Dyffrynnoedd Nedd a Mellte, a Moel Penderyn (grid reference SN921090) is a 421.1 hectare biological and geological Site of Special Scientific Interest on the border of Neath Port Talbot and Powys, Wales, notified in 1954.
The name of the site means "The valleys of Nedd and Mellte and Moel Penderyn".[1]
This site includes the wooded valleys of the rivers Nedd and Mellte and their tributaries above Pontneddfechan as they pass through a millstone grit and limestone plateau, and the hill of Moel Penderyn, which lies to the east. The rivers have eroded deep, narrow valleys in the plateau, which lies some 300 m above sea level, with gorges, river cliffs, block scree, and waterfalls.
Biological interest
The site is of special biological interest for its extensive and diverse semi-natural woodland, important populations of several flowering plants and supporting outstanding assemblages of mosses, liverworts and lichens.
More than 600 species of plant have been recorded from the site, including a very large proportion of the bryophyte flora of mid and south Wales. It is the most southerly known locality in Britain for Marsh Hawk's-beard (Crepis paludosa).
Geological interest
The site's geological interest lies in the range of geological features, well-exposed in the cliffs and rocky river beds. These include exposures at Moel Penderyn, Craig y Ddinas and Bwa Maen. The geomorphological features within parts of the valleys of the Hepste and Mellte are also of special interest.
Access
Large sections of the site are designated open access land. Other sections are accessible via public footpaths.[1]
External links
- SSSI citation sheet, released as part of a response from Countryside Council for Wales to a request made using WhatDoTheyKnow, accessed 13 May 2010.
References
- ^ a b "Dyffrynnoedd Nedd a Mellte, a Moel Penderyn". Countryside Council for Wales / Natural Resources Wales. Archived from the original on 24 October 2013. Retrieved 23 October 2013.
51°46′10.93″N 3°33′51.82″W / 51.7697028°N 3.5643944°W
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This page was last edited on 16 July 2023, at 18:34