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. The large rock fragments which cover the ground on the upper part of the mountain are all made of these grey volcanic lavas. These form the Ben Nevis central ring complex (Strachan et al., 2002). 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. Ben Nevis, in the Western Highlands, is Britain’s highest mountain. Ben Nevis was formed approximately 350 million years ago when a volcano collapsed.See the related Wikipedia link listed below for more information: Ben Nevis, highest mountain of the British Isles, in the Highland council area, Scotland. Volcanic eruptions, in this area, added layers of lavas on top. Two huge magma chambers developed in the Glen Nevis area, one in the Mamores and another formed directly beaneath what is now the summit of Ben Nevis. Ben Nevis History. Ben Nevis Visitor Centre » Geology of the Glen. Snow can be found on the mountain nearly all throughout the year. This, and many other Scottish peaks, are made of granite, a rock that resists erosion well. It’s peak is the collapsed dome of the volcano that imploded millions of years ago. James Roberston, a botanist from Edinburgh, was the first person to climb to the top of Ben Nevis. Glen Nevis is a beautiful place and a Geologist’s idea of heaven! 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. The mountain was formed when the roof of a huge volcanic caldera collapsed. Ben Nevis is all that’s left of an ancient volcano. The heat and pressure baked the surrounding crustal rocks into schists and domed them up. Another early ascent was in 1774 by John Williams, who provided the … Ben Nevis is the highest mountain in the British Isles. 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. Geologist Noel Williams describes the unusual geology of Ben Nevis. The liquid granite magma was originally forced up into (intruded) the surrounding rocks deep beneath an active volcano about 350 million years ago. 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. Snow lies in some parts all how was ben nevis formed like fault or fold Roger Federer Beats Andy Murray to Win 2008 US Open Final. 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