Twenty-Five Years in a Waggon in South Africa: Sport and Travel in South AfricaAnderson, Andrew A.
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Twenty-Five Years in a Waggon in South Africa: Sport and Travel in South Africa
Anderson, Andrew A.
Africa, Southern -- Description and travel; Anderson, Andrew A. -- Travel -- Africa, Southern
I also shot one of those beautiful blue jays,
as there were many in this district.
I pass over my shooting exploits, as there is nothing worth recording,
each daily trek being almost a repetition of the last, until we arrive
in sight of Wakkerstroom, a poor village, a few houses, flat roofs,
single floors, built in an open country near a lofty hill, which stands
on the main road from Natal to Lydenburg; we remained only a few days,
then went north, as far as Lake Crissie, an open piece of water, no
trees or bushes near; a solitary sea-cow is the only occupant of this
dismal-looking place. In this district the Vaal river rises, and many
small branches meet, until the veritable river is formed. The elevation
at the lake was 5613 feet, and on a hill a few miles north I found the
altitude above sea-level to be 6110 feet, an open grass undulating
country as far as the eye could see, except on the east, where the
mountain range that forms the Quathlamba is seen in the distance. I
retraced part of the road, and turned south-east, over the hills leading
to where Lunenburg now stands, and on towards Swaziland, which is an
independent native territory, thickly populated and very mountainous;
there are rich gold-mines there now, and some of the mountains attain an
altitude of 8000 feet.
The greater part of the summer months, a mist envelops the hills, but it
is a very healthy part of Africa, and horse sickness is rarely known to
exist, consequently many horses are bred here. Passing Kruger's post,
through Buffel forest, which is hilly, and splendid timber trees cover
the entire country, the scenery is grand and wild; quartz reefs crop out
in all directions, sandstone, shale, and in some places limestone
overlap the granite formation, which compose these lofty ridges of the
Drakensberg; shale, which indicates the existence of coal, is frequently
seen in the valleys, and along the Pongola river and its several
branches.
I left Harrysmith on the 20th September, 1863, arriving on the banks of
the Pongola river on the 16th October. In that time I had treked 350
miles, being delayed on the road shooting and exploring.
Public-domain text, read in full here on John Shaqi.
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