Garvellachs
The Garvellachs or Isles of the Sea form a small archipelago in the Inner Hebrides of Scotland. The islands include Garbh Eileach, Dùn Chonnuill and Eileach an Naoimh. Part of the Argyll and Bute council area, they lie in Firth of Lorne west of Lunga and northwest of Scarba and have been uninhabited since the 19th century.
The islands are known for their early Christian connections to Brendan the Navigator and Columba and for their bedrock containing rare formations in relation to the global Sturtian glaciation.
Overview
The waters surrounding the islands are extensively used for leisure sailing. Due to the array of separate tidal races produced by the underwater topography there are some treacherous stretches of water. These include the Grey Dog between Scarba and Lunga and the Gulf of Corryvreckan, between Scarba and Jura, in which is located the infamous Corryvreckan whirlpool, which is the third-largest whirlpool in the world.The area is part of the Scarba, Lunga and the Garvellachs National Scenic Area, one of 40 such areas in Scotland, which are defined so as to identify areas of exceptional scenery and to ensure its protection by restricting certain forms of development. The Scottish plant collector, Clara Winsome Muirhead surveyed the plant life of the islands and published The Flora of Easdale and the Garvellachs in 1962.
Garbh Eileach is the largest island in the group and extends to and reaches a maximum elevation of above sea level. The area of Eileach an Naoimh is and the maximum height. A' Chùli lies between the two and is in extent with Dùn Chonnuill, the northernmost isle, being roughly half this size.
Etymology
Na Garbh Eileacha is Gaelic for "the rough rocks" with the Anglicised version of the name giving rise to the archipelago's name of the Garvellachs. Garbh Eileach itself then means the "rough rock" or "rough rocky mound". Eileach an Naoimh is from na h-Eileacha Naomha and means either "the rocky place of the saint" or "the holy rocks". A’ Chùli is from Cùil Bhrianainn meaning "Brendan's retreat" and Dùn Chonnuill means "Conal's castle" and may be named after an Ulster chieftain of the first century CE.Geology
The geology of the Garvellachs consists entirely of rocks of the Neoproterozoic Dalradian Supergroup apart from several basaltic dykes of Palaeogene age, associated with the nearby Mull Igneous Centre. The Dalradian rocks come from the uppermost part of the Appin Group and the lowermost part of the Argyll Group. The oldest preserved strata are exposed on the north of Garbh Eileach, a ~70 m thick sequence of carbonates, the Garbh Eileach Formation. The boundary between this and the overlying Port Askaig Tillite Formation is conformable. The Port Askaig Tillites are a sequence of sedimentary rocks that record a series of glacial, interglacial and periglacial episodes. This formation reaches it thickest development of 1,100 m in the area of Islay and the Garvellachs, thinning rapidly away from this region. The formation has been subdivided into five members, the lowest three of which are exceptionally well exposed on the Garvellachs. The sequence contains 48 diamictite beds, while 35–40 % of the formation is formed of sandstone of non-glacial origin, deposited in a deltaic to shallow marine sedimentary environment, interbedded with minor amounts of siltstones and dolomites.There are two candidates within the Cryogenian period for the glacial interval represented by the Port Askaig Tillites, the older Sturtian glaciation (~717–660 million years ago
History
At least three of the four main islands of the Garvellachs were inhabited in the distant past. There is a ruined castle on the top of Dùn Chonnuill that may have been built by the Macleans of Duart in the early fifteenth century after the island was received by them as a gift from King Robert III. The fort consists of walling up to 2.0m high and generally of a similar width. The remains of ten buildings have been identified. Brendan is said to have been buried on A’ Chùli although no trace of his chapel there remains and a similar fate appears to have befallen two unroofed buildings, thought to be shielings, recorded in 1881 by the Ordnance Survey.There is a small anchorage and landing place on Garbh Eileach where there are the remains of a burial ground and of a fort that measures about 14m by 11m. About northeast of this dun there are the ruins of a house and byre with a corn-drying kiln a short distance away, probably erected in the late 18th or 19th century. The island had a population of thirty-two adults in the late 17th century but only four houses were occupied by 1861, and from then on it is likely that only the shepherd's cottage near the landing-place remained in use.
However, the most significant evidence of previous occupation is found on Eileach an Naoimh. About 542, Brendan the Navigator founded a monastery on Ailach, some years before Columba came to Iona. The ruins of the monastic buildings include two chapels, beehive huts, and a graveyard with three crosses and another circular grave. These ruins are amongst the best-preserved early Christian monasteries in Scotland and the site is in the care of Historic Environment Scotland.
Columba is also believed to have visited the island and it is one of the proposed locations of the Columban retreat isle of Hinba. Eileach an Naoimh may be the burial site of Columba's mother Eithne. The monastery was destroyed by Viking raiders who were present in the area from about 800. Although there was a small permanent population in the 1700s the island's intermittent occupation since the Norse settlement of Scotland has likely contributed to the survival of the structures.
A lease dated 1817 granted grazing for 60 cattle and 240 sheep on the archipelago as a whole.