Abstract:
English: The vegetation of the two kloofs in the Magaliesberg
range is described. These kloofs are 10 miles west of the
Hartebeespoortdam in die Brits district covering an area
of approximately 35 morgen. The altitude of the area
varies from 4200 to 5200 feet above sea level.
Geologically the region is situated within the Pretoria
Series of the Transvaal System and consists of Magaliesberg
Quartzites and Magaliesberg Shales.
The soils conform very closely to the geological
structure. They are residual and formed in situ. Owing
to the mountainous topography there has been alluvial
drift.
The average annual rainfall of the area is 696.7 mm.
measured at Wolhuterskop, of which 85% falls during the
summer months October to March. There is an indication that
the precipitation is higher at the top of the mountain than
at the base, and also higher on the south side of the
mountain than on the north side.
The temperatures of the north and south sides of
those.
the mountain as well as those of the slopes of the kloofs
are compared. Maximum temperatures are lower at the top
of the mountain than at the base while minimum temperatures
are higher at the top. Temperatures in general are
higher on the north side. The temperatures of the slopes
of the kloofs, receiving the greater insolation, are
higher than those of the opposite slopes.
The influence of biotic factors on the vegetation is
discussed. The vegetation is classified according to the method
described by Goodall (1953) into 16 groups. These 16
groups are described as belonging to the following six
communities:-
1. Mimusops-Chrysophyllum-community.
2. Rauvolfia-community.
3. Croton-community
4. Chrysophyllum-community
5. Acacia caffra-community
6. Acalypha glabrata-community.
The Mimuso-Chrysophyllum-community occupies most of
the west slope and small patches of the lower portion of the
east slope of the north kloof. The dominant trees are
Mimusops zeyheri and Chrysophyllum magalismontanum.
The Rauvolfia-community is confined to the streambanks
in the north kloof. This community is characterized
by the tropical element in the flora. Rauvolfia caffra is
the dominant tree, while species such as Trema guineenais,
Ilex mitis, Pygeum africanum_and Pittosporum viridiflorum
are present.
The east slope of the north kloof is occupied by the
Croton-community. This is a dry open community with Croton-
subgratissimus, Combretum zeyheri and Combretum holosericeum
being the dominant trees.
The Chrysophyllum-community covers the western slopes
of the kloof near the northern top of the mountain.
Chrysophyllum magalismontanum is the dominant tree. Trees
such as Cornbretum holosericeum and Ochna pulchra are important
constituents of the tree layer.
The Acacia caffra-community occupies the slopes of the
south kloof and small parts of the upper portion of the north kloof. This community is dominated by Acacia caffra.
In the parts of the north kloof where the Acacia caffracommunity
occurs, some of the associated species show an
affinity with the Bushveld flora. Species such as
Combretum zeyheri, Crysophyllum magalismontanum and Mimusops
zeyheri are found in this community. On the south side
the associated species are mostly widely distributed species,
such as Dombeya rotundifolia and Euclea,_lanceolata.
The Acalypha glabrata-community occupies the streambanks
of the south kloof. The dominant tree is Buddle salicifolia, a specie of the Kalahari Thornveld.
Calondendrum_capense and Celtis_africana, temperate forest
species, form on important consituent of the tree layer.
The vegetation of the north side of the range is
dominated by Bushveld species, but a number of tropical
forest species are present, e.g. Rauvolfia caffra, Pittosporum
viridiflorum, Pygeum africanum and Trema guineensis.
The vegetation of the south side of the mountain is dominated by widely distributed species, but there are
traces of temperate or transitional forest, with species
such as Celtis africana, Kiggelaria africana, Halleria
lucida, Leucosidea sericea, Buddleja salvifolia and
Cassinopsis ilicifolius.