Around 400 million years ago, the rocks that form the area around Ben Nevis were part of a chamber of molten rock in the upper layers of earth’s crust. Both mountains are among the nine in the UK over 4,000 feet (1,200 m), as are Aonach Mòr and Aonach Beag (1,234m) immediately to the east; the other five are all in the Cairngorms. The large rock fragments which cover the ground on the upper part of the mountain are all made of these grey volcanic lavas. James Roberston, a botanist from Edinburgh, was the first person to climb to the top of Ben Nevis. A History… The first recorded ascent of Ben Nevis was made on 17 August 1771 by James Robertson, an Edinburgh botanist, who was in the region to collect botanical specimens. Glen Nevis is a beautiful place and a Geologist’s idea of heaven! Snow can be found on the mountain nearly all throughout the year. The mountain was formed when the roof of a huge volcanic caldera collapsed. Snow lies in some parts all Ben Nevis History. Geologist Noel Williams describes the unusual geology of Ben Nevis. There are 6 main stopping points along a ‘geo trail’ that help to explain the forces that have shaped the glen we see today: glacial features that will fascinate even the novice geologist. how was ben nevis formed like fault or fold Roger Federer Beats Andy Murray to Win 2008 US Open Final. Its summit, reaching an elevation of 4,406 feet (1,343 metres), is a plateau of about 100 acres (40 hectares), with a slight slope to the south and a sheer face to the northeast. Andy Murray failed to produce his best tennis and fell at the last hurdle losing the US Open final to former world number 1 Roger Federer 6-2, 7-5, 6-2. He did this on 17th August 1771. Ben Nevis Visitor Centre » Geology of the Glen. Volcanic eruptions, in this area, added layers of lavas on top. Another early ascent was in 1774 by John Williams, who provided the … Ben Nevis Geography Ben Nevis forms a massif with its neighbour to the north-east, Carn Mòr Dearg (1,223m), to which it is linked by the Carn Mòr Dearg Arête. Remains of these lavas can be seen forming the upper half of Ben Nevis. Ben Nevis is all that’s left of an ancient volcano. Ben Nevis is the highest mountain in the British Isles. It is located at the western end of the Grampian Mountains, close to the town of Fort William. These form the Ben Nevis central ring complex (Strachan et al., 2002). This, and many other Scottish peaks, are made of granite, a rock that resists erosion well. The liquid granite magma was originally forced up into (intruded) the surrounding rocks deep beneath an active volcano about 350 million years ago. 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