glacial landforms left from the last ice age.
An intermittently stagnant ice front has left a classic series of deglacial landforms around the Lough Fea area.
There are often small woodlands on the ends of the drumlins and dense hedgerows around the base, giving visual emphasis to drumlin landforms.
eruptive style, volcanic hazards and the landforms and structures associated with them.
Relating fluvial processes (erosion, transport and deposition) to the formation of fluvial landforms.