Islay whisky is Scotch whisky made on Islay or Ìle in Gaelic, one of the southernmost of the Inner Hebridean Islands located off the west coast of Scotland. Islay is one of five whisky distilling localities and regions in Scotland whose identity is protected by law.
Argyll, sometimes called Argyllshire, is a historic county and registration county of western Scotland.
Port Ellen is a small town on the island of Islay, in Argyll, Scotland. The town is named after the wife of its founder, Frederick Campbell of Islay. Its previous name, Leòdamas, is derived from Old Norse meaning "Leòd's Harbour".
Bowmore is a distillery that produces Scotch whisky on the Isle of Islay, an island of the Inner Hebrides. The distillery, which lies on the South Eastern shore of Loch Indaal, is one of the oldest in Scotland and is said to have been established in 1779. The distillery is owned by Morrison Bowmore Distillers Ltd, a holding company owned by Beam Suntory, a subsidiary of Japanese multinational drinks conglomerate Suntory. Morrison Bowmore also own the Auchentoshan and Glen Garioch distilleries and produce the McClelland's Single Malt range of bottlings.
Bowmore is a small town on the Scottish island of Islay. It serves as administrative capital of the island, and gives its name to the noted Bowmore distillery producing Bowmore single malt scotch whisky.
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 Highland Boundary Fault is a major fault zone that traverses Scotland from Arran and Helensburgh on the west coast to Stonehaven in the east. It separates two different geological terranes which give rise to two distinct physiographic terrains: the Highlands and the Lowlands, and in most places it is recognisable as a change in topography. Where rivers cross the fault, they often pass through gorges, and the associated waterfalls can be a barrier to salmon migration.
Port Askaig is a port village on the east coast of the island of Islay, in Scotland.
In geology, the term Torridonian is the informal name for the Torridonian Group, a series of Mesoproterozoic to Neoproterozoic arenaceous and argillaceous sedimentary rocks, which occur extensively in the Northwest Highlands of Scotland. The strata of the Torridonian Group are particularly well exposed in the district of upper Loch Torridon, a circumstance which suggested the name Torridon Sandstone, first applied to these rocks by James Nicol. Stratigraphically, they lie unconformably on gneisses of the Lewisian complex and their outcrop extent is restricted to the Hebridean Terrane.
The Rev. Dr. Robert Blair DD VD was a Scottish minister and a Gaelic scholar.
Loch Indaal is a sea loch on Islay, the southernmost island of the Hebrides, off the west coast of Scotland. Together with Loch Gruinart to the north, it was formed by the Loch Gruinart Fault, which branches off the Great Glen Fault.
Islay is the southernmost island of the Inner Hebrides of Scotland. Known as "The Queen of the Hebrides", it lies in Argyll just south west of Jura and around 40 kilometres (25 mi) north of the Northern Irish coast. The island's capital is Bowmore where the distinctive round Kilarrow Parish Church and a distillery are located. Port Ellen is the main port.
The geology of the Orkney islands in northern Scotland is dominated by the Devonian age Old Red Sandstone (ORS). In the southwestern part of Mainland, this sequence can be seen to rest unconformably on a Moinian type metamorphic basement.
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.
David MacBrayne is a limited company owned by the Scottish Government. Formed in 1851 as a private shipping company, it became the main carrier for freight and passengers in the Hebrides, with a co-ordinated network of shipping, road haulage and bus operations. In 1973, it was merged with Caledonian Steam Packet Company as state-owned Caledonian MacBrayne. Since 2006 it has been the holding company for ferry operators CalMac Ferries Ltd and Argyll Ferries.
The Colonsay Group is an estimated 5,000 m thick sequence of mildly metamorphosed Neoproterozoic sedimentary rocks that outcrop on the islands of Colonsay, Islay and Oronsay and the surrounding seabed. They have been correlated with the Grampian Group, the oldest part of the Dalradian Supergroup.
The Grampian Group is an estimated 9,000 m thick sequence of metamorphosed Neoproterozoic sedimentary rocks that outcrop across the Central Highlands of Scotland, east of the Great Glen. It forms a part of the Dalradian Supergroup. The sequence thickness at any one place is limited to 5km.
This article describes the geology of the Cairngorms National Park, an area in the Highlands of Scotland designated as a national park in 2003 and extended in 2010. The Cairngorms National Park extends across a much wider area than the Cairngorms massif itself and hence displays rather more varied geology.
The geology of the Isle of Mull in Scotland is dominated by the development during the early Palaeogene period of a ‘volcanic central complex’ associated with the opening of the Atlantic Ocean. The bedrock of the larger part of the island is formed by basalt lava flows ascribed to the Mull Lava Group erupted onto a succession of Mesozoic sedimentary rocks during the Palaeocene epoch. Precambrian and Palaeozoic rocks occur at the island's margins. A number of distinct deposits and features such as raised beaches were formed during the Quaternary period.
