Entrance grave is a type of Neolithic and early Bronze Age chamber tomb found primarily in Great Britain. The burial monument typically consisted of a circular mound bordered by a stone curb, erected over a rectangular burial chamber and accessed by a narrow, stone lined entrance. Entrance graves have been discovered in the Isles of Scilly, west Cornwall, southeast Ireland, southwest Scotland, Brittany and the Channel Islands. They are often referred to as the Scillonian Group, named for the Scillonian Islands where the majority of entrance graves have been discovered.
Entrance graves in Britain are also known as Scillonian entrance graves, because the majority of these ancient burial monuments are found on the Isles of Scilly, [1] a group of islands 25 miles (40 m) west of Cornwall. [2] The islands were originally settled during the Neolithic era, circa 2500 BC. [3] Burials on the islands range in date from the later Neolithic period to the Middle Bronze Age (c. 2500–1000 BC). [4] Over eighty entrance graves have been recorded on the Isles of Scilly. Many date to the late Neolithic period and continued in use until the beginning of the eighth century BC. [5] Excavated entrance graves have contained human remains, cremation urns, and pottery fragments. The excavation of the Knackyboy Carn entrance grave on St. Martin's Island uncovered sixty or more cremated individuals. Entrance graves continued to be built on the Isles of Scilly for many years after individual burials had become the standard burial practice on the mainland of Britain. Besides being used for interments, it has been suggested that entrance graves could have been used for ritualistic and cultural purposes, or to mark land boundaries between different family groups. [4]
An entrance grave usually consisted of a circular mound of stacked rubble and earth, generally up to 25m in diameter. The edge of the mound would be marked with stone. The mound encompassed a rectangular, roofed burial chamber lined with stone, either large slabs or rubble masonry. [6] Many graves have a narrow entrance or passage lined with stone slabs. The chamber roof was typically covered by small stones are large granite slabs. Some grave entrance are blocked with a large stone. [2] Entrance graves may contain single or multiple interments and occur in small or large groups. Along with other types of megalithic chambered tombs, entrance graves are found in western Cornwall, the Isles of Scilly, southeast Ireland, southwest Scotland, the Channel Islands and Brittany. In Britain, the majority of entrance graves are located on the Isles of Scilly. [6]
Carn Euny is an archaeological site near Sancreed, on the Penwith peninsula in Cornwall, United Kingdom with considerable evidence of both Iron Age and post-Iron Age settlement. Excavations on this site have shown that there was activity at Carn Euny as early as the Neolithic period. There is evidence that shows that the first timber huts there were built about 200 BC, but by the 1st century BC, these had been replaced by stone huts. The remains of these stone huts are still visible today.
A gallery grave is a form of megalithic tomb built primarily during the Neolithic Age in Europe in which the main gallery of the tomb is entered without first passing through an antechamber or hallway. There are at least four major types of gallery grave, and they may be covered with an earthen mound or rock mound.
Bant's Carn is a Bronze Age entrance grave located on a steep slope on the island of St Mary's in the Isles of Scilly, England. The tomb is one of the best examples of a Scillonian entrance grave. Below Bant's Carn, lies the remains of the Iron Age village of Halangy Down.
Porth Hellick Down is a Neolithic and Bronze Age archeological site located on the island of St Mary's, in the Isles of Scilly in Great Britain. The ancient burial monument encompasses a large cairn cemetery that includes at least six entrance graves, other unchambered cairns, and a prehistoric field system. The site is notable for having the largest assembly of surviving entrance graves.
Gugh could be described as the sixth inhabited island of the Isles of Scilly, but is usually included with St Agnes with which it is joined by a sandy tombolo known as "The Bar" when exposed at low tide. The island is only about 1 km (0.62 mi) long and about 0.5 km (0.31 mi) wide, with the highest point, Kittern Hill at 34 m (112 ft). The geology consists of Hercynian granite with shallow podzolic soils on the higher ground and deeper sandy soils on the lower ground. The former Gugh farm is just north of the neck across the middle of the island between the two hills. The two houses were designed and built in the 1920s by Charles Hamlet Cooper. The name is often mispronounced as "Goo", "Guff" or even "Gogh".
The Tregiffian Burial Chamber is a Neolithic or early Bronze Age chambered tomb. It is near Lamorna in west Cornwall, United Kingdom. It is a rare form of a passage grave, known as an Entrance grave. It has an entrance passage, lined with stone slabs, which leads into a central chamber. This type of tomb is also found in the neighbouring Isles of Scilly.
Trethevy Quoit is a well-preserved megalithic structure between St Cleer and Darite in Cornwall, United Kingdom. It is known locally as "the giant's house". Standing 9 feet (2.7 m) high, it consists of five standing stones capped by a large slab and was added to the Heritage at Risk Register in 2017.
Chapel Carn Brea is an elevated Hercynian granite outcrop, owned by the National Trust at the southern edge of the civil parish of St Just, Cornwall, England, United Kingdom. The hill is 5 kilometres (3.1 mi) south of St Just and 3.5 kilometres (2.2 mi) east of Sennen Cove, and just to the north of the A30 London to Land's End road, which runs through the village of Crows-an-Wra. It should not be confused with another Carn Brea, the hill overlooking the Camborne–Redruth area.
The dolmens of Jersey are neolithic sites, including dolmens, in Jersey. They range over a wide period, from around 4800 BC to 2250 BC, these dates covering the periods roughly designated as Neolithic, or “new stone age”, to Chalcolithic, or “copper age”.
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Obadiah's Barrow or Obadiah's Grave is a Neolithic entrance grave located on the island of Gugh in the Isles of Scilly. The grave sits on a steep slope on the southwestern side of Kittern Hill, the highest point on Gugh. The grave was excavated in 1901 by British archaeologist, George Bonsor.
The unchambered long barrowearthen long barrow, non-megalithic long barrow or non-megalithic mound, is a type of long barrow found across the British Isles, in a belt of land in Brittany, and in northern Europe as far east as the River Vistula. The term "unchambered" means that there is no stone chamber within the stone enclosure. In Great Britain they are often known as non-megalithic long barrows or unchambered long cairns.
The architecture of Scotland in the prehistoric era includes all human building within the modern borders of Scotland, before the arrival of the Romans in Britain in the first century BCE. Stone Age settlers began to build in wood in what is now Scotland from at least 8,000 years ago. The first permanent houses of stone were constructed around 6,000 years ago, as at Knap of Howar, Orkney and settlements like Skara Brae. There are also large numbers of chambered tombs and cairns from this era, particularly in the west and north. In the south and east there are earthen barrows, often linked to timber monuments of which only remnants remain. Related structures include bank barrows, cursus monuments, mortuary enclosures and timber halls. From the Bronze Age there are fewer new buildings, but there is evidence of crannogs, roundhouses built on artificial islands and of Clava cairns and the first hillforts. From the Iron Age there is evidence of substantial stone Atlantic roundhouses, which include broch towers, smaller duns. There is also evidence of about 1,000 hillforts in Scotland, most located below the Clyde-Forth line.
Brane Barrow, or Chapel Euny Barrow, is a Neolithic entrance grave located near the hamlet of Brane, Cornwall, England, UK. It is considered to be one of the smallest and best preserved burial monuments in Britain.
Innisidgen is the site of two Bronze Age entrance graves on the island of St Mary's in the Isles of Scilly. The two burial monuments, lie on a steep slope of Innisidgen Hill overlooking Crow Sound with a view towards the Eastern Isles.
British megalith architecture is the study of those ancient cultures that built megalithic sites on the British Isles, including the research and documentation of these sites. The classification sometimes used of these cultures based on geological criteria is problematic.
Pawton Quoit is a prehistoric portal dolmen, which dates to the Early and Middle Neolithic period in England. The burial monument is located near Haycrock Farm, south of St Breock, in Cornwall, England.
Bosiliack Barrow is a barrow on the Penwith Moors between Madron and Morvah near the hamlet of Bosiliack in Cornwall, UK.
Halangy Down is a prehistoric settlement located on the island of St Mary's, in the Isles of Scilly. The ancient site covers the lower slope of Halangy Down hill, overlooking the coastal inlet between the island of St. Mary's and Tresco Island. On the site are the remains of an Iron Age village, two entrance graves, prehistoric field systems, standing stones, post-medieval breastworks, and a Victorian kelp pit. The settlement was in continuous use for 500 years, from the late Iron Age until the end of the Roman occupation in Britain.
The Cornish Bronze Age is an era of the history of Cornwall that spanned the period from c. 2400 BCE to c. 800 BCE. It was preceded by the Cornish Neolithic, and followed by the Cornish Iron Age. It is characterized by the introduction and widespread use of copper and copper-alloy (bronze) weapons and tools.