MAPPING GEOLOGICAL FAULT STRUCTURES IN THE CAPE FOLD BELT
MOUNTAINS – A CARTOGRAPHIC APPROACH
G. Brunsdon, P.W.K. Booth
Nelson Mandela Metropolitan University, Geosciences
Departmant, Port Elizabeth, South Africa
gideon.brunsdon@nmmu.ac.za
Rocks of
the Palaeozoic Cape Fold Belt cover the southern tip of Africa and are known as
the Cape Supergroup. These Cape Fold
Belt rocks were deposited between 520 – 340 million years ago and have been
extensively faulted and folded due to compression forces between 280 – 215
million years ago, directed from the present day south to the north.
To gain a better understanding of where these
compression forces came from and what caused them, a great emphasis has been
placed on studying and understanding the structure of these rocks. In general it has been found that rock layers
of the Cape Fold Belt strike in a more or less east to west direction, with
individual layers either dipping to the north or the south, depending on fold
structure. Many thrust faults have been
described that have a more or less a similar trend, but most of these faults
dip in a south-south-westerly direction.
Normal faults strike in an east to west direction in general, but mostly
are of a more recent deformation age and therefore usually occur after the
thrust faulting. Strike-slip faults are
sometimes associated with the normal faults, but strike in a north to south
direction.
These structural trends are clearly visible on
Landsat ETM imagery and visual interpretation of individual Landsat bands gives
one an overall bird’s eye view of a large area, which enables one to see the
continuation of these structures which is not possible when using aerial
photographs. Individual hills and
mountain ridges can be traced showing the general east-west striking trends,
whereas river valleys often truncate the mountainous areas in a north-south
direction along pre-existing strike-slip faults, in an uniformly spaced
parallel pattern.
The mapped geology and structural data allows
for further interpretation when it is combined and draped over a digital
terrain model (DEM). The geological structure of the mountain ranges with large
scale overturned folds, creating ridges and valleys within the mountain range,
becomes clearly visible.
Including GIS and Remote Sensing into a
geological study, greatly aids and enhances the interpretation and analysis of
data, and it creates enhanced visualisation and cartographic output, especially
with the use of three dimensional modelling.
To do this properly one needs to understand and apply many cartographic
principles, but the knowledge of cartography is often lacking or ignored when
geological mapping is done.