Rhinogydd
The Rhinogydd are a range of mountains in Merionethshire located east of Harlech. The name Rhinogydd derives from the names of two of the more famous peaks, Rhinog Fawr and Rhinog Fach, although the greatest elevation in the range is reached by Y Llethr, 2,480 feet. The name Rhinogydd is a Welsh-language plural form, but the range is also known as the Rhinogs or the alternative Welsh plural Rhinogau.
The Rhinogydd are notably rocky and heather-clad towards the northern end of the range, especially around Rhinog Fawr, Rhinog Fach and towards Moel Ysgyfarnogod. The southern end of the range around Y Llethr, Diffwys and the Ysgethin Valley has a softer, grassy character.
A healthy population of feral goats can also be found in the range. Over 12 square miles of the range are protected as a Special Area of Conservation and a National Nature Reserve.
Contents
Geology
The Rhinogydd are formed of hard sedimentary rocks of Cambrian age which occur as a major anticlinal structure known to geologists as the Harlech Dome. This structure which originated during the Caledonian Orogeny (mountain-building period) extends from Cadair Idris in the south to Blaenau Ffestiniog in the north. Its erosion by successive ice ages has left the valleys and peaks of the Rhinogydd visible today.[1] The core of the area is formed from the hard-wearing greywackes of the Rhinog Formation. The formation also contains and is overlain by some siltstones and mudstones which form a broken zone of softer scenery around the periphery of the area's rugged core. In places, swarms of dolerite dykes cut through the country rocks in a generally northwest-southeast direction. Much of the lower ground is mantled by glacial till, a legacy of the last ice age.[2]
History of geological investigations
The geology of the area was first characterised by Adam Sedgwick and Roderick Murchison in 1835.[3] The Geological Survey began work in the area in 1846 and their first maps were published in 1855.[4] With the discovery of gold in the area in 1846, the state of geological knowledge increased dramatically. At least a dozen major publications appeared between 1844 and 1939.
Hillwalking in the Rhinogydd
The Rhinogydd are far less well known than the areas in the north of the Snowdonia National Park, such as the Glyderau, Carneddau and the Snowdon massif itself. This is due to the rugged nature of the landscape in the Rhinogydd and the fame of Snowdon as the highest peak in Wales. The Rhinog mountains are popular with hillwalkers looking for a more isolated, wilder walking experience.
The peaks of the range are most easily accessed from the west side. Two valleys - Cwm Nantcol ('valley of the Nantcol (stream)') and Cwm Bychan ('small valley') - lead deep into the mountains and may be reached from the village of Llanbedr.
The most popular walking route in this area begins at the Roman Steps at 52°51’17"N, 4°0’18"W, which leads from Cwm Bychan through Bwlch Tyddiad and around Rhinog Fawr. Despite the name, these steps are not Roman and are in fact the well preserved remains of a mediæval packhorse trail leading from Chester to Harlech Castle. At the top of the Roman Steps, the route curves around the eastern end of Rhinog Fawr and enters Cwm Nantcol via Bwlch Drws Ardudwy (The Pass of the Doorway of Ardudwy). A different path leads from Cwm Nantcol, passing around the western end of Rhinog Fawr back to Cwm Bychan via Gloywlyn ('gleaming lake'), completing a circular route that can easily be completed in a day.
Main peaks
The range contains the following Marilyns:
- Y Llethr 2,480 ft
- Rhinog Fawr 2,362 ft
- Y Garn 2,064 ft
- Moel Ysgyfarnogod 2,044 ft
- Moelfre 1,932 ft
the following Hewitts:
- Rhinog Fach 2,336 ft
- Diffwys 2,461 ft
and the following Nuttalls:
- Crib-y-rhiw 2,198 ft
- Diffwys West Top 2,106 ft
- Foel Penolau 2,014 ft
References
- ↑ Snowdonia National Park - The geology of Snowdonia Retrieved 5 January 2012
- ↑ British Geological Survey 1:50,000 scale geological map sheet 135/149 Harlech
- ↑ Sedgwick, A. and Murchison, R.I. 'On the Silurian and Cambrian systems, exhibiting the order in which the older sedimentary strata succeed each other in England and Wales' Rep. Br. Assoc. Adv. Sci. (for 1835 Dublin), Trans., Sect., 59-61
- ↑ Allen, P.M. and Jackson, A.A. "Geology of the Country Around Harlech" British Geological Survey 1985 ISBN 0-11-884367-2
