Isle of Skye & Trotternish

The strange tilted pinnacles and terraced hillsides of the Quiraing and the Old Man of Storr are frequently photographed as if they were simply ancient, static rock formations. They are, in fact, part of the largest actively moving landslip complex in Britain — a slow-motion geological process that is not finished, with parts of the Trotternish escarpment still classified as geologically active today rather than a fixed "ancient" feature.

This article tiers claims as documented (the landslip's geological mechanism and scale, the surveyed heights of the Storr and Quiraing features, the 1955 first ascent of the Old Man of Storr, Flora MacDonald's recorded residence at Flodigarry), traditional (long-repeated local and family history around specific crofting townships and named individuals, broadly credible but not always independently source-verified in full detail), and legend-myth (claims with no solid evidential basis, including some place-name folklore and any suggestion that the ridge's rock formations are long-settled "ancient wonders" rather than an ongoing geological process). The Trotternish landscape rewards this careful tiering more than most, since its most famous features are literally still changing.

Geological formation

The Trotternish ridge is, geologically, a textbook case of catastrophic slope failure on a massive scale, and remains one of the most studied landslip complexes in Britain. Its structure is a layer cake with an inherent instability built in from the start: Middle and Upper Jurassic marine sedimentary rocks — clays, shales, and sandstones — were laid down roughly 145 to 174 million years ago, forming a relatively weak and water-retentive base. Tens of millions of years later, during the intense Palaeogene volcanic activity that also produced the Cuillin's gabbro further south on Skye, around two dozen basalt lava flows erupted in succession, building up a dense cap roughly 300 metres thick directly on top of those weak sediments. The physics that follow are straightforward but dramatic: the heavy basalt cap presses down on the comparatively soft, often waterlogged Jurassic clay beneath it, and along a series of roughly north-south trending faults, enormous blocks of the lava cap have sheared away from the main escarpment and slid seaward along a rotational glide plane. The result is the largest mass-movement landslide complex in Britain, with the Quiraing section of this process extending across more than two kilometres of width and comprising at least five distinguishable phases of movement from the scarp face to the coast. Crucially, this is not a finished, ancient event frozen in the landscape: geological surveys confirm that while major features like the Storr and the main Quiraing terraces are currently considered stable, other sections of the Trotternish escarpment remain actively moving today, making this one of the few landscapes in this collection genuinely still being shaped in observable, human-timescale increments.

Human history and historical associations

Trotternish's human history runs through the broader story of Skye's clan conflicts, Jacobite-era drama, and the upheavals of the Highland Clearances. The peninsula lay within territory long contested between Clan MacDonald and Clan MacLeod, and Duntulm Castle at its northern tip — originally an Iron Age broch site, later a Viking stronghold, and eventually a MacDonald castle — reflects that layered strategic history; King James V is recorded visiting the castle in 1540 during a royal tour intended partly to assert crown authority over the Hebrides. The peninsula's best-known individual historical figure is Flora MacDonald, who famously assisted Prince Charles Edward Stuart's escape after the 1746 Battle of Culloden; she settled at Flodigarry on Trotternish in 1751 and raised several of her children there before later emigrating. Much of the romantic popular narrative around her life — her supposed unwavering Jacobite conviction, certain dramatic details of the escape itself — has been embellished in retelling over the subsequent centuries, and this article treats the core documented facts of her residence and escape role as established while flagging the more decorative narrative flourishes as traditional rather than verified in every particular. Like much of the Highlands, Trotternish's crofting townships were profoundly affected by the Clearances and subsequent 19th-century land reform agitation, as sheep farming and later sporting estates reorganised much of the peninsula's land use and population distribution; the Skye Museum of Island Life today interprets this crofting history directly, presenting it as a lived way of life substantially altered rather than romanticising it as timeless tradition.

Emigration from Skye and Trotternish

established Skye sent emigrants overseas long before the famine of the 1840s. The historian Marjory Harper, in Adventurers and Exiles (2003), notes that chain migration made North Carolina a focus for emigrants from Argyll and Skye before the American Revolution, Flora MacDonald and her husband among them. In 1791 some 200 would-be emigrants from Skye, stormbound at Greenock, were recruited instead by David Dale for his cotton mills at New Lanark. In 1802 Lord Selkirk's agents signed up Hebridean families from Mull, Skye and the Uists for his Prince Edward Island colony, which 800 emigrants reached in 1803.

established Northern Skye kept that Prince Edward Island connection. In January 1829 the Inverness Journal reported that "several hundred souls" from Lord MacDonald's estates were to sail for the island, recruited by two fellow islanders in a venture "partly a trading speculation, and partly an act of philanthropy". Harper records that 84 families arrived in 1829 and named their settlement Uigg, beside Selkirk's settlement at Belfast, and that through the 1830s and 1840s many more followed from Lord MacDonald's lands in Kilmuir, Snizort and Portree, the parishes that cover Trotternish. The estate manager John Bowie told the 1841 select committee that 1,250 of the 1,850 Skye emigrants he had sent out since 1837 had chosen Prince Edward Island and Cape Breton, because their countrymen were already there.

shared How willing these emigrants were is disputed. Bowie told the Poor Law inquiry of 1844 that Lord MacDonald's Skye and North Uist tenants showed "an anxious desire to emigrate". The ministers of Strath and Portree told the same inquiry the opposite: the people were not disposed to go if they could live at home, and poor reports from earlier emigrants had made them less inclined. By then the potato famine was approaching. In summer 1849 removal notices were served on 600 families on Lord MacDonald's Skye estates, and even the pro-emigration Scotsman called the expected eviction of about 3,000 people "an extremely painful" case. In 1851 Thomas Fraser, Sheriff Substitute of Skye, told Sir John McNeill that "a considerable emigration is indispensable". Fraser's scheme grew into the Highland and Island Emigration Society, which sent Skye families to Australia from 1852. Harper's wider argument, that most Highland emigrants responded to opportunity as well as to coercion, is contested by historians of the Clearances such as James Hunter, who give more weight to landlord pressure.

established Skye emigrants also shaped the places they settled, not always for the good. Harper notes that Angus McMillan, an emigrant from Skye who explored Gippsland in Victoria from 1840, played a leading part with other Scottish settlers in the Warrigal Creek massacre of 1843, in which an estimated 60 to 150 Aboriginal people were killed.

Ecology and distinctive natural features

The Trotternish landslip terrain creates a distinctive mosaic of habitats: exposed basalt cliff faces and scree slopes support specialist plant communities, while the complex terraced ground of the Quiraing and the sheltered hollows beneath the Storr's pinnacles create microclimates favouring particular montane and coastal plant species. Kilt Rock, further north along the peninsula's coast, exposes the same basalt-over-sediment structure in dramatic cliff section, its name derived from the tartan-like banding visible in the exposed rock strata, with a waterfall dropping directly from the clifftop to the sea below. The peninsula's cliffs and moorland support breeding seabirds and raptors, and its varied geology makes it a site of ongoing interest to geomorphologists studying large-scale slope failure processes.

National identity, recreation, and tourism

Trotternish today anchors much of Skye's modern tourism economy and visual identity, with the Old Man of Storr and the Quiraing ranking among the most photographed landscape features in Scotland and appearing extensively in film, advertising, and social media. This popularity has brought real management pressure: footpath erosion, parking congestion at peak season, and a steady stream of mountain rescue incidents among visitors who underestimate the terrain's steepness and slipperiness have all required active management responses from NatureScot, local landowners, and the Highland Council in recent years — a reminder that the "wild, empty" framing often used in marketing sits alongside genuine visitor-management infrastructure and real safety risk. The peninsula is deliberately treated here as a distinct landscape from the Cuillin further south on Skye: where the Cuillin is technical mountaineering terrain built on gabbro, Trotternish is accessible (if genuinely steep and sometimes hazardous) hillwalking terrain built on a basalt-over-sediment landslip, and the two should not be conflated as a single generic "Skye mountains" story.

Gaelic on Skye

established Skye has been Gaelic-speaking throughout its recorded history. Ministers writing for the Statistical Accounts, collected by the historical geographer Charles Withers in Gaelic in Scotland 1698–1981 (1984), show English arriving slowly. In 1795 the minister of Portree complained that Gaelic was "much corrupted by a mixture of English words, which the common people, ambitious to be thought to understand something of that language, are fond of using on every occasion". In 1841 his successor credited "steam navigation and Parliamentary roads" with giving the people "a taste for the English language". At Kilmuir in 1840 the young men who went south each year for work brought back "a smattering of English".

established In 1815 the minister of Kilmuir reported that people taught to read Gaelic in the new Gaelic schools were "becoming anxious for English Teachers", confirming, he wrote, that "to cultivate the Gaelic language is a certain though indirect road to promote the study of the English". By 1867 Sheriff Nicolson found Skye children addressing each other in English "as often as in the mother tongue". Even so, Portree was 81 per cent Gaelic-speaking in the 1881 census, and the Skye and Lochalsh district 54 per cent in 1981, the highest share anywhere outside the Western Isles. Sabhal Mòr Ostaig, the Gaelic college at Sleat, was founded in 1973.

Harpers at Duntulm and Dunvegan

established In the 17th century the two great houses of Skye both kept music of the old Gaelic kind. Keith Sanger and Alison Kinnaird, in Tree of Strings (1992), the standard history of the harp in Scotland, quote the poet Iain Lom on the MacDonald stronghold at Duntulm in Trotternish. One poem promises "harps and fair-bosomed women" in the tower of Domhnall Gorm Òg MacDonald. Another follows Sir Donald MacDonald of Sleat's galley home to "Duntulm of the robust men", where minstrels greet his young bride, Margaret Douglas, daughter of the Earl of Morton, whom he married in 1662, with "the shining harps", as quoted by Sanger and Kinnaird. At Dunvegan, on the other side of the island, Iain Breac MacLeod kept the blind harper and poet Roderick Morison (Ruairidh Dall) as his household harper until 1688, alongside the MacCrimmon pipers. A separate article covers Morison.

shared Two visiting Irish harpers are linked with the MacDonalds of Sleat. Arthur O'Neill's memoirs say the famous Ruairi Dall Ó Catháin died "in a nobleman's house" and left his harp and a silver tuning key there; Sanger and Kinnaird identify the house as that of Sir James MacDonald of Sleat (died 1678). A century later the Irish harper Echlin O'Kane played for Alexander, Lord MacDonald, in Sleat. Boswell, touring with Johnson in 1773, was told that the laird had given O'Kane a jewelled harp key worth 80 or 100 guineas. Lord MacDonald replied in a letter of 1785 that he had dismissed "the drunken blind harper" with two guineas and a key "made of common agate". Sanger and Kinnaird, following Colm Ó Baoill, suspect the story of Ó Catháin's key was O'Kane's own invention.

traditional Skye folklore gave the harp a darker side. A tale told on Skye and Eigg, "How Music first came to the Western Isles", has a mother sell her soul so that her son can play a harp found floating in the sea; in the Skye version he can afterwards play only sad music. Martin Martin, the Skye-born writer, recorded about 1695 the belief in the Western Isles that spirits made sounds in the air "resembling those of a Harp, Pipe".

• The Quiraing landslip is the largest mass-movement slide in Britain, with its disturbed zone extending across more than two kilometres.
• Some sections of the Trotternish escarpment are still actively moving today, meaning the landscape is not a static "ancient" feature but an ongoing geological process.
• The Old Man of Storr, now one of Scotland's most photographed rock pinnacles, was not successfully climbed until 1955.
• Kilt Rock takes its name from the tartan-like banding pattern visible in its exposed basalt-over-sediment cliff face, not from any clan or textile history.
• Duntulm Castle's site was used in succession by Iron Age, Viking, and medieval Scottish occupants long before its final MacDonald-era castle structure.
• Flora MacDonald raised several of her children at Flodigarry on Trotternish before the family later emigrated, a quieter chapter of her life than her famous Jacobite escape story.
• The basalt lava flows capping Trotternish are part of the same Palaeogene North Atlantic volcanic episode that produced the gabbro of the Cuillin further south and the Giant's Causeway in Northern Ireland.
• The Skye Museum of Island Life at Kilmuir, on Trotternish, preserves original thatched crofting buildings illustrating a way of life substantially ended by the Clearances and later agricultural change.
• There is a Uigg on Prince Edward Island, founded in 1829 by families from Lord MacDonald's estates in northern Skye.
• Gaelic poetry describes harps playing in Duntulm Castle in the 17th century.

• Do not describe the Storr and Quiraing landscape as simply "ancient and unchanging" — it is the product of ongoing mass-movement landslip processes, and parts of the escarpment remain actively moving today.
• Avoid conflating Trotternish with the Cuillin as a single "Skye mountains" story; they are geologically and experientially distinct landscapes, and this card should be read alongside, not duplicating, the separate Cuillin card.
• Romantic popular narrative around Flora MacDonald sometimes overstates dramatic or ideological details beyond what contemporary sources support; her documented residence at Flodigarry and role in the 1746 escape are established, but embellished anecdotes should be flagged as traditional.
• Place-name folklore for individual Quiraing features (such as fanciful origin stories for named rock formations) should be treated as legend-myth unless a documentary source is available.
• Do not treat every emigrant from Skye as a cleared exile. Some left under eviction notices, but many paid their own way to join relatives in Prince Edward Island and Cape Breton.
• Do not repeat the story of a jewelled harp key given by Lord MacDonald to Echlin O'Kane as fact; Lord MacDonald himself said it was common agate.
• Tourism material sometimes implies the Old Man of Storr walk is an easy stroll; the path is genuinely steep and has caused injuries, and should not be minimised.