All these karst landforms are the result of long term geomorphological processes typical of this temperate climatic zone.
An intermittently stagnant ice front has left a classic series of deglacial landforms around the Lough Fea area.
As long as the plantlife is not invasive and the vegetation isn't overpowering or there aren't any disruptive landforms, this is an ideal choice.
Our objective was to study the odd landforms developed on the gypsum - deep tubes dissolved into the surface.
Relating fluvial processes (erosion, transport and deposition) to the formation of fluvial landforms.
The range, variety and location of periglacial landforms (to include patterned ground) and their impact on human activity.
There are often small woodlands on the ends of the drumlins and dense hedgerows around the base, giving visual emphasis to drumlin landforms.
This lecture describes the action of wind upon desert sediments and the resultant desert landforms.
We walked up to Easedale Tarn to look at glacial landforms left from the last ice age.