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Parc Le Breos
''Parc le Breos'' was a great medieval deer park in the south of the Gower Peninsula, about west of Swansea, Wales, and about north of the Bristol Channel. The park was an enclosed, oval area of in circumference, covering about and measuring  miles (east–west) by just over  miles (4.1 km by 2.9 km). ''Parc le Breos'' was established in the 1220s CE by John de Braose (of the powerful Cambro-Norman de Braose dynasty), Marcher Lord of Gower and husband to Margaret Ferch Llywelyn, ''Llywelyn Fawr's'' daughter. Other than for deer husbandry, the park received an income from agistment, pannage, and from sales of wild honey, ferns and dead wood. There is evidence of rabbit warrens in the park. Whether the warrens were free or domestic is unknown. The park's boundary was originally marked by a wooden fence, or pale, on the top of an earth bank inside a ditch. Some parts of the pale survive. Prehistoric finds and an Iron Age enclosure (above Parkmill ...
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Iron Age
The Iron Age is the final epoch of the three-age division of the prehistory and protohistory of humanity. It was preceded by the Stone Age (Paleolithic, Mesolithic, Neolithic) and the Bronze Age (Chalcolithic). The concept has been mostly applied to Iron Age Europe and the Ancient Near East, but also, by analogy, to other parts of the Old World. The duration of the Iron Age varies depending on the region under consideration. It is defined by archaeological convention. The "Iron Age" begins locally when the production of iron or steel has advanced to the point where iron tools and weapons replace their bronze equivalents in common use. In the Ancient Near East, this transition took place in the wake of the Bronze Age collapse, in the 12th century BC. The technology soon spread throughout the Mediterranean Basin region and to South Asia (Iron Age in India) between the 12th and 11th century BC. Its further spread to Central Asia, Eastern Europe, and Central Europe is somewhat dela ...
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Projectile Point
In North American archaeological terminology, a projectile point is an object that was hafted to a weapon that was capable of being thrown or projected, such as a javelin, dart, or arrow. They are thus different from weapons presumed to have been kept in the hand, such as knives, spears, axes, hammers, and maces. Stone tools, including projectile points, can survive for long periods, were often lost or discarded, and are relatively plentiful, especially at archaeological sites. They provide useful clues to the human past, including prehistoric trade. A distinctive form of point, identified though lithic analysis of the way it was made, is often a key diagnostic factor in identifying an archaeological industry or culture. Scientific techniques exist to track the specific kinds of rock or minerals that were used to make stone tools in various regions back to their original sources. As well as stone, projectile points were also made of worked wood, bone, antler, horn, or ivory ...
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Cambrian Archaeological Association
The Cambrian Archaeological Association ( cy, Cymdeithas Hynafiaethau Cymru) was founded in 1846 to examine, preserve and illustrate the ancient monuments and remains of the history, language, manners, customs, arts and industries of Wales and the Welsh Marches and to educate the public in such matters. The association's activities include sponsoring lectures, field visits, and study tours; as well as publishing its journal, ''Archaeologia Cambrensis'', and monographs. It also provides grants to support research and publications. Activities Meetings and lectures The association holds two meetings each year, a week in mid-summer and an autumn weekend, visiting sites and monuments in all parts of Wales and, on occasions, in England, Scotland, Ireland and abroad. Easter conferences with lectures on matters of current concern in history and archaeology are held on a bi-annual basis. It arranges a lecture in the Welsh language each year at the National Eisteddfod. Research grants and ...
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Culturenet Cymru
Culturenet Cymru Ltd. is funded by the Welsh Assembly Government and is based at The National Library of Wales in Aberystwyth.Welsh Assembly Government press release
Retrieved 13 October 2008 Its brief is to work in conjunction with both its members and community groups to develop a range of exciting and innovative projects. Its aim is to use online resources to increase awareness of, and improve access for all to, the culture and history of . Culturenet Cymru projects include: *

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Ossuary
An ossuary is a chest, box, building, well, or site made to serve as the final resting place of human skeletal remains. They are frequently used where burial space is scarce. A body is first buried in a temporary grave, then after some years the skeletal remains are removed and placed in an ossuary ("os" is "bone" in Latin). The greatly reduced space taken up by an ossuary means that it is possible to store the remains of many more people in a single tomb than in coffins. Persian ossuaries In Persia, the Zoroastrians used a deep well for this function from the earliest times (c. 3,000 years ago) and called it '' astudan'' (literally, "the place for the bones"). There are many rituals and regulations in the Zoroastrian faith concerning the ''astudans''. Jewish ossuaries During the Second Temple period, Jewish burial customs were varied, differing based on class and belief. For the wealthy, one option available included primary burials in burial caves, followed by secondary buri ...
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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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Mesolithic
The Mesolithic (Greek: μέσος, ''mesos'' 'middle' + λίθος, ''lithos'' 'stone') or Middle Stone Age is the Old World archaeological period between the Upper Paleolithic and the Neolithic. The term Epipaleolithic is often used synonymously, especially for outside northern Europe, and for the corresponding period in the Levant and Caucasus. The Mesolithic has different time spans in different parts of Eurasia. It refers to the final period of hunter-gatherer cultures in Europe and Western Asia, between the end of the Last Glacial Maximum and the Neolithic Revolution. In Europe it spans roughly 15,000 to 5,000  BP; in Southwest Asia (the Epipalaeolithic Near East) roughly 20,000 to 10,000  BP. The term is less used of areas farther east, and not at all beyond Eurasia and North Africa. The type of culture associated with the Mesolithic varies between areas, but it is associated with a decline in the group hunting of large animals in favour of a broader hunter-g ...
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Canyon
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosion, erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's River source, headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examp ...
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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ...
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Outcrop
An outcrop or rocky outcrop is a visible exposure of bedrock or ancient superficial deposits on the surface of the Earth. Features Outcrops do not cover the majority of the Earth's land surface because in most places the bedrock or superficial deposits are covered by soil and vegetation and cannot be seen or examined closely. However, in places where the overlying cover is removed through erosion or tectonic uplift, the rock may be exposed, or ''crop out''. Such exposure will happen most frequently in areas where erosion is rapid and exceeds the weathering rate such as on steep hillsides, mountain ridges and tops, river banks, and tectonically active areas. In Finland, glacial erosion during the last glacial maximum (ca. 11000 BC), followed by scouring by sea waves, followed by isostatic uplift has produced many smooth coastal and littoral outcrops. Bedrock and superficial deposits may also be exposed at the Earth's surface due to human excavations such as quarrying and build ...
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Parc Cwm Long Cairn
, alternate_name = , image = Parc le Breos, Gwyr o'r dwyrain.JPG , caption = , alt = Elevated view of the cairn in the middle distance, from its side, with deciduous trees in leaf to its rear. To its front passes a wide asphalt path, dissecting flat ground of short grass. The tumulus' trapezium shape is evident, its boulders retained by a short wall, missing at the very front, left, where the rubble has tumbled out. , location = near Parkmill, Gower , region = City and County of Swansea, Wales , coordinates = , type = chambered tomb , epochs = Neolithic , public_access = , condition = nearly intact , website = Parc Cwm long cairn ( cy, carn hir Parc Cwm), also known as Parc le Breos burial chamber (), is a partly restored Neolithic chambered tomb, identified in 1937 as a Severn-Cotswold type of chambered long barrow. The cromlech, a megalithic burial chamber, was built around 5850  years before present (BP), during the early Neolithic. It ...
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