Black Mountains trip report

Bank Holiday weekend and on the Sunday a weather forecast to get enthused about for a late afternoon excursion to the northern escarpment of the Black Mountains. The Black Mountains escarpment is part of the Great Red Edge that runs across the Brecon Beacons National Park, so named due to the underlying Old Red Sandstone bedrock. The Black Mountains have undergone repeated exposure to the action of glacial ice and periglacial processes, yet the plateau areas show little apparent sign of glaciation. Surprisingly, comparatively little research has been published on elucidating the evolution of the Black Mountains landscape. The Black Mountains also held some importance for ancient people, as a number of funerary monuments were built in the adjacent landscape. From some viewpoints on the escarpment a number of Neolithic chambered tombs sited at lower elevations can be viewed and Bronze age cairns also occupy some prominent positions at higher elevations. The reason for the siting of the Neolithic funerary monuments locations remains an enigma.

The plan was to walk along the escarpment, with stops to take in the views and to photograph the expansive views as shower light flitted across the landscape, before looping back over moorland and deciding on where to linger for sunset.
The weather was warm and the ascent made in full sunshine, which made matters unpleasant. When the hill slope eased, unerringly, cloud rolled in and that was the last of the sun for the next couple of hours walking. Stops were made to take in the views from the escarpment, the camera gear was not required. A notable highlight was watching a Kestrel demonstrate its mastery of the wind to quarter the escarpment ridge, at times it hovered a matter of metres away, too close for the binoculars field of view. It was surprisingly warm, even with the absence of sunshine and with a stiff breeze at ~750m ASL, a base layer was sufficient.

A brighter area of sky on the western horizon provided some cause for photographic optimism. However the elevated views were marred by reduced visibility, I guess due to a moisture associated with the low level overhead cloud, whilst lower down below 600m the visibility was good. The air clarity determined where a location for sunset would be and a descent made to an outcrop of bedrock with views.
The nature of the vertical joints/fractures in the bedrock outcrop, appeared to correlate with the orientation of the ridge. It would not be unreasonable to suggest that the geological structure exerted some control on the evolution of the landscape.

The sun did sink into the letterbox of clear sky on the horizon and with overhead cloud, the quality of the resulting light was very good.

Needless to say it was a good trip.