Fola is often classed as part of Glen Coe (see for example the location of Glencoe ski centre), but is in fact part of the upper reaches of Glen Etive. The south side of the glen is marked by a succession of distinct peaks: Buachaille Etive Beag at the eastern end, followed by the Three Sisters, shoulders of the Bidean nam Bian massif which are subdivided by Coire Gabhail and Coire nan Lochan. The name Coire Gabhail (corrie of the bounty, or hollow of capture) refers to former times when the corrie was used by members of Clan MacDonald to hide cattle and other livestock, whether their own or stolen from others. The wide flat glen is well suited for this purpose since from Glen Coe it appears to be a normal v-shaped glen approached only by a steep narrow gorge. Summits in the Bidean nam Bian massif include Stob Coire Sgreamhach, Stob Coire nan Lochan and Aonach Dubh (the third "sister"). By contrast the north side of the glen is a stark wall of mountain, the Aonach Eagach ridge. The ridge is crossed at the eastern end by the Devil's Staircase, an old military road opposite Buachaille Etive Mòr. The western end terminates with the conical Pap of Glencoe (Sgùrr na Cìche), above Glencoe village, at the point where the glen opens out to Loch Leven. Other than a few scattered farms, the only settlement in Glen Coe is the village of Glencoe, which lies at the western end of the glen close to Invercoe where the river joins Loch Leven. About to the west, on the southern shore of the loch, is the village of Ballachulish, known in the past for its slate quarries, which have been worked since 1693. Climate Geology Geologically speaking, Glen Coe is the remains of an ancient supervolcano. The caldera forming eruptions took place about 420 million years ago during the Silurian period, and the volcano has long since become extinct. The glen is considered to be one of the best examples of a subsidence caldera, being the place where this phenomenon was first described. A caldera is a volcanic process in which a circular fault allows a section of crust to sink, leading to magma being forced to the surface at the periphery. This sinking allows layers of rock which would otherwise have been eroded to remain visible, can be seen in