Between the Sunset and the Sea: A View of 16 British Mountains. Simon Ingram. Читать онлайн. Newlib. NEWLIB.NET

Автор: Simon Ingram
Издательство: HarperCollins
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Жанр произведения: Природа и животные
Год издания: 0
isbn: 9780007547890
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heap of native rocks, one the shape of an incisor tooth poking out of the top to the height of my shoulder. Within that cairn – somewhere around the height of my hip – was the 3,000-foot contour line.

      And herewith lies the great irony of Beinn Dearg, and the third reason I’d chosen to climb this mountain above all others hereabouts. Beinn Dearg is considered the least noteworthy of Torridon’s central quartet of mountains, not for lacking challenge, nor spectacle, nor location: it has all of these in plenty. Despite being the nucleus of the area that contains Liathach, Beinn Eighe and Beinn Alligin, the mountain is ignored by the bulk of human traffic because it’s 30 inches too short. Thirty inches: that’s the distance between the sole of my boot and the middle of my thigh. You cannot imagine how spectacularly, how ridiculously insignificant that is in mountain terms. A 3,000-foot mountain is 36,000 inches high; 30 inches represents 0.08 per cent of its total height. On a 6-foot person, that’s the equivalent of cutting just under two millimetres of hair from the very top of their head, then dismissing them for being inconsequentially small. The reason for this is that 3,000 feet is quite an important measurement for a mountain in Scotland; it’s the height at which a mountain becomes a Munro.

      There are, at the time of writing, 282 Munros in Scotland. I say ‘at the time of writing’ – new mountains don’t appear or disappear at a rate necessary to be monitored by hillwalkers, after all – because nobody can really decide what actually constitutes a Munro. The original list was compiled by a London-born, Scottish-raised baronet, Sir Hugh Munro, as a way of categorising the hills of his familial homeland into some sort of quantifiable system. It was published in 1891, and surprised most by its sheer length; most people thought Scotland harboured a mere handful of mountains over 3,000 feet, so the whole thing was a splendid surprise.

      But despite being thorough, Munro wasn’t particularly specific. His Tables reflected what he considered ‘separate mountains above 3,000 feet’, but he neglected to define what constituted ‘separate,’ and this is of course unsatisfactory for today’s levels of numerical scrutiny. Alas, much quarrelling continues about which peaks should and shouldn’t be on the list, and it all gets terribly complicated. The debates on the matter are filled with terms such as ‘overall drop’, ‘relative height’ and ‘subsidiary tops’, which all broadly circle around the fact that nowhere did Munro give a specific figure for how tall a summit had to be in relation to the one next to it to qualify it as a separate mountain – and therefore a true Munro.

      As of May 2013, some 5,000 people have completed all of the Munros, some of them having done so twice, a few without stopping. That’s an awesome achievement. Superhuman, even.

      Yet how many of those people looked up at Beinn Dearg, saw it, and thought: ‘Wow! But not on my list,’ before shuffling on?

      It’s all a lot of fun and certainly makes a pleasingly functional answer to the perennial question ‘Why climb a mountain’ (Answer: ‘I’ve got them written down on this piece of paper, so I have to’). And whatever legacy Hugh Munro left when he died of influenza in 1919 – presumably without someone sitting anxiously at his bedside imploring him to write a number, any number, down on this piece of paper before you go, old chap, because one day this could be important – you have to admire his style. Other than that 3,000-foot criterion, Munro went on instinct rather than anything more mathematical; it was simply a question of how grand a summit felt. And at its core this all brings us back to the argument of what is and what isn’t a mountain. It really doesn’t matter. If it feels like a mountain, then it is one.

      I didn’t have time to do the Munros, even if I wanted to. I certainly couldn’t do all the Corbetts, or even the Wainwrights. I admired and envied the experiences of all those who did, but I couldn’t invest the precious time I had to spend in the mountains to one geographical area, and certainly not to the same narrow band of the vertical scale.

      Stand on Beinn Dearg’s summit, make a little indentation in your thigh, and take a moment to consider your context – there’s the Atlantic, there’s the river, wriggling along far below, and here you are, alone amongst it – and you’ll realise how little numbers matter when it comes to climbing mountains. Beinn Dearg is a mountain: each and every one of its 35,970 inches builds towards a top of such elevated spectacle, you’d be mad to discount it on any basis, let alone it not making the coveted slate of a man whose life occupied but a flash of its own existence.

      I looked at my watch. Six p.m. It had taken far more time than I’d thought to reach the summit and darkness would soon start falling. Cloud was beginning to mither the higher tops, and was creeping up the gullies and valleys around me. Walking out would take hours. Time I got down.

      Taking a last look around, I walked south from the summit cairn, intending to follow Beinn Dearg’s skyline as it curved around to the east, then find a comely slope to descend into the valley once the mountain had surrendered most of its height.

      Ahead of me, the edge of the summit appeared as a hard line against the sky, like the side of a flat roof or the end of a diving board. I wasn’t alarmed: the convex slopes that built these mountains meant that easy terrain beyond – a broad series of rock steps, or a thin path negotiating a steep slope – would emerge as I got closer.

      Only it didn’t. I reached the edge of the summit plateau and froze. For the first time I saw the descent route, and it was a shock. Ahead of me and below was a thin sail of brown, bitten rock. Curved slightly, its outside edge was completely vertical in its fall to the valley floor, whilst the right side – now filling with rising cloud – had a steeply tilting grassy ledge across which a thin path beetled. Beneath that, a crag, then a drop of similar horror. From the top of the mountain down to the first bit of buttress-cut slope was probably in the order of 500 metres. That was the only way the mountain went. I’d two choices: climb the crest on good rock but over big exposure, or traverse the grassy ledge and pray it wasn’t slippery. My company on both of these options would be open intimacy with a drop as high and as vertical as the Empire State Building. I didn’t remember this! And this wasn’t even the most pressing problem.

      At my feet – far from an easy toddle down a few amenably angled rocks – was a vertical step of about three metres. Its bottom was a little platform of rock, on either side of which the mountain fell away with fatal steepness. To get to it required a down-climb as if on a very steeply raked ladder, only with tilted footholds of wet rock instead of rungs, with no guarantees of integrity and no margin for error at the bottom. Piece of cake.

      Descents like this are what fatal-accident statistics are made of. Coming down mountains claims more people