The Torrent is a long meandering river, which drains the hills to the north-west of Dungannon. The underlying geology is varied and includes basal clastic, carboniferous limestone, coal and Old Red Sandstone.
The Torrent is a winding watercourse, which drains the hills to the northwest of Dungannon. The underlying terrain is diverse and comprises basal clastic, carboniferous limestone, coal, and Old Red Sandstone.