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Heathery Burn Cave
Heathery Burn Cave is a cave near Stanhope, County Durham, England, in which a large collection of Late Bronze Age weapons and tools was discovered and excavated between 1859 and 1872. Location The cave was in a ravine formed by Stanhope Burn, a small tributary of the River Wear.Greenwell, W. 1894. "Antiquities of the Bronze Age found in the Heathery Burn Cave, County Durham", ''Archaeologia'' (2nd Series, 4), 87–114. The cave itself was about a mile north of the confluence of the burn and the river, on the left bank. The floor of the cave was above the level of the burn, and was a tourist destination before the quarrying of the limestone for smelting purposes. The cave has subsequently been destroyed.Britton, D. 1971. "The Heathery Burn Cave Revisited: Towards the Reconstruction of a Well-Known Archaeological Discovery", ''The British Museum Quarterly'' 35 (1/4), 20–38. Geology The geology of the area forms part of the Yoredale Group of limestone with subordinate sandsto ...
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County Durham
County Durham ( ), officially simply Durham,UK General Acts 1997 c. 23Lieutenancies Act 1997 Schedule 1(3). From legislation.gov.uk, retrieved 6 April 2022. is a ceremonial county in North East England.North East Assembly �About North East England. Retrieved 30 November 2007. The ceremonial county spawned from the historic County Palatine of Durham in 1853. In 1996, the county gained part of the abolished ceremonial county of Cleveland.Lieutenancies Act 1997
. Retrieved 27 October 2014.
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Yorkshire Museum
The Yorkshire Museum is a museum in York, England. It was opened in 1830, and has five permanent collections, covering biology, geology, archaeology, numismatics and astronomy. History The museum was founded by the Yorkshire Philosophical Society (YPS) to accommodate their geological and archaeological collections, and was originally housed in Ousegate, York, until the site became too small. In 1828, the society received by royal grant, of land formerly belonging to St Mary's Abbey for the purposes of building a new museum. The main building of the museum is called the Yorkshire Museum; it was designed by William Wilkins in a Greek Revival style and is a Grade I listed building. It was officially opened in February 1830, which makes it one of the longest established museums in England. A condition of the royal grant was that the land surrounding the museum building should be a botanic gardens and one was created in the 1830s. The botanic gardens are now known as the Museum G ...
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Caves Of County Durham
A cave or cavern is a natural void in the ground, specifically a space large enough for a human to enter. Caves often form by the weathering of rock and often extend deep underground. The word ''cave'' can refer to smaller openings such as sea caves, rock shelters, and grottos, that extend a relatively short distance into the rock and they are called ''exogene'' caves. Caves which extend further underground than the opening is wide are called ''endogene'' caves. Speleology is the science of exploration and study of all aspects of caves and the cave environment. Visiting or exploring caves for recreation may be called ''caving'', ''potholing'', or ''spelunking''. Formation types The formation and development of caves is known as ''speleogenesis''; it can occur over the course of millions of years. Caves can range widely in size, and are formed by various geological processes. These may involve a combination of chemical processes, erosion by water, tectonic forces, microorganisms ...
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Geology Of England
The geology of England is mainly sedimentary. The youngest rocks are in the south east around London, progressing in age in a north westerly direction.Southampton University
retrieved 21/1/07
The Tees–Exe line marks the division between younger, softer and low-lying rocks in the south east and the generally older and harder rocks of the north and west which give rise to higher relief in those regions. The geology of England is recognisable in the landscape of its counties, the building materials of its towns and its regional extr ...
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Flint
Flint, occasionally flintstone, is a sedimentary cryptocrystalline form of the mineral quartz, categorized as the variety of chert that occurs in chalk or marly limestone. Flint was widely used historically to make stone tools and start fires. It occurs chiefly as nodules and masses in sedimentary rocks, such as chalks and limestones.''The Flints from Portsdown Hill''
Inside the nodule, flint is usually dark grey, black, green, white or brown in colour, and often has a glassy or waxy appearance. A thin layer on the outside of the nodules is usually different in colour, typically white and rough in texture. The nodules can often be found along streams and
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Littorina Obtusata
''Littorina obtusata'', common name the flat periwinkle, is a species of sea snail, a marine gastropod mollusk in the family Littorinidae, the winkles or periwinkles. Distribution This marine species occurs wherever brown seaweeds grow. It is widely distributed : the Baltic Sea, in European waters from Norway down to Southern Spain, in the Mediterranean Sea, in the Northeast Atlantic Ocean along the Gulf of Maine. Description The maximum recorded shell length is 13.5 mm.Welch J. J. (2010). "The "Island Rule" and Deep-Sea Gastropods: Re-Examining the Evidence". '' PLoS ONE'' 5(1): e8776. . center, Habitat This species can be found in the littoral and sublittoral zone The neritic zone (or sublittoral zone) is the relatively shallow part of the ocean above the drop-off of the continental shelf, approximately in depth. From the point of view of marine biology it forms a relatively stable and well-illuminated ... on rocky shores and piers, usually on brown alga ...
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Dog Whelk
The dog whelk, dogwhelk, or Atlantic dogwinkle (''Nucella lapillus'') is a species of predatory sea snail, a carnivorous marine gastropod in the family Muricidae, the rock snails. ''Nucella lapillus'' was originally described by Carl Linnaeus in his landmark 1758 10th edition of ''Systema Naturae'' as ''Buccinum lapillus'' (the basionym). "Dog whelk" can also refer to the Nassariidae. Distribution This species is found around the coasts of Europe and in the northern west Atlantic coast of North America. It also can be found in estuarine waters along the Atlantic coasts. This species prefers rocky shores, where it eats mussels and acorn barnacles.Colin Little, J. A. Kitching, 1996''The Biology of Rocky Shores'' pp. 140-145. Shell description The dog whelk shell is small and rounded with a pointed spire and a short, straight siphonal canal (a groove on the underside of the shell) and a deep anal canal. The overall shell shape varies quite widely according to the ...
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Metapodial
Metapodials are long bone The long bones are those that are longer than they are wide. They are one of five types of bones: long, short, flat, irregular and sesamoid. Long bones, especially the femur and tibia, are subjected to most of the load during daily activities and ...s of the hand ( metacarpals) and feet ( metatarsals) which connect the digits to the lower leg bones. In humans, five are present in each hand and foot. In quadrupeds, these form the lower limb, rather than being part of the extremity, thus what looks to be the elbow of a sheep is actually the wrist. Bones of the upper limb Bones of the lower limb Bones of the hand {{musculoskeletal-stub ...
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Tibia
The tibia (; ), also known as the shinbone or shankbone, is the larger, stronger, and anterior (frontal) of the two bones in the leg below the knee in vertebrates (the other being the fibula, behind and to the outside of the tibia); it connects the knee with the ankle. The tibia is found on the medial side of the leg next to the fibula and closer to the median plane. The tibia is connected to the fibula by the interosseous membrane of leg, forming a type of fibrous joint called a syndesmosis with very little movement. The tibia is named for the flute '' tibia''. It is the second largest bone in the human body, after the femur. The leg bones are the strongest long bones as they support the rest of the body. Structure In human anatomy, the tibia is the second largest bone next to the femur. As in other vertebrates the tibia is one of two bones in the lower leg, the other being the fibula, and is a component of the knee and ankle joints. The ossification or formation of the bo ...
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Red Deer
The red deer (''Cervus elaphus'') is one of the largest deer species. A male red deer is called a stag or hart, and a female is called a hind. The red deer inhabits most of Europe, the Caucasus Mountains region, Anatolia, Iran, and parts of western Asia. It also inhabits the Atlas Mountains of Northern Africa; its early ancestors are thought to have crossed over to Morocco, then to Algeria, Libya and Tunisia via the Strait of Gibraltar, becoming the only species of true deer ( Cervidae) to inhabit Africa. Red deer have been introduced to other areas, including Australia, New Zealand, the United States, Canada, Peru, Uruguay, Chile and Argentina. In many parts of the world, the meat (venison) from red deer is used as a food source. Red deer are ruminants, characterized by a four-chambered stomach. Genetic evidence indicates that the red deer, as traditionally defined, is a species group, rather than a single species, though exactly how many species the group includes remains ...
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Eastgate, County Durham
Eastgate is a village in County Durham, England. It is situated in Weardale, a few miles west of Stanhope. In the 2001 census Eastgate had a population of 163. Eastgate originally marked the eastern border of the private hunting park of the Prince Bishops of Durham. This was second in extent only to the royal hunting park of the New Forest in Hampshire. To the west of Eastgate are a number of medieval sites. A suspected hunting lodge near Round Hill (Cambokeels) and a settlement site at Westerhopeburn. The latter is described as a hunting lodge or shielding and may be connected to the “Westirhirstshele” mentioned in Robert Strangeway's lease of the park in 1419 (described in the Calendar of Rolls of Bishop Booth). It was in use during the period when Strangeways and later his son held the grazing rights in the park. It may have been abandoned around 1458 when the lease was split up. The hunting lodge and supposed chapel at Cambokeels may also have been part of the Stra ...
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Wolsingham
Wolsingham is a market town in Weardale, County Durham, England. It is situated by the River Wear, between Crook and Stanhope. History Wolsingham sits at the confluence of the River Wear and Waskerley Beck. It is a small settlement and one of the first market towns in County Durham, deriving its name from Waelsingas, or Sons of Wael, an ancient Saxon family that once lived there. The earliest known record of the town is to be found in Reginald of Durham's ''Life of Godric'' where it is stated that the saint lived there for almost two years about 1120 AD with Elric the hermit. Wolsingham was then a thriving community, holding land by servile tenure. There were shepherds, plough-makers, beekeepers, forest keepers, wood turners, carters, etc. They toiled for two purposes – producing corn and other foodstuffs for themselves and supplying the larder of the Bishop's Castle. The bishop and his friends indulged in hawking, but hunting for red deer in the parks of Wolsingham and ...
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