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Y Garn is a mountain in Snowdonia, North Wales, part of the Glyderau. It is one of the Welsh 3000s — the 15 summits in Wales over 3,000 feet (914.4 metres) in height. It is the tenth-highest peak in Wales. Moderate snow accumulations can take place on the western-sloping side of the mountain from October to May.
Glyder Fawr is a mountain in Snowdonia, Wales, the highest peak in the Glyderau range at just over 1,000 metres. It is the fifth-highest mountain in Wales and has several walking and scrambling routes leading to its summit. According to Sir Ifor Williams, the word "Glyder" derives from the Welsh word "Gludair", meaning a heap of stones. [1]
The trail is arranged in 13 sections, ranging in length from 3 to 11 miles: [9] (Distances, ascent and time are taken from the website.) Section 1 - Bangor to Bethesda - (Distance: 10.2KM, 6.3MLS ; Ascent: 325M, 1050FT ; Time: 3 – 4hrs)
Llyn Idwal, Summer 2008. Cwm Idwal is a spectacular product of glaciation, surrounded by high crags, screes, moraines and rounded rocks, with a lake on its floor ().Cwm Idwal comprises volcanic and sedimentary rock which was laid down in a shallow Ordovician sea, and later folded to give rise to the distinctive trough-shaped arrangement of strata known today as the Idwal Syncline.
Coed y Brenin (Welsh for King's Forest) is a forest in the Snowdonia National Park, North Wales near Dolgellau at grid reference. It is popular for its mountain bike trails and hiking paths. It has several man-made mountain bike singletrack courses in a woodland setting, varying in length from 12 to 38 km (7 to 23 mi), and one dual slalom course.
Snowdon (Yr Wyddfa) from Crib Goch, Snowdonia. The Welsh 3000s are the 15 Welsh Munros.These are mountains in Wales that are over 3,000 feet (914.4 m). Geographically they fall within three ranges (the Snowdon Massif, the Glyderau, and the Carneddau), but close enough to make it possible to reach all 15 summits within 24 hours, a challenge known as the Welsh 3000s challenge.
To the north of the summit is a small lake, Marchlyn Mawr, which is the upper reservoir for Dinorwig power station, a pump-storage power station hidden inside the mountain. Water from this lake flows through huge tunnels into the lower reservoir Llyn Peris. From the north, Elidir Fawr is very prominent, and can appear to be higher than the ...
The Glyderau were formed in the Ordovician period about 500 million years ago as the result of two land masses moving together and causing the Snowdonia massif to rise up. Since then, erosion and the advance and retreat of glaciers during the Ice Ages has worn down the mountains to their present proportions. The underlying rock is a mixture of ...