Pen y Fan, Brecon Beacons - from air - Aerofilms postcard c.1970s

Postcard
• Picture / Image:  Brecon Beacons from North West - Pen y Fan centre foreground
• Publisher:  Hunting / Aerofilms Ltd.
• Postally used:  no
• Stamp:  n/a
• Postmark(s): n/a
• Sent to:  n/a
• Notes / condition: 

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Text from the free encyclopedia WIKIPEDIA may appear below to give a little background information (internal links may not  work) :

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Pen y Fan /p?n.?.'væn/ is the highest peak in South Wales and the southern United Kingdom, situated in the Brecon Beacons National Park. At 886 metres (2,907 ft) above sea-level, it is also the highest British peak south of Cadair Idris in Snowdonia. The twin summits of Pen y Fan and Corn Du were formerly referred to as Cadair Arthur or 'Arthur's Seat'.^[1]

The summit lies on a ridge stretching from Talybont Reservoir in the east, to the A470. 500 m (1,600 ft) west lies the subsidiary top of Corn Du, beyond which the terrain drops at a moderate angle to the subsidiary top of Y Gyrn then more steeply to the Storey Arms on the A470. To the east, the ridge drops steeply to the col connecting it to Cribyn, the next mountain along the ridge. From Corn Du, a gentle ridge descends south towards Merthyr Tydfil.

The mountain and surrounding area are owned by the National Trust whose work parties attempt to combat the erosion caused by the passage of thousands of feet up and down this most popular of South Wales' peaks. The mountain is used by the military as part of the selection process of the UK's Special Forces personnel. Four soldiers who collapsed and subsequently died in July 2013 were believed to have been climbing the mountain (see ""Fan Dance"") while undergoing Special Air Service selection.^[2]

Pen y Fan is formed from various units of the Old Red Sandstone which were laid down during the Devonian period. The lower slopes of the mountain are formed from the sandstones and mudstones of the Senni Formation whilst the upper slopes are formed from those of the Brownstones Formation. The very summit, like that of neighbouring Corn Du, is composed of hard-wearing sandstones of the Plateau Beds Formation. The beds of sandstone dip gently southwards towards the South Wales Coalfield basin.
The Brecon Beacons nurtured their own glaciers during the last ice age and both Cwm Llwch and Cwm Sere were excavated by glaciers which grew in the lee of the high ground. Llyn Cwm Llwch occupies a glacially excavated rock hollow and the lake is partly dammed by a late-glacial moraine.^[3] The mountain is the highest point within the Fforest Fawr Geopark which was established in 2005 to promote economic development, particularly sustainable tourism, based on the area's geological heritage.

type=printed

city/ region=brecon

period=post-war (1945 - present)

publisher=aerofilms

postage condition=unposted

number of items=single

size=continental/ modern (150x100mm)