TheIslands of the Firth of Clyde are the fifth largest of the majorScottish island groups after theInner andOuter Hebrides,Orkney andShetland. They are situated in theFirth of Clyde betweenArgyll and Bute in the west andInverclyde,North Ayrshire andSouth Ayrshire in the east. There are about forty islands andskerries. Only four are inhabited, and only nine are larger than 40 hectares (99 acres).^{[Note 1]} The largest and most populous areArran andBute. They are served by dedicated ferry routes, as areGreat Cumbrae andHoly Island.^[4][5] Unlike the isles in the four larger Scottish archipelagos, none of the isles in this group are connected to one another or to the mainland by bridges.

Thegeology andgeomorphology of the area is complex, and the islands and the surrounding sealochs each have distinctive features. The influence of theAtlantic Ocean and theNorth Atlantic Drift create a mild, damp oceanic climate. There is a diversity of wildlife, including three species of rare endemic trees.

The larger islands have been continuously inhabited sinceNeolithic times. The cultures of their inhabitants were influenced by the emergence of the kingdom ofDál Riata, beginning in 500 AD. The islands were then politically absorbed into the emergingkingdom of Alba, led byKenneth MacAlpin. During theearly Middle Ages, the islands experiencedViking incursions. In the 13th century, they became part of theKingdom of Scotland.

TheHighland Boundary Fault runs past Bute and through the northern part of Arran. Therefore, from a geological perspective, some of the islands are in the Highlands and some in theCentral Lowlands.^[6] As a result of Arran's geological similarity to Scotland, it is sometimes referred to as "Scotland in miniature" and the island is a popular destination forgeologists. They come to Arran to study itsintrusive igneous landforms, such assills anddykes, as well as itssedimentary and metasedimentary rocks, which range widely in age.^[7] Visiting in 1787, the geologistJames Hutton found his first example of anunconformity there. The spot where he discovered it is one of the most famous places in the history of the study of geology.^[8][9] The group of weakly metamorphosed rocks that form theHighland Border Complex lie discontinuously along the Highland Boundary Fault. One of the most prominent exposures is along Loch Fad on Bute.^[10]Ailsa Craig, which lies some 25 kilometres (16 mi) south of Arran, has been quarried for a rare type ofmicro-granite containingriebeckite, known as "Ailsite". It is used byKays of Scotland to makecurling stones. (As of 2004, 60 to 70% of all curling stones in use globally were made from granite quarried on the island.)^[11]

Like the rest of Scotland, the Firth of Clyde was covered by ice sheets during thePleistoceneice ages, and the landscape has been much affected byglaciation.^[12] Back then, Arran's highest peaks may have beennunataks.^[13] Sea-level changes and theisostatic rise of land after the last retreat of the ice created clifflines behindraised beaches, which are a prominent feature of the entire coastline. The action of these forces has made charting thepost glacial coastlines a complex task.^[14][15]

The various soil types on the islands reflect their diverse geology. Bute has the most productive land, and it has a pattern of deposits that is typical of the southwest of Scotland. In the eroded valleys, there is a mixture ofboulder clay and other glacial deposits. Elsewhere, especially to the south and west, there are raised beach- and marine deposits, which in some places, such as Stravanan, result in amachair landscape inland from the sandy bays.^[16][17]

The Firth of Clyde, in which these islands lie, is north of the Irish Sea and has numerous branching inlets. Some of those inlets, includingLoch Goil,Loch Long,Gare Loch,Loch Fyne, and the estuary of theRiver Clyde, have their own substantial features. In places, the effect of glaciation on the seabed is pronounced. For example, the Firth is 320 metres (1,050 ft) deep between Arran and Bute, even though they are only 8 kilometres (5.0 mi) apart.^[18] The islands all stand exposed to wind and tide. Variouslighthouses, such as those on Ailsa Craig,Pladda, andDavaar, act as an aid to navigation.^[19]

The Firth of Clyde lies between 55 and 56 degrees north latitude. This is the same latitude asLabrador in Canada and north of theAleutian Islands. However, the influence of theNorth Atlantic Drift—the northern extension of theGulf Stream—moderates the winter weather. As a result, the area enjoys a mild, damp oceanic climate. Temperatures are generally cool, averaging about 6 °C (43 °F) in January and 14 °C (57 °F) in July at sea level.^[20] Snow seldom lies at sea level, and frosts are generally less frequent than they are on the mainland. In common with most islands off the west coast of Scotland, the average annual rainfall is generally high: between 1,300 mm (51 in) on Bute, in the Cumbraes, and in the south of Arran, and 1,900 mm (75 in) in the north of Arran. The Arran mountains are even wetter: Their summits receive over 2,550 mm (100 in) of rain annually. May, June and July are the sunniest months: on average, there is a total of 200 hours of bright sunshine during that 3-month period each year. Southern Bute benefits from a particularly large number of sunny days.^[20]

Mesolithic humans arrived in the area of the Firth of Clyde during the 4th millennium BC, probably fromIreland. This initial arrival was followed by another wave ofNeolithic peoples using the same route. In fact, there is some evidence that the Firth of Clyde was a significant route through which mainland Scotland was colonised during the Neolithic period.^[21] The inhabitants of Argyll, the Clyde estuary, and elsewhere in western Scotland at that time developed a distinctive style of megalithic structure that is known today as theClyde cairns. About 100 of these structures have been found. They were used for interment of the dead. They are rectangular or trapezoidal, with a small enclosing chamber into which the person's body was placed. They are faced with large slabs of stone set on end (sometimes subdivided into smaller compartments). They also feature a forecourt area, which may have been used for displays or rituals associated with interment.^[22] They are mostly found in Arran, Bute, and Kintyre. It is thought likely that the Clyde cairns were the earliest forms of Neolithic monument constructed by incoming settlers. However, only a few of the cairns have beenradiocarbon dated. A cairn at Monamore on Arran has been dated to 3160 BC, although other evidence suggests that it was almost certainly built earlier than that, possibly around 4000 BC.^{[22][23][24][25]} The area also features numerousstanding stones dating from prehistoric times, including sixstone circles on Machrie Moor in Arran, and other examples on Great Cumbrae and Bute.^[26][27]

Later,Bronze Age settlers also constructed megaliths at various sites. Many of them date from the 2nd millennium BC. However, instead ofchambered cairns, these peoples constructed burialcists, which can be found, for example, on Inchmarnock. Evidence of settlement during this period, especially the early part of it, is scant.^[27][28] However, one notable artifact has been found on Bute that dates from around 2000 BC. Known today as the “Queen of the Inch necklace,” it is an article of jewellery made oflignite (commonly called “jet”).

During the earlyIron Age, theBrythonic culture held sway. There is no evidence that theRoman occupation of southern Scotland extended into these islands.^[23][29]

Beginning in the 2nd century AD, Irish influence was at work in the region, and by the 6th century,Gaels had established the kingdom ofDál Riata there. Unlike earlier inhabitants, such as theP-Celtic speaking Brythons, these Gaels spoke a form ofGaelic (a modern version of which is still spoken today in theHebrides). During this period, through the efforts ofSaint Ninian and others, Christianity slowly supplantedDruidism. The kingdom of Dál Riata flourished from the rule ofFergus Mór in the late 5th century until theViking incursions beginning in the late 8th century.^[30] Islands close to the shores of modernAyrshire presumably remained part of theKingdom of Strathclyde during this period, whilst the main islands became part of the emergingKingdom of Alba founded by Kenneth MacAlpin (Cináed mac Ailpín).

Beginning in the 9th century and into the 13th century, the Islands of the Clyde constituted a border zone between the NorseSuðreyjar and Scotland, and many of them were under Norse hegemony.

Beginning in the last half of the 12th century, and then into the early 1200s, the islands may well have served as the power base ofSomhairle mac Giolla Brighde andhis descendants. During this time, the islands seem to have come under the sway of theSteward of Scotland’s authority and to have been taken over by the expandingStewart lordship.^[31]

This western extension of Scottish authority appears to have been one of the factors motivating the Norwegian invasion of the region in 1230, during which the invaders seizedRothesay Castle.^[32]

In 1263, Norwegian troops commanded byHaakon Haakonarson repeated the feat, but the ensuingBattle of Largs between Scots and Norwegian forces, which took place on the shores of the Firth of Clyde, was inconclusive as a military contest.^[33][34]

This battle marked an ultimately fatal weakening of Norwegian power in Scotland. Haakon retreated toOrkney, where he died in December 1263, consoled on his death bed by recitations of the old sagas. Following his death, under the 1266Treaty of Perth, all rights that the Norwegian Crown "had of old therein" in relation to the islands were yielded to the Kingdom of Scotland.^[35][36][37]

Politically, from the conclusion of theTreaty of Perth in 1266 to the present day, all of the islands of the Clyde have been part of Scotland.

Ecclesiastically, beginning in the early medieval period all of these isles were part of theDiocese of Sodor and Man, based atPeel, on theIsle of Man. After 1387, the seat of theBishopric of the Isles was relocated to the north, first toSnizort onSkye and then toIona.^[38] This arrangement continued until theScottish Reformation in the 16th century, when Scotland broke with the Catholic Church.

The mid-1700s marked the beginning of a century of significant change. New forms of transport, industry, and agriculture brought an end to ways of life that had endured for centuries. TheBattle of Culloden in 1746 foreshadowed the end of theclan system. These changes improved living standards for some, but came at a cost for others.^[39]

In the late 18th and early 19th centuries,Alexander, the 10th Duke of Hamilton (1767–1852), and others implemented a controversial agricultural-reform programme called theHighland Clearances that had a devastating effect on many of Arran's inhabitants. Whole villages were emptied, and the Gaelic culture of the island was dealt a terminal blow. (A memorial to the tenant farmers evicted from the island by this programme was later erected on the shore atLamlash, funded by a Canadian descendant of some of those evicted.)^{[40][41][42][43]}

From the 1850s to the late 20th century, cargo ships known as “Clyde Puffers” (made famous by an early-20th-century story collection called theVital Spark), were the workhorses of the islands, carrying a great deal of produce and a great variety of products to and from the islands. In May 1889, theCaledonian Steam Packet Company (CSP) was founded and began operating steamer services to and from Gourock for theCaledonian Railway. The company soon expanded by taking over rival steamer operators.^[44]David MacBrayne operated the Glasgow-to-Ardrishaig steamer service, as part of the so-called "Royal Route" to Oban.^[45] During the 20th century, many of the islands were developed as tourist resorts along the lines of mainland resorts such asLargs andTroon, but catering for Glaswegians who preferred to holiday "Doon the Watter".^[46][47]In 1973, CSP and MacBraynes combined their Clyde and West Highland operations under the new name ofCaledonian MacBrayne.^[48] Agovernment-owned corporation, they serve Great Cumbrae, Arran, and Bute, and also run mainland-to-mainland ferries across the firth.^[4][49] Private companies operate services from Arran to Holy Isle,^[5] and from McInroy's Point (Gourock) to Hunter's Quay on the Cowal peninsula.^[50]

Politically, from 1890 to 1975, most of the islands comprised the traditionalCounty of Bute, and its inhabitants were represented by the county council. Since the 1975 reorganization, however, the islands have been split more or less equally between two modern council authorities:Argyll and Bute, andNorth Ayrshire. OnlyAilsa Craig andLady Isle inSouth Ayrshire are not part of either of these twocouncil areas.

Below is a table listing the nine islands of the Firth of Clyde that have an area greater than 40 hectares (approximately 100 acres), showing their population and listing the smaller uninhabited islets adjacent to them (including tidal islets separated only when the tide is higher, andskerries exposed only when the tide is lower).

As of 2001, six of the islands were inhabited, but that included one with only two residents (Davaar), and one with only one resident (Sanda).^[51] At the2011 census, there was no one usually resident on either of these islands.^[52]

The islets that lie remote from the larger islands are described separately below.^[62]

There are two islets in Gare Loch: Green Island and Perch Rock. Gare Loch is small, but it hosts theFaslane Naval Base, where the UK'sTrident nuclear submarines are located. At its southern end, the loch opens into theFirth of Clyde via theRhu narrows.^[63]

There are also several islets in theKilbrannan Sound, which lies between Arran and theKintyre peninsula. They are: An Struthlag, Cour Island, Eilean Carrach (Carradale), Eilean Carrach (Skipness), Eilean Grianain, Eilean Sunadale, Gull Isle, Island Ross and Thorn Isle.

(The Norse sagas tell a story about the Kintyre peninsula. In the late 11th century, aking of Norway (Magnus Barefoot) devised a plan to increase his territorial possessions. He persuaded a king of Scotland (Malcolm III orEdgar) to agree that he could take possession of an area of land on the west coast of Scotland if a ship could sail around it. Magnus then arranged for one of hislongships to be dragged across the 1.5 kilometres (0.93 mi)-long isthmus at the northern tip of the Kintyre peninsula, which connects Kintyre to the mainland. (The isthmus lies betweenEast Loch Tarbert andWest Loch Tarbert). He took command of the ship's tiller himself. Then, declaring that Kintyre had "better land than the best of theHebrides", he claimed that dragging his ship across the isthmus had been equivalent to “sailing around” the peninsula, and thus that the peninsula counted as “land around which a ship could sail.” As a result of this maneuver, he was able to claim possession of the peninsula, which remained under Norse rule for more than a dozen years.^{[64][65][66][67][Note 3]})

There are also several islets and skerries in Loch Fyne, which extends 65 kilometres (40 mi) inland from theSound of Bute, and is the longest of Scotland's sea lochs.^[69] They are: Duncuan Island, Eilean Ardgaddan, Eilean a' Bhuic, Eilean Aoghainn, Eilean a' Chomhraig, Eilean an Dúnain, Eilean Buidhe (Ardmarnock), Eilean Buidhe (Portavadie), Eilean Fraoch, Eilean Math-ghamhna, Eilean Mór, Glas Eilean, Heather Island, Inverneil Island, Kilbride Island, and Liath Eilean.

There are several islets surroundingHorse Isle inNorth Ayrshire: Broad Rock, East Islet, Halftide Rock, High Rock and North Islet.

Lady Isle lies off the South Ayrshire coast nearTroon. At one time it housed "ane old chapell with an excellent spring of water".^[70] However, in June 1821, someone set fire to the "turf and pasture". Once the pasture had burned away, gales blew much of the island's soil into the sea. This permanently destroyed the island's ability to support grazing.^[71]

There are no islands in Loch Goil or Loch Long, which arefjord-like arms in the northern part of the firth.^[57]

Here is a list of places along that shores of the Firth of Clyde that are not islands, but have names that misleadingly suggest they are islands (eilean being Gaelic for "island"): Eilean na Beithe, Portavadie; Eilean Beag,Cove; Eilean Dubh, Dalchenna, Loch Fyne; Eilean nan Gabhar, Melldalloch,Kyles of Bute; Barmore Island, just north ofTarbert, Kintyre;^[72] Eilean Aoidh, south of Portavadie; Eilean Leathan, Kilbrannan Sound just south ofTorrisdale Bay; Island Muller, Kilbrannan Sound north ofCampbeltown.^[73]

Around the Firth of Clyde, there are populations ofred deer,red squirrel,badger,otter,adder, andcommon lizard. In the Firth itself, there areharbour porpoises,basking sharks and various species ofdolphin.^[74] Davaar is home to a population of wildgoats.^[75]

Over 200 bird species have been recorded as sighted in the area, including theblack guillemot, theeider, theperegrine falcon, and thegolden eagle.^[74] In 1981, there were 28ptarmigans sighted on Arran, but in 2009 it was reported that extensive surveys had been unable to find any recorded ptarmigans sightings.^[76] Similarly, thered-billed chough no longer breeds on the island.^[77]

Arran has three species of the rareendemic trees known asArran Whitebeams:^[78] theScottish or Arran whitebeam; thecut-leaved whitebeam; and theCatacol whitebeam. All of them are found only in Gleann Diomhan, and they are amongst the most endangered tree species in the world. (Gleann Diomhan was formerly part of a designatednational nature reserve—the designation was removed in 2011)- and it continues to be part of an area designated as aSite of Special Scientific Interest.)^[79] Only 283 Arran whitebeam and 236 cut-leaved whitebeam were recorded as mature trees in 1980,^[80] and it is thought that grazing pressures and insect damage are preventing regeneration of the woodland.^[79] The Catacol whitebeam was discovered in 2007, but only two specimens have been found, so steps have been taken to protect them.^[81][82]

TheRoman historianTacitus refers to theClota, meaning the Clyde. The derivation is not certain but is probably from theBrythonicClouta, which becameClut inOld Welsh. The name literally means "wash", probably referring to a river goddess who is seen as "the washer" or "the strongly flowing one".^[83] The derivation of the word “Bute” is also uncertain. The Norse name for it isBót an Old Irish word for "fire", which might be a reference to signal fires.^[84] The etymology of “Arran” is no clearer. Haswell-Smith (2004) suggests that it derive from a Brythonic word meaning "high place",^[85] although Watson (1926) suggests it may be pre-Celtic.^{[86][Note 4]}

• Islands of the Clyde
• Lists of islands of Scotland
• Archipelagoes of Scotland
• Archipelagoes of the Atlantic Ocean

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