“Listen to the streams as they gurgle from their cradles
and you will hear the story of the mountains. You will hear fascinating tales
if only you listen! Lie next to a stream and listen to the song of the
mountains. The smiling faces of the flowers, dancing in the wind. Venture into
the remote valleys or stand on a peak at sunrise or sunset, after snow has fallen,
and you will hear a song that you will never forget - the Song of the High
Mountain".
DRAKENSBERG WILDERNESS PHOTOS ©
WILLEM PELSER
“IT HAD TO DO
WITH HOW IT FELT TO BE IN THE WILD. THE EXPERIENCE WAS POWERFUL AND
FUNDAMENTAL, AND AS LONG AS THE WILD EXIST IT WILL ALWAYS FEEL THIS WAY.”
UNKNOWN
THE DRAKENSBERG
The highest point on the Drakensberg is the incongruously named Ntaba
Ntlenyane (nice little mountain), which reaches a height of 3483 m. The
whole summit of the basalt island is a jumble of spongy, water-soaked bogs,
complex, zigzagging valleys, springs, waterfalls, streams, mist, snow and
clouds, all inextricably mixed into a gigantic scenic symphony perfectly
described by the greetings exchanged by the Sotho horsemen when they meet one
another on the bridle paths which seem to reach almost to the stars: ‘Khotso’
(peace); and ‘Pula’ (rain).
The most spectacular length of the Drakensberg
looks down on KZN, Griqualand East and the north-eastern portion of the Cape.
For 350 km the Drakensberg presents a high wall of basalt precipices. There are
no easy ways over this mass of rock. The few passes are steep, zigzag routes
following water-courses. Bridle paths, wilderness trails and tracks follow the
contours along the lower slopes, but it takes a mountaineer to find a way to
the summit of most of the peaks. In some areas mountain hotels and holiday
resorts have been established. Other areas remain completely wild and difficult
of access, and demand no little endurance from those with the energy to explore
them.
Snow can fall along the Drakensberg in any month of
the year, but winter usually sees the heaviest falls. The summer months are
marked by some of the noisiest and most spectacular thunderstorms occurring
anywhere on earth. From November to May these violent storms break in two days
out of three.
Clouds start to close in for the brawl at about 11
a.m. Preliminaries commence at about 1 p.m. with a few bangs and buffets. By 2
p.m. there is a general uproar. To a hiker caught in such a storm is something
like trying to shelter in a box of fireworks after somebody else has thrown in
a match. Tremendous flashes of lightning seem to tear the sky to pieces.
Thunder rumbles, explodes and echoes in an incessant uproar. Rain streaks down
at over 50 km an hour, usually turning into hail at some stage, with lumps the
size of pigeon’s eggs.
Even more abruptly than they started, these
mountain thunderstorms end. The clouds suddenly lift, there is a real flaming
sunset and by evening all the stars are out, quite dazzling in the well-washed,
pollution-free sky. Storms of longer duration, accompanied by days of clammy
mist, also set in at times and bring an average rainfall of 2000 mm, the water
soaking into the basalt and then oozing out to feed the rivers.
The vegetation on the slopes, a thick covering
of grass and a few shrubs, is sufficient hardy to be able to shrug off these
storms – not, however, without many scars. Slopes with a southern aspect – the coldest
slopes – are particularly marked by such storm scars. Bare, crescent-shaped
terraces pattern the slopes in the thousands. Each of these neat little
terraces is about 1 m wide and up to 10 m in length. They appear to be caused
mainly by melted water from snow and frost. This icy water saturates the soil,
causing it to sag and form these strange-looking scars, rather reminiscent of
the incisions made on the faces of certain primitive tribespeople.
The north-eastern end of the basalt ‘island’ is
fittingly marked by an outstanding, fang-shaped peak known as the Sentinel. It
is 3165 m high and a dominant landmark, visible from KZN and the Orange Free
State. Behind it lies a high, boggy plateau overlooked by a gently rising
height known as Mont-aux-Sources (the
mountain of springs), around whose slopes dozens of springs bubble up and
combine their clear waters to form several major rivers in South Africa flowing
east and west.
To the east, the plateau falls away in some of
the most majestic precipes of the whole Drakensberg.
The End.
No comments:
Post a Comment