A glance at the geological map reveals a series of bands of colour stretching across the area.  Each band represents a different rock type, a different period in geological history.

One such band reveals where the oldest rocks of the Geopark are to be found - in a belt of country between Llangadog and Llandovery - they belong to the Ordovician period. Just to their south are similar rocks from the Silurian period underyling places like Mynydd Myddfai and Garn Goch.  These rocks chart the coming and going of seas across central Wales.

The broadest band which sweeps from one end of the Geopark to the other is that of the 'Old Red Sandstone' - mostly of Devonian age - the record of the destruction of a Himalayan-size mountain range which had risen to the north of our area.

Further south a narrower band of limestone gives rise to a very special landscape both above and below ground.  It dates from the early Carboniferous period and tells of shallow tropical seas.  It is in turn overlain by the 'Millstone Grit' - the quartz grains of which were carried here by rivers from the north. 

Lastly, along the southern edge of the Geopark, the Coal Measures put in an appearance with their mudstones, sandstones and of course coal seams.

All of these layers have been faulted and folded since their formation, often with dramatic effects on the landscape.

Legacy of the Ice Ages

The presence of all of these rock formations alone would be interesting enough but the dramatically changing climate of the last two million years has added another dimension.  Numerous ice ages have resulted in the sculpting of the bedrock by ice, the scouring of valleys by meltwater and the deposition of eroded fragments as moraines.

Taken all together this rich geological legacy makes for a rewarding area to explore whether you're an expert or have a more casual interest.