Impressions in rock, with a resemblance to hominid foot- and
animal hoof-prints, have been discovered on the western
slope of the Usambara Mountains in north-eastern Tanzania.
The initial interpretation was that these were ancient trace
fossils similar to the tracts made in freshly deposited
volcanic ash, some 3 million years ago at Laetoli in the
Olduvai Gorge, by a passing group of early Australopithecine
hominids.
Unfortunately, no volcanic or fossil-bearing sediments occur
in the Usambara’s. The mountains are formed by feldspathic
gneisses and granulite of Precambrian age in the Usagaran,
arm of the northerly trending Mozambique Mobile Belt. The
Usambara Plateau, which is a Late Creatceous / Lower
Tertiary land surface, is covered by red-brown lateritic
soils and clays and, in the vicinities of Mabughai and
Magamba, developments of bauxite. The impressions, which are
a weathering phenomenon, are developed in highly
metamorphosed biotite-rich feldspathic gneisses cut by small
quartz-rich pegmatites.
However, although only a freak of nature, the
‘pseudo-footprints’ near Mambo View Point give an excellent
impression of what ancient hominid and animal tracts look
like and, combined with the breath taking views of the
northern Usambara escarpment and surrounding plains,
are well worth visiting.