The Ultimate Guide to the Munros Vol 1 by Ralph Storer sampler
From the pen of a dedicated Munro bagger comes The Ultimate Guide to everything you've wished the other books had told you before you set off. The lowdown on the state of the path, advice on avoiding bogs and tricky situations, tips on how to determine which bump is actually the summit in misty weather... this is the only guide to the Munros you'll ever need.
From the pen of a dedicated Munro bagger comes The Ultimate Guide to everything you've wished the other books had told you before you set off. The lowdown on the state of the path, advice on avoiding bogs and tricky situations, tips on how to determine which bump is actually the summit in misty weather... this is the only guide to the Munros you'll ever need.
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xvii<br />
THE SOUTHERN HIGHLANDS<br />
he region covered <strong>by</strong> this<br />
T guidebook, as its name implies,<br />
is <strong>the</strong> most sou<strong>the</strong>rly region in <strong>the</strong><br />
Scottish Highlands. It is bounded on<br />
<strong>the</strong> west <strong>by</strong> <strong>the</strong> sea, on <strong>the</strong> east <strong>by</strong><br />
<strong>the</strong> Tay Valley (<strong>the</strong> A9 Perth –<br />
Pitlochry road) and on <strong>the</strong> north <strong>by</strong><br />
a line that runs along <strong>the</strong> A85 from<br />
Oban <strong>to</strong> Tyndrum, up <strong>the</strong> A82 <strong>to</strong><br />
Rannoch Moor, <strong>the</strong>n eastwards along<br />
Loch Rannoch and Loch Tummel <strong>to</strong><br />
Pitlochry. In <strong>the</strong> south it is bounded<br />
<strong>by</strong> <strong>the</strong> central belt of Scotland<br />
between Glasgow and Edinburgh,<br />
below which <strong>the</strong> Sou<strong>the</strong>rn Uplands<br />
continue <strong>to</strong> <strong>the</strong> English border.<br />
<strong>The</strong> region itself is divided in<strong>to</strong> two<br />
distinct halves <strong>by</strong> a geological zone<br />
of fracture known as <strong>the</strong> Highland<br />
Boundary Fault, which runs in a<br />
straight line across <strong>the</strong> breadth of<br />
Scotland from south-west <strong>to</strong> nor<strong>the</strong>ast.<br />
From <strong>the</strong> west coast it crosses<br />
Loch Lomond at Balmaha, passes<br />
through <strong>the</strong> Trossachs at Aberfoyle<br />
and heads north-east through Glen<br />
Artney <strong>to</strong> <strong>the</strong> Tay Valley and beyond,<br />
eventually <strong>to</strong> reach <strong>the</strong> east coast<br />
at S<strong>to</strong>nehaven.<br />
Although <strong>the</strong> fault is hundreds of<br />
millions of years old, tremors are still<br />
felt along it as <strong>the</strong> rocks continue <strong>to</strong><br />
settle, making <strong>the</strong> <strong>to</strong>wn of Crieff <strong>the</strong><br />
earthquake capital of <strong>the</strong> British Isles.<br />
South of <strong>the</strong> Highland Boundary<br />
Fault lie green rounded hills, while<br />
north of it lie rougher mountains,<br />
including all <strong>the</strong> region’s 46 <strong>Munros</strong><br />
and accompanying 21 Tops, <strong>to</strong> say<br />
nothing of 36 Corbetts. <strong>The</strong> rocks are<br />
mostly sedimentary but <strong>the</strong>y have<br />
been greatly metamorphosed, uplifted<br />
and folded over time. Rolling folds<br />
parallel <strong>to</strong> <strong>the</strong> Highland Boundary Fault<br />
have rippled <strong>the</strong> land in<strong>to</strong> Munroheight<br />
mountains separated <strong>by</strong> deep<br />
depressions, of which <strong>the</strong> largest is<br />
<strong>the</strong> great strath that runs from<br />
Crianlarich through Glen Dochart <strong>to</strong><br />
Killin, <strong>the</strong>n along Loch Tay <strong>to</strong><br />
Aberfeldy and Pitlochry.<br />
Although <strong>the</strong> ground <strong>to</strong> <strong>the</strong> north<br />
of <strong>the</strong> fault is rougher than that <strong>to</strong> <strong>the</strong><br />
south, it is nowhere near as rugged<br />
as fur<strong>the</strong>r north and west in <strong>the</strong><br />
Highlands, while <strong>the</strong> igneous<br />
Cairngorm plateaus <strong>to</strong> <strong>the</strong> east are<br />
different again. <strong>The</strong> Sou<strong>the</strong>rn Highland<br />
landscape is more gentle, more<br />
rounded and more verdant, though<br />
with enough geological variation and<br />
Ice Age sculpting <strong>to</strong> include an<br />
occasional rock playground for<br />
climbers and scramblers. Examples<br />
include <strong>the</strong> overhanging rock faces of<br />
<strong>The</strong> Cobbler, <strong>the</strong> great Prow of Stuc a’<br />
Chroin and <strong>the</strong> craggy corries of <strong>the</strong><br />
Bridge of Orchy mountains.<br />
Apart from some notable<br />
exceptions, <strong>the</strong> <strong>Munros</strong> cluster in<br />
groups separated <strong>by</strong> lochs and deep<br />
glens, which carry an extensive road<br />
system that eases access. Within each<br />
group <strong>the</strong> <strong>Munros</strong> are often close<br />
enough <strong>to</strong>ge<strong>the</strong>r <strong>to</strong> make multibagging<br />
trips practicable. <strong>The</strong> region<br />
<strong>the</strong>refore has <strong>the</strong> best of both worlds.<br />
Its <strong>Munros</strong> are easily accessible