Hudson, J.D., Miller, A.D., Allwright, A. (2016) The geology of Eigg: a description of the geology of Eigg for all those interested in the landscape and natural history of the Hebrides, with suggested excursions. Edinburgh: Edinburgh Geological Society
Excursion 5: Eilean Thuilm and Sgor Sgaileach—reptile bones and a columnar sill
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More spectacular views, impressive columnar cliffs, and a chance to find bones of a plesiosaur. This is a strenuous walk, involving a steep grassy climb followed by a descent over rough landslipped ground without a marked path.
Bealach Thuilm
The best access to the north-east corner of the island is from Howlin
As you descend to the north, the scene changes dramatically. The green fields of Cleadale and the white sandy bays are lost from view. The north-facing cliffs are dark basalt in their upper part, with sandstone beneath; the shore shows black basalt sills, and the slopes between are a jumble of landslip debris. It is a remarkable change from one of the sunniest scenes in the Hebrides to one of gloomy grandeur. The Cuillin of Skye stand proud to the north. The contact between the Valtos Sandstone and the basalt represents a long period of erosion, for the higher Jurassic strata seen around Laig are absent here. Pick your way among the tumbled landslips of Talm and descend towards Eilean Thuilm.
The shore at Eilean Thuilm
The storm beach
The Sgor Sgaileach columnar sill
Eilean Thuilm is made of quartz porphyry (page 21), which also makes the red- weathering columnar cliffs of Sgor Sgaileach that form the north-eastern extremity of Eigg. Sloping surfaces just west
Cliff erosion
The northern basalt cliffs give a fine opportunity to examine the various means by which cliffs retreat. In places, screes form from small detached rock fragments. At others, large blocks record catastrophic rock falls. The locus of scree formation has evidently changed over comparatively recent time, for all that we can now observe post-dates the last glaciation. The largest process of cliff recession is the formation of rotational landslips, best seen on the east coast (Excursion 6). A combination of these processes has formed the jumbled topography of Talm.
Return to Cleadale by climbing back to Bealach Thuilm and thence to Howlin.
Excursion 5 extension: Beinn Bhuidhe
Those with remaining energy can climb the heathery slope above the col, which here gives access to the Beinn Bhuidhe plateau, between the inaccessible cliffs above Cleadale to the south and above Talm to the east. There is a zigzag path, which led to former peat diggings on the plateau. Follow the western edge of the plateau, above the basalt cliffs, to the summit, being rewarded with even more spectacular views, and alpine flowers such as Dryas octopetala and Silene acaulis. Return the same way or continue southwards, eventually regaining the road beyond Cuagach, but the going is very rough.