A broch is an Iron Age drystone hollow-walled structure found in Scotland. Brochs belong to the classification "complex Atlantic roundhouse" devised by Scottish archaeologists in the 1980s. Their origin is a matter of some controversy.
Shetland, also called the Shetland Islands and formerly Zetland, is a subarctic archipelago in the Northern Atlantic, between Great Britain, the Faroe Islands and Norway. It is the northernmost part of the United Kingdom.
The Mainland is the main island of Shetland, Scotland. The island contains Shetland's only burgh, Lerwick, and is the center of Shetland's ferry and air connections.
The Mainland, also known as Hrossey and Pomona, is the main island of Orkney, Scotland. Both of Orkney's burghs, Kirkwall and Stromness, lie on the island, which is also the heart of Orkney's ferry and air connections.
Unst is one of the North Isles of the Shetland Islands, Scotland. It is the northernmost of the inhabited British Isles and is the third-largest island in Shetland after Mainland and Yell. It has an area of 46 sq mi (120 km2).
Whalsay is the sixth largest of the Shetland Islands in the north of Scotland.
The Northern Isles are a pair of archipelagos off the north coast of mainland Scotland, comprising Orkney and Shetland. They are part of Scotland, as are the Hebrides. The climate is cool and temperate and much influenced by the surrounding seas. There are a total of 36 inhabited islands. The landscapes of the fertile agricultural islands of Orkney contrast with the more rugged Shetland islands to the north, where the economy is more dependent on fishing and on the oil wealth of the surrounding seas. Both island groups have a developing renewable energy industry. Both have a Pictish and Norse history. Both were part of the Kingdom of Norway until they were absorbed into the Kingdom of Scotland in the 15th century. They remained part of it until the 1707 formation of the Kingdom of Great Britain and the 1801 formation of the United Kingdom. And they both played a significant naval role during the world wars of the 20th century.
The North Isles are the northern islands of the Shetland Islands, Scotland. The main islands in the group are Yell, Unst and Fetlar. Sometimes the islands in Yell Sound are included in this group.
The Moine Thrust Belt or Moine Thrust Zone is a linear tectonic feature in the Scottish Highlands which runs from Loch Eriboll on the north coast 190 kilometres (120 mi) south-west to the Sleat peninsula on the Isle of Skye. The thrust belt consists of a series of thrust faults that branch off the Moine Thrust itself. Topographically, the belt marks a change from rugged, terraced mountains with steep sides sculptured from weathered igneous, sedimentary and metamorphic rocks in the west to an extensive landscape of rolling hills over a metamorphic rock base to the east. Mountains within the belt display complexly folded and faulted layers and the width of the main part of the zone varies up to 10 kilometres (6.2 mi), although it is significantly wider on Skye.
The Dalradian Supergroup is a stratigraphic unit in the lithostratigraphy of the Grampian Highlands of Scotland and in the north and west of Ireland. The diverse assemblage of rocks which constitute the supergroup extend across Scotland from Islay in the west to Fraserburgh in the east and are confined by the Great Glen Fault to the northwest and the Highland Boundary Fault to the southeast. Much of Shetland east of the Walls Boundary Fault is also formed from Dalradian rocks. Dalradian rocks extend across the north of Ireland from County Antrim in the north east to Clifden on the Atlantic coast, although obscured by later Palaeogene lavas and tuffs or Carboniferous rocks in large sections.
The geography of Scotland is varied, from rural lowlands to unspoilt uplands, and from large cities to sparsely inhabited islands. Located in Northern Europe, Scotland comprises the northern third of the island of Great Britain as well as 790 surrounding islands encompassing the major archipelagos of the Shetland Islands, Orkney Islands and the Inner and Outer Hebrides.
The geology of Scotland is unusually varied for a country of its size, with a large number of differing geological features. There are three main geographical sub-divisions: the Highlands and Islands is a diverse area which lies to the north and west of the Highland Boundary Fault; the Central Lowlands is a rift valley mainly comprising Palaeozoic formations; and the Southern Uplands, which lie south of the Southern Uplands Fault, are largely composed of Silurian deposits.
Benjamin Neeve Peach was a British geologist.
Northmavine or Northmaven is a peninsula in northwest Mainland Shetland in Scotland. The peninsula has historically formed the civil parish Northmavine. The modern Northmavine community council area has the same extent. The area of the parish is given as 204.1 km2.
Esha Ness, also spelled Eshaness, is a peninsula on the west coast of Northmavine, on the island of Mainland, Shetland, Scotland. Esha Ness Lighthouse on the west coast, just south of Calder's Geo. It was designed by David Alan Stevenson and commissioned in 1929. The hamlet of Tangwick contains the Tangwick Haa Museum, which opened in the former Laird's house in 1987.
Uyea is an uninhabited tidal island located to the northwest of Mainland, Shetland. Uyea lies off the Northmavine peninsula, from where it can be reached by foot at low tide. The island's highest elevation is 70 metres (230 ft) and its area is 45 hectares (0.17 sq mi).
The North West Highlands Geopark is a geopark in the Scottish Highlands. Awarded UNESCO geopark status in 2004, it was Scotland's first geopark, featuring some of the oldest rocks in Europe, around 3,000 million years old. The park contains many notable geological features, such as the Moine Thrust Belt and Smoo Cave and covers an area of around 2,000 square kilometres (770 sq mi).
The Lewisian complex or Lewisian gneiss is a suite of Precambrian metamorphic rocks that outcrop in the northwestern part of Scotland, forming part of the Hebridean Terrane and the North Atlantic Craton. These rocks are of Archaean and Paleoproterozoic age, ranging from 3.0–1.7 billion years (Ga). They form the basement on which the Torridonian and Moine Supergroup sediments were deposited. The Lewisian consists mainly of granitic gneisses with a minor amount of supracrustal rocks. Rocks of the Lewisian complex were caught up in the Caledonian orogeny, appearing in the hanging walls of many of the thrust faults formed during the late stages of this tectonic event.
The Zenith of Iron Age Shetland is a combination of three sites in Shetland that have applied to be on the United Kingdom "Tentative List" of possible nominations for the UNESCO World Heritage Programme list of sites of outstanding cultural or natural importance to the common heritage of humankind. The application was made by the Shetland Amenity Trust in 2010, and in 2011 the site became one of 11 successful UK applications to join the Tentative List, three of them from Scotland.
Delting is a civil parish and community council area on Mainland, Shetland, Scotland. It includes the Sullom Voe oil terminal and its main settlements are Brae, Mossbank and Voe.
