The Coire Glas site lies within a geologically complex part of the Great Glen. Reporting on the exploratory works states that the site includes two main geological domains: the Great Glen Fault Zone, with heavily sheared and brecciated fault rocks, and the Tarvie
Psammite Formation to the north, which consists of more competent meta-sedimentary rocks dominated by psammite. The exploratory
adit later encountered a zone of very poor, highly deformed rock, which led to further investigation of the fault zone and changes to the support design. ==Proposal==