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.
Assynt is a sparsely populated area in the south-west of Sutherland, lying north of Ullapool on the west coast of Scotland. Assynt is known for its landscape and its remarkable mountains, which have led to the area, along with neighbouring Coigach, being designated as the Assynt-Coigach National Scenic Area, one of 40 such areas in Scotland.
Ardvreck Castle is a castle, now ruinous, standing on a rocky promontory in Loch Assynt, Sutherland, Scotland, UK. The structure dates from about 1490 and is associated with the then landowners, the Macleods of Assynt.
St Clement's Church is a late fifteenth-century or early sixteenth-century church in Rodel, Harris, Scotland, built for the Chiefs of the MacLeods of Harris. It is dedicated to Pope Clement I. It is sometimes known as Eaglais Roghadail or Rodal Church.
Benjamin Neeve Peach was a British geologist.
John Horne PRSE FRS FRSE FEGS LLD was a Scottish geologist. He served as president of the Royal Society of Edinburgh from 1915 to 1919.
Clan MacLeod of The Lewes, commonly known as Clan MacLeod of Lewis, is a Highland Scottish clan, which at its height held extensive lands in the Western Isles and west coast of Scotland. From the 14th century up until the beginning of the 17th century there were two branches of Macleods: the MacLeods of Dunvegan and Harris ; and the Macleods of the Isle of Lewis. In Gaelic the Macleods of Lewis were known as Sìol Thorcaill, and the MacLeods of Dunvegan and Harris were known as Sìol Thormoid.
Longforgan is a village and parish in the Carse of Gowrie, in Perth and Kinross, Scotland. It lies 5 miles west of Dundee on the main A90 road.
Conival is a Scottish mountain situated in Assynt in the Sutherland area of the Highland Council Area, thirty kilometres north-northeast of Ullapool.
Loch Assynt is a freshwater loch in Sutherland, Scotland, 8 kilometres (5.0 mi) east-north east of Lochinver.
Auchenblae is a village in the Kincardine and Mearns area of Aberdeenshire, formerly in Kincardineshire, Scotland. The village was known for its weavers, a whisky distillery and the annual Paldie's Fair horse market.
The Parish Church of St Cuthbert is a parish church of the Church of Scotland in central Edinburgh. Probably founded in the 7th century, the church once covered an extensive parish around the burgh of Edinburgh. The church's current building was designed by Hippolyte Blanc and completed in 1894.
Knockan Crag lies within the North West Highlands Geopark in the Assynt region of Scotland 21 kilometres (13 mi) north of Ullapool. During the nineteenth century Knockan Crag became the subject of much debate when geologists noted that the Moine schists at the top of the crag appeared to be older than the Cambrian and Ordovician rocks such as Durness limestone lower down. Disagreements over the processes that could have caused this to occur were referred to at the time as the "Highlands Controversy". The argument was primarily between Roderick Murchison and Archibald Geikie on the one hand and James Nicol and Charles Lapworth on the other. Murchison and Geikie believed the sequence was wrong and that the Moine schists must be the younger rocks. The controversy was finally resolved by the work of Ben Peach and John Horne whose 1907 paper on the subject remains a classic text. Peach and Horne demonstrated that the situation resulted from the action of a thrust fault - this being the first to be discovered anywhere in the world. The older rocks had been moved some 70 kilometres to the west over the top of the younger rocks due to tectonic action.
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).
Cavers is a parish in the Scottish Borders area of Scotland, in the former county of Roxburghshire, south and east of Hawick. The largest village in the parish is Denholm.
The Highlands controversy was a scientific controversy which started between British geologists in the middle of the nineteenth century concerning the nature of the rock strata in the Northwest Highlands of Scotland. The debate became contentious, even acrimonious, because of some of the personalities involved and because it pitted professional geologists of the Geological Survey against academic and amateur geologists. An initial resolution was achieved by about 1886 but the great complexity and scientific importance of the discovery of the Moine Thrust Belt and the geological processes involved in its creation led to field work continuing for a further twenty years culminating in the 1907 publication by the Geological Survey of a book of fundamental geological significance: The Geological Structure of the North-West Highlands of Scotland.
Kirkandrews, sometimes written as Kirkanders in older documents, is a coastal hamlet about 9 kilometres (6 mi) west-southwest of Kirkcudbright in Dumfries and Galloway, Scotland. It sits in farmland at the head of Kirkandrews Bay, an inlet of Wigtown Bay.
Anwoth Old Church is a ruined church building which was built in 1626 to serve the parish of Anwoth in Dumfries and Galloway, Scotland. It is roofless, but much of the walls remain, including the west gable which is surmounted by a bellcote. A number of substantial monuments exist within the church and its surrounding churchyard.
Kinnoull Parish Church is a Church of Scotland church in the Kinnoull area of Perth, Perth and Kinross, Scotland. A Kinnoull Church appears in documents when it was granted to Cambuskenneth Abbey in 1361. It was rebuilt in 1779 but demolished in 1826 after the completion of a church on the Perth side of the River Tay, which flows a short distance behind the church.
