Ben Vane (Scottish Gaelic: A' Bheinn Mheadhain) is a Scottish mountain situated in the southern Highlands. The underlying geology almost entirely comprises the Beinn Bheula Schist Formation - psammite and pelite with a Siluro-Devonian dyke prominent round the northern and eastern face. It is one of the Arrochar Alps and stands slightly separate from the other mountains of the group being connected on its western side to the neighbouring Beinn Ìme by a low col at 492 metres. Ben Vane itself just qualifies as a Munro reaching a height of 915 metres (3,002 feet) and is characterised by steep and rugged slopes which fall away to the Inveruglas Water to the east and the Allt Coiregroigan to the south; to the north the descent is more undulating going over the subsidiary top of Beinn Dubh before