Gordon, J.E. and Sutherland, D.G. GCR Editor: W.A. Wimbledon. 1993. Quaternary of Scotland. Geological Conservation Review Series No. 6. JNCC, Peterborough, ISBN 0 412 48840 X.
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J.E. Gordon
Sections in the stream gully at Drumhollistan show the till succession on the north coast of Caithness and allow interpretation of the associated patterns of ice movement.
Drumhollistan
The deposits are exposed along a narrow stream valley that deepens to over 30 m at its western end. The flanks of the valley are heavily dissected by gullies separated by narrow, intervening ridges. The deposits were recorded by Omand (1973) and comprise the following composite sequence:
| 4. Head | up to 1 m |
| 3. Brown till with shell fragments near the base | up to 21 m |
| 2. Sand and gravel; boulders up to 0.75 m length in the lower 1.5 m, fining upwards | up to 3.5 m |
| 1. Grey till | > 3 m |
The lower till (bed 1) is exposed only at the western end of the gully. It is lighter in colour than the upper till and the matrix appears gritty and sandy. No shells have been found in it. A stone count of 50 clasts by Omand (1973) revealed that 94% of the sample consisted of gneiss or migmatite, probably derived from the area to the south and west of the site. At the western end of the gully on the south side, the lower till is overlain by unbedded sand and gravel with a layer of sand at the top. The upper till (bed 3) in its lower part is a darker, chocolate-brown colour with a sandy/silty matrix. Of 50 clasts sampled by Omand, 76% were from the Old Red Sandstone group and probably derived from the area to the south-east of the site. The upper part of the till is weathered to a depth of 5–6 m and has a reddish appearance. A few shell fragments were found in this till, but they are scarce and considerably comminuted in comparison with those at Dunbeath and other sites on the east coast of Caithness. On the north side of the gully the brown till (bed 3) rests directly on the grey till (bed 1). The lower layers of the former are bouldery with lenses of sand and gravel in the lower 3 m.
In the middle part of the gully on the south side, a layer of sand occurs at the base of the upper till. Possibly it corresponds with the sand and gravel at the western end of the section, but the continuity of the beds could not be traced because of slumping. Bands of the upper till are interbedded with the sands which here have a rusty, weathered appearance, and the two units interdigitate.
A stone layer occurs at the surface of the upper till beneath a cover of peat. On the northern side of the gully at the western end, up to 1 m of head locally covers the upper till.
An additional feature of the site is the fine example it provides of active gullying and incipient earth pillar formation along the corrugated and dissected flanks of the main gully.
The general characteristics and distribution of the glacial deposits of Caithness, the theories proposed to explain them and the outstanding problems have already been discussed. The evidence at Drumhollistan appears to confirm two distinct ice movements on the north coast followed by a period or periods of weathering and head formation. The lower till, associated with a northerly ice movement occupies a similar stratigraphic position to the lower till at Dunbeath, but it is still open to question whether it represents an early local glaciation or was broadly contemporaneous with the shelly till as at Dunbeath (Hall and Whittington, 1989). The upper till is part of the widely recognized shelly till of Caithness deposited by ice moving northwest. The weathering of the upper part of the sequence at Drumhollistan is typical of many parts of Caithness (Jamieson, 1866; Peach and Horne, 1881c; Omand, 1973; Hall and Whittington, 1989), as is the overlying head (Omand, 1973; Futty and Dry, 1977; Hall and Whittington, 1989).
In south-east Caithness, Hall and Whittington (1989) noted weathering and mottling of the tills, with decalcification to a depth of 2.7 m. They concluded that this was compatible with Holocene weathering. Although the weathering at Drumhollistan extends to a greater depth of 5–6 m, this could reflect local factors and is still compatible with depths of Holocene weathering in eastern England (Madgett and Catt, 1978; Eyles and Sladen, 1981). At present there is no evidence that the weathering in Caithness might reflect a long period of ice-free conditions during the Devensian. The head deposits at Drumhollistan are undated, but in south-east Caithness comparable deposits have been ascribed to the Loch Lomond Stadial (Hall and Whittington, 1989). Again, there is no evidence that they might relate to periglacial episodes earlier in the Devensian, although this cannot be completely ruled out without further work.
Drumhollistan has not been investigated in detail, and (as is also the case for Baile an t-Stratha) several intriguing questions remain unanswered about the deposits, their wider relationships with other sites and the implications they carry for the Pleistocene history of Caithness. These concern:
Drumhollistan is an important reference site for the succession of Pleistocene deposits on the north coast of Caithness. It demonstrates the western extent of the shelly till and the northern extent of local till, together with evidence for subsequent head formation and weathering. Comparable sites to Drumhollistan on the south-east coast of Caithness that show shelly till superimposed on local till, occur at Dunbeath (Baile an t-Sratha), Leavad and Latheronwheel (Omand, 1973; Hall and Whittington, 1989).
Baile an t-Sratha is notable for better exposure of local till and better preservation of shells in the upper till, whereas at Leavad the main interest is a large erratic of soft strata incorporated in the shelly till. Exposures at Latheronwheel are poor and have not been recorded in detail. Together, therefore, Drumhollistan, Baile an t-Sratha and Leavad demonstrate key aspects of the Pleistocene deposits of Caithness.
The contemporary erosion and gullying of the till are also of interest and are representative of a type of phenomenon that is known from a number of localities in Scotland, for example at Rosemarkie Dens (Miller, 1858; Geikie, 1901), Fochabers (Hinxman and Wilson, 1902; Geikie, 1903) and in the Nairn valley near Clava. The narrow ridges illustrate an incipient form of earth pillar formation, although the absence of large boulders has inhibited the development of classic earth pillars (cf. Whalley, 1976b).
The deposits at Drumhollistan demonstrate the glacial history of the north coast of Caithness. They show two (ice-deposited) tills, locally separated by a layer of sand and gravel. The value of the site is as a reference locality for establishing the glacial succession and pattern of ice movements in this area. There are different interpretations of the age of these deposits and whether they were formed during the Early or Late Devensian (approximately 65,000 and 18,000 years ago, respectively).