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Snowdon Peak is a 13,077-foot-elevation (3,986-meter) mountain summit located in San Juan County, Colorado, United States. [3] It is situated seven miles south of the community of Silverton , in the Weminuche Wilderness , on land managed by San Juan National Forest .
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)
Y Lliwedd is a mountain, connected to Snowdon in the Snowdonia National Park, North Wales. Its summit lies 898 metres (2,946 ft) above sea level. The eastern flanks are steep cliffs rising above Glaslyn and Llyn Llydaw. Y Lliwedd is the most conspicuous of the peaks for those who approach Snowdon via the Miners' and Pyg tracks.
Yr Aran is a mountain peak on a ridge radiating south from Snowdon, Wales' highest mountain, with views of the summit of Snowdon, Moel Hebog and the Nantlle Ridge.It has an elevation of 747.2 m (2,451 ft) and a prominence of 235 m (771 ft).
Mount of the Holy Cross is a high and prominent mountain summit in the northern Sawatch Range of the Rocky Mountains of North America.The 14,011-foot (4270.5 m) fourteener is located in the Holy Cross Wilderness of White River National Forest, 6.6 miles (10.7 km) west-southwest (bearing 244°) of the Town of Red Cliff in Eagle County, Colorado, United States.
All the major mountain ranges in the state of Colorado, United States, are considered subranges of the Southern Rocky Mountains. As given in the table, topographic elevation is the vertical distance above the reference geoid , a mathematical model of the Earth's sea level as an equipotential gravitational surface.
The iconic narrow gauge railway climbing Wales’ highest peak is the ultimate closer-to-home bucket-list experience; Daniel Fahey gives the lowdown on what to expect
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.