Camaderry mountain contains the Luganure mineral vein which is a source of lead in the form of galena (PbS), and also contains traces of silver. In 1859 the Glendasan and Glendalough mines were connected with each other by a series of tunnels called adits, which are now mostly flooded, through the mountain. After several revivals, mining ceased in Camaderry in 1957; however, remains of the Miner's Village at Glendalough can still be seen.