text: Geography and geology The Matobo Hills are composed entirely of granite, making up the Matopos Batholith. The granite weathers into fantastic shapes, such as the balancing rocks known as Mother and Child Kopje. Between the granite mountains, narrow valleys form. These are often swampy valleys known as dambos or vleis, due to runoff from the whaleback mountains. These valleys form the headwaters of the Maleme, Mpopoma and Mtsheleli rivers, and the source of the Thuli River is just east of the park.
  Archaeological, historical and cultural sites
  San (Bushmen) lived in the hills about 2,000 years ago, leaving a rich heritage in hundreds of rock paintings. There are over 3,000 registered rock art sites, with the main periods of painting being between 320 and 500 C.E.. In the many crevices and caves, clay ovens and other historic artefacts have been found, and various archaeological finds date back as far as the Pre-Middle Stone Age, around 300,000 B.P. The following major sites have been developed for tourist access:
  Bambata Cave is a major archaeological site, located in the west of the national park, north of the game park on the Kezi-Bulawayo road. The frieze includes elephants, giraffes, warthogs, tsessebe and mongoose.
  Inanke Cave has the most extensive paintings, located in a remote cave accessible by a three-hour hike from Toghwana Dam. Along the route of the hike is an Iron Age furnace.