Calton Road runs from nearby the Palace of Holyroodhouse to Leith Street. The road passes underneath Waterloo Place through the ravine between Calton Hill and Princes Street. This area was previously known as the Low Calton. Arthur's Seat and Salisbury Crags form an unmistakable part of Edinburgh's skyline. Rising 247 metres above sea level Arthur's Seat is one of five visible volcanic vents left over from volcanic activity in the area 354 million years ago. The peak's name is possibly a corruption of the gaellic Ard-na-saith, meaning height of arrows, indicating a past usage as a practice place for archery. It is also known as the Lion's Head. Salisbury Crags are an igneous sill, composed of cooled magma during the period of volcanic activity and later shaped by glacial erosion. The steep cliffs of the crags provided natural defence for early human inhabitants. Traces of a stone rampart dating from the early part of the first millennium BC have been found there. More recently James Hutton's studies of the Crags led to the release in 1788 of his 'Theory of the Earth', the work which established him in the eyes of many as the father of modern geology.