A crannog is typically a partially or entirely artificial island, usually built in lakes and estuarine waters of Scotland, Wales, and Ireland. Unlike the prehistoric pile dwellings around the Alps, which were built on the shores and not inundated until later, crannogs were built in the water, thus forming artificial islands.
Perthshire, officially the County of Perth, is a historic county and registration county in central Scotland. Geographically it extends from Strathmore in the east, to the Pass of Drumochter in the north, Rannoch Moor and Ben Lui in the west, and Aberfoyle in the south; it borders the counties of Inverness-shire and Aberdeenshire to the north, Angus to the east, Fife, Kinross-shire, Clackmannanshire, Stirlingshire and Dunbartonshire to the south and Argyllshire to the west.
Loch Rannoch is a freshwater loch in Perth and Kinross, Scotland. It is over 15 kilometres (9.3 mi) long in a west–east direction with an average width of about 1.2 kilometres (0.75 mi), and is deepest at its eastern end, reaching a depth of 130 metres (440 ft). The River Tummel begins at its eastern end, where the small village of Kinloch Rannoch can be found, whilst the wild expanse of Rannoch Moor extends to the west of the loch. The area surrounding Loch Rannoch, along with Rannoch Moor itself, was formerly part of the native Caledonian Forest that stretched across much of Northern Scotland. Native forest is now largely absent from much of the area, due partly to logging, and partly to the climate becoming wetter, and Loch Rannoch is now largely surrounded by commercial forestry and open hillsides, although a small area remains at the Black Wood of Rannoch on the southern shore of the loch.
Archaeology and geology continue to reveal the secrets of prehistoric Scotland, uncovering a complex past before the Romans brought Scotland into the scope of recorded history. Successive human cultures tended to be spread across Europe or further afield, but focusing on this particular geographical area sheds light on the origin of the widespread remains and monuments in Scotland, and on the background to the history of Scotland.
Ian Armit identifies the islet of Eilean Dòmhnuill, Loch Olabhat, on North Uist, Scotland, as what may be the earliest crannog. Unstan ware pottery found there suggests a Neolithic period date of 3200–2800 BC. A surrounding timber screen and the turf-walled houses seem to have been repeatedly taken down and rebuilt, and in the final phase two oblong stone-footed structures bear a resemblance to Knap of Howar on Papa Westray, Orkney.
Ben Lawers is the highest mountain in the Breadalbane region of the Scottish Highlands. It lies north of Loch Tay and is the highest peak of the 'Ben Lawers group', a ridge that includes six other Munros: Beinn Ghlas, Meall Garbh, Meall Corranaich, An Stùc, Meall Greigh and Meall a' Choire Leith. It is also the highest peak in Perthshire, and the tenth highest Munro in Scotland. Ben Lawers was long thought to be over 4,000 feet in height, but accurate measurement in the 1870s showed it to be only 3,983 feet (1,214 m). It is formed of metamorphic rock, most notably calcareous mica-schists, and lower down, schistose grits.
Kenmore is a small village in Perthshire, in the Highlands of Scotland, located where Loch Tay drains into the River Tay.
Loch Torridon is a sea loch on the west coast of Scotland in the Northwest Highlands. The loch was created by glacial processes and is in total around 15 miles (25 km) long. It has two sections: Upper Loch Torridon to landward, east of Rubha na h-Airde Ghlaise, at which point it joins Loch Sheildaig; and the main western section of Loch Torridon proper. Loch a' Chracaich and Loch Beag are small inlets on the southern shores of the outer Loch, which joins the Inner Sound between the headlands of Rubha na Fearna to the south and Red Point to the north.
Killin is a village in Perthshire in the central Highlands of Scotland. Situated at the western head of Loch Tay, it is administered by the Stirling Council area. Killin is a historic conservation village and sits within the Loch Lomond and The Trossachs National Park. It is the central settlement of the historic region of Breadalbane.
Lochearnhead is a village in Perthshire on the A84 Stirling to Crianlarich road at the foot of Glen Ogle, 14 miles north of the Highland Boundary Fault. It is situated at the western end of Loch Earn where the A85 road from Crieff meets the A84.
Kinloch Rannoch is a village in Perth and Kinross, Scotland, at the eastern end of Loch Rannoch, 18 miles (29 km) west of Pitlochry, on the banks of the River Tummel. The village is a tourist and outdoor pursuits centre. It has a small population and is fairly remote.
The prehistory of Ireland has been pieced together from archaeological evidence, which has grown at an increasing rate over the last decades. It begins with the first evidence of permanent human residence in Ireland around 10,500 BC and finishes with the start of the historical record around 400 AD. Both the beginning and end dates of the period are later than for much of Europe and all of the Near East. The prehistoric period covers the Palaeolithic, Mesolithic, Neolithic, Bronze Age and Iron Age societies of Ireland. For much of Europe, the historical record begins when the Romans invaded; as Ireland was not invaded by the Romans its historical record starts later, with the coming of Christianity.
The Hebrides were settled early on in the settlement of the British Isles, perhaps as early as the Mesolithic era, around 8500–8250 BC, after the climatic conditions improved enough to sustain human settlement. There are examples of structures possibly dating from up to 3000 BC, the finest example being the standing stones at Callanish, but some archaeologists date the site as Bronze Age. Little is known of the people who settled in the Hebrides but they were likely of the same Celtic stock that had settled in the rest of Scotland. Settlements at Northton, Harris, have both Beaker & Neolithic dwelling houses, the oldest in the Western Isles, attesting to the settlement.
Finlaggan is a historic site on Eilean Mòr in Loch Finlaggan. The Loch, the island, and Finlaggan Castle lie on Islay, around two kilometres to the northwest of Ballygrant.
This timeline of prehistoric Scotland is a chronologically ordered list of important archaeological sites in Scotland and of major events affecting Scotland's human inhabitants and culture during the prehistoric period. The period of prehistory prior to occupation by the genus Homo is part of the geology of Scotland. Prehistory in Scotland ends with the arrival of the Romans in southern Scotland in the 1st century AD and the beginning of written records. The archaeological sites and events listed are the earliest examples or among the most notable of their type.
The Neolithic period in the British Isles lasted from c. 4100 to c. 2,500 BC. Constituting the final stage of the Stone Age in the region, it was preceded by the Mesolithic and followed by the Bronze Age.
Loch Freuchie, also known as Fraoch, the heatherly loch, is a large freshwater loch on a north-west to south-east orientation, within Glen Quaich in Perth and Kinross. The loch is located 2 miles (3.2 km) west of Amulree and 6.5 miles (10.5 km) southeast of Kenmore.
Loch Beanie also known as Loch Shechernich, is a small shallow freshwater loch that is located in Glen Shee in Perth and Kinross, Scotland.
