, or zinc) and sometimes non-metals, such as phosphorus, or metalloids such as arsenic or silicon. These additions produce a range of alloys that may be harder than copper alone, or have other useful properties, such as ultimate tensile strength, strength, ductility, or machinability. The three-age system, archaeological period in which bronze was the hardest metal in widespread use is known as the Bronze Age. The beginning of the Bronze Age in western Eurasia and India is conventionally dated to the mid-4th millennium BCE (~3500 BCE), and to the early 2nd millennium BCE in China; elsewhere it gradually spread across regions. The Bronze Age was followed by the Iron Age starting from about 1300 BCE and reaching most of Eurasia by about 500 BCE, although bronze continued to be much more widely used than it is in mod ...
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Iron
Iron () is a chemical element with symbol Fe (from la, ferrum) and atomic number 26. It is a metal that belongs to the first transition series and group 8 of the periodic table. It is, by mass, the most common element on Earth, right in front of oxygen (32.1% and 30.1%, respectively), forming much of Earth's outer and inner core. It is the fourth most common element in the Earth's crust. In its metallic state, iron is rare in the Earth's crust, limited mainly to deposition by meteorites. Iron ores, by contrast, are among the most abundant in the Earth's crust, although extracting usable metal from them requires kilns or furnaces capable of reaching or higher, about higher than that required to smelt copper. Humans started to master that process in Eurasia during the 2nd millennium BCE and the use of iron tools and weapons began to displace copper alloys, in some regions, only around 1200 BCE. That event is considered the transition from the Bronze Age to the Iron A ...
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Cairn
A cairn is a man-made pile (or stack) of stones raised for a purpose, usually as a marker or as a burial mound. The word ''cairn'' comes from the gd, càrn (plural ). Cairns have been and are used for a broad variety of purposes. In prehistoric times, they were raised as markers, as memorials and as burial monuments (some of which contained chambers). In modern times, cairns are often raised as landmarks, especially to mark the summits of mountains. Cairns are also used as trail markers. They vary in size from small stone markers to entire artificial hills, and in complexity from loose conical rock piles to elaborate megalithic structures. Cairns may be painted or otherwise decorated, whether for increased visibility or for religious reasons. A variant is the inuksuk (plural inuksuit), used by the Inuit and other peoples of the Arctic region of North America. History Europe The building of cairns for various purposes goes back into prehistory in Eurasia, ranging in s ...
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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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Cairn At Summit Of Corndon Hill - Geograph
A cairn is a man-made pile (or stack) of stones raised for a purpose, usually as a marker or as a burial mound. The word ''cairn'' comes from the gd, càrn (plural ). Cairns have been and are used for a broad variety of purposes. In prehistoric times, they were raised as markers, as memorials and as burial monuments (some of which contained chambers). In modern times, cairns are often raised as landmarks, especially to mark the summits of mountains. Cairns are also used as trail markers. They vary in size from small stone markers to entire artificial hills, and in complexity from loose conical rock piles to elaborate megalithic structures. Cairns may be painted or otherwise decorated, whether for increased visibility or for religious reasons. A variant is the inuksuk (plural inuksuit), used by the Inuit and other peoples of the Arctic region of North America. History Europe The building of cairns for various purposes goes back into prehistory in Eurasia, ranging in s ...
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Long Mynd
, photo = , photo_alt = , photo_caption = View down Townbrook Valley toward Burway Hill , country_type = , country = England , subdivision1_type = County , subdivision1 = Shropshire , borders_on = , biome = HeathlandMoorland , topo_map = , topo_maker = , highest = Pole Bank , highest_location = , elevation_m = 516 , elevation_system = , coordinates = , length_km = 11.26 , width_km = 4.8 , area_km2 = 54 , length_orientation= N-S , width_orientation = E-W , length_ref = , width_ref = , area_ref = , parent = , range_coordinates = , range_coordinates_ref= , formed_by = Glaciation , geology = Sandstone , age = Quaternary , orogeny = , map = Shropshire , map_alt = , map_caption = The Long Mynd , map_ ...
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Caer Caradoc
Caer Caradoc ( cy, Caer Caradog, the fort of Caradog) is a hill in the English county of Shropshire. It overlooks the town of Church Stretton and the village of All Stretton and offers panoramic views to the north towards the Wrekin, east to Wenlock Edge, and west over the nearby Long Mynd. It is not to be confused with another hillfort of the same name 1 km west of Chapel Lawn near Bucknell. Caer Caradoc rises sharply out of a narrow valley known as the Stretton Gap. It is the highest point on a high, narrow, northeast–southwest "whaleback ridge", sometimes called a hogsback ridge. The Wrekin is a very similarly shaped hill and on the same alignment, some to the north-east. Caer Caradoc can be fairly easily climbed from Church Stretton but the ascent/descent is steep; a more gentle climb is from the village of Cardington, which lies two miles (3 km) east. Much of the hill is composed from volcanic rocks, like the Wrekin and other hills, formed of narrow ri ...
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