| Cadair Idris | |
|---|---|
Llyn Cau within the steep rock walls of Craig Cau. Penygadair, the summit of the mountain, is to the right |
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| Elevation | 893 m (2,930 ft) |
| Prominence | 608 m (1,995 ft) |
| Parent peak | Aran Fawddwy |
| Listing | Marilyn, Hewitt, Nuttall |
| Translation | Chair of Idris (Welsh) |
| Pronunciation | Welsh: [ˈkadair ˈɪdrɪs] |
| Location | |
| Location | Gwynedd, Wales |
| Range | Snowdonia |
| Topo map | OS Landranger 124, Explorer OL23 |
| OS grid | SH711130 |
| Climbing | |
| Easiest route | Hike |
Cadair Idris or Cader Idris is a mountain in Gwynedd, Wales that lies at the southern end of the Snowdonia National Park. The peak, which is one of the most popular in Wales for walkers and hikers, [1] is composed largely of Ordovician igneous rocks, with classic glacial erosion features such as cwms, moraines, striated rocks, and roches moutonnées.
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The name of the mountain has several theories. The most well known is that Cadair Idris (English: the chair of Idris) is in reference to a giant of Welsh mythology who was said to have used Llyn Cau as an enormous armchair to gaze at the stars. [2] The spelling Cader Idris is also found in both Welsh and English, as reflected in the local name of the local secondary school, Ysgol y Gader (never Ysgol y Gadair). [2] Although cader is not incorrect, Cadair Idris is the form used on current maps in reflection of modern standardised Welsh spelling.
An alternative theory is that a 7th-century Meirionnydd prince Idris ap Gwyddno (or Gweiddno) won a battle against the Irish on the mountain. [2] Cadr is the Welsh word for stronghold which sounds similar to the Welsh word for chair cadair. Cad is also a prefix that relates to battle. Cadr Idris may have been the stronghold of Idris ap Gwyddno.[3]
The entire mountain is called Cader Idris but its summit is known as Penygader (English: top of the chair).
| Listed summits of Cadair Idris | ||||
| Name | Grid ref | Height | Status | |
|---|---|---|---|---|
| Mynydd Moel | SH727136 | 863 metres (2,831 ft) | Hewitt Nuttall |
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| Cyfrwy | SH703133 | 811 metres (2,661 ft) | Hewitt Nuttall |
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| Craig Cwm Amarch | SH710121 | 791 metres (2,595 ft) | Hewitt Nuttall |
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| Gau Graig | SH744141 | 683 metres (2,241 ft) | Hewitt Nuttall |
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| Tyrrau Mawr | SH677135 | 661 metres (2,169 ft) | Hewitt Nuttall |
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| Craig-y-llyn | SH677135 | 622 metres (2,041 ft) | Hewitt Nuttall |
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There are three main trails that lead to the top of Cadair Idris. The summit, which is covered in scree, is marked by a trig point. There is also a low-standing stone shelter with a roof.
This route, which begins in the north from either Dolgellau or the Mawddach estuary, is the easiest but the longest of the main trails. Its length from the mountain's base is 5 kilometres (3.1 mi) with a 600 metres (2,000 ft) climb.
This is the most direct way to the summit as the trail leads straight up the northern face. The 3.8 kilometres (2.4 mi) ascent involves a climb up a 310 metres (1,020 ft) cliff-scree face. However this part of the Fox's Path has been heavily eroded in recent years making the descent dangerous.
This route starts on the southern side of the mountain near the glacial Tal-y-llyn Lake. Hikers using this ascent climb past Llyn Cau and along the rim of Craig Cau (rockwall) to Penygadair. Its length is 4.4 kilometres (2.7 mi) and involves two climbs of over 300 metres (980 ft).
The crater-like shape of Llyn Cau has given rise to the occasional mistaken claim that Cadair Idris is an extinct volcano. This theory was discounted as early as 1872, when Charles Kingsley commented in his book Town Geology [4]:
| “ | I have been told, for instance, that that wonderful little blue Glas Llyn,[5] under the highest cliff of Snowdon, is the old crater of the mountain; and I have heard people insist that a similar lake, of almost equal grandeur, in the south side of Cader Idris, is a crater likewise. But the fact is not so. | ” |
The natural bowl-shaped depression was formed by a cirque glacier during the last ice age when snow and ice accumulated in the corries due to avalanches on higher slopes. In these depressions, snow persisted through summer months, and becomes glacial ice. The cirque was up to a square kilometre in size surrounded on three sides by steep cliffs. The highest cliff was the headwall. The fourth side was the "lip" from which the glacier flowed away from the cirque. Over thousands of years ice flowed out through the bowl's opening carving the chair of Caldair Idris.
As the glacier eroded the lip down to the bedrock, there are several tear-drop shaped hills above the edge of Lyn Cau. These geologically-important rocky outcrops are called roche moutonnée (English: sheep-like rock) and were formed from the abrasive action of the ice.
Much of the area around Cadair Idris was designated a National Nature Reserve in 1957, and is home to arctic-alpine plants such as purple saxifrage and dwarf willow .[6]
There are numerous legends about Cadair Idris. Some nearby lakes are supposed to be bottomless, and anyone who sleeps on its slopes alone, will supposedly awaken either a madman or a poet. This tradition (of sleeping on the summit of the Mountain) apparently stems from bardic traditions, where bards would sleep on the mountain in hope of inspiration.[7]
The mountain's name refers to the mythological giant Idris (Idris Gawr) who was said to have been skilled in poetry, astronomy and philosophy.[7] The name has sometimes been mistranslated by some popular authors as Arthur's Seat, in reference to King Arthur (and to the hill of the same name in Edinburgh), an idea used by author Susan Cooper in her book The Grey King. However, this is a modern invention and there is no etymological or traditional connection between Idris and Arthur.
In Welsh mythology, Cadair Idris is also said to be one of the hunting grounds of Gwyn ap Nudd and his Cŵn Annwn. The howling of these huge dogs foretold death to anyone who heard them, the pack sweeping up that person's soul and herding it into the underworld.
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