Английская Википедия:Ben More (Mull)

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Версия от 23:53, 7 февраля 2024; EducationBot (обсуждение | вклад) (Новая страница: «{{Английская Википедия/Панель перехода}} {{short description|966m high mountain in Scotland}} {{Use dmy dates|date=April 2022}} {{Infobox mountain | name = Ben More | native_name ={{native name|gd|Beinn Mhòr}} | photo = Ben More (Mull).jpg | photo_caption = Ben More from the shores of Loch na Keal | elevation_m = 966 | elevation_ref = <ref>{{cite web |url=http://www.walkhighlands.co.uk/munros/ben-more-mull |title=Ben More (M...»)
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Шаблон:Short description Шаблон:Use dmy dates Шаблон:Infobox mountain Ben More (Шаблон:Lang-gd, meaning "great mountain") is the highest mountain and only Munro (mountains in Scotland that reach an elevation of at least Шаблон:Convert) on the Isle of Mull, Scotland. It is also the highest peak in the Scottish isles – and the only Munro – apart from those on the Isle of Skye. The mountain is situated close to the centre of the island, above the shores of Шаблон:Lang.

Access and climbing route

The peak is easiest reached from Loch na Keal, the walk up from the B8035 road following farm tracks, the side of a stream; Шаблон:Lang, and ultimately up scree slopes to the top. From the summit on a clear day, the view encompasses the Sound of Mull, Staffa, Ulva, the Ross of Mull and Iona in the distance. From sea loch to summit is approximately a four-hour walk.

The more demanding but rewarding route follows a boggy path up the banks of Шаблон:Lang to the Шаблон:Lang (mountain pass) between Шаблон:Lang ("The Breast") and Шаблон:Lang (not to be confused with its namesake in Kintail). From the Шаблон:Lang the route follows South West along a steep and rocky ridge first to the peak of Шаблон:Lang then on and up to Ben More itself. There is respite at the top in a circular refuge of stones. This route starts and ends on the B8035 road and is approximately a six-hour walk and scramble.

Climbers should be cautious when using a compass in misty conditions since there is magnetic rock in places, especially near the summit of the mountain.[1]

Geology

Around 60 million years ago, the region was volcanically active, with Ben More being the remnant of a volcano, and it was in this period that the famous rock formations of Staffa and the basaltic columns of "The Castles" on Ulva came into being.[2] The lava flows are known as the "Staffa Magma Type member" and can also be seen on Mull at Шаблон:Lang, Шаблон:Lang, and near Tobermory on its east coast. They are particularly rich in silica.[3]

See also

References

Шаблон:Reflist

External links

Шаблон:Commons category

Шаблон:Scottish Munros section 17 Шаблон:British hills Шаблон:Mull