Falkirk - Geography

Geography

Falkirk is located in an area of undulating topography between the Slamannan Plateau and the upper reaches of the Firth of Forth. The area to the north of Falkirk is part of the floodplain of the River Carron. Two tributaries of the River Carron - the East Burn and the West Burn flow through the town and form part of its natural drainage system. Falkirk sits at between 50 metres (164 ft) and 125 metres (410 ft) above sea level.

The underlying geology of the town of Falkirk is characterised by glacial deposits. Elevations above 100 metres (328 ft) are covered by a mixture of glacial till and boulder clay with low lying areas covered by sandy soils and loams. As Falkirk is not far from the coast, post-glacial features akin to raised beaches are particularly predominant to the north of the town centre, and this gives rise to differing elevations within the town.

Unsorted glacial till gives rise to such features of glacial deposition as eskers, and drumlins which are predominant over much of the area. Such elements provide natural transport routes and it is this complex underlying geology that the town is built upon.