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Barberton is a town in the Mpumalanga province of South Africa, which has its origin in the 1880s gold rush in the region. It is situated in the De Kaap Valley and is fringed by the Makhonjwa Mountains. It is 43 kilometres (27 mi) south of Mbombela and 360 kilometres (220 mi) east of Johannesburg.
Location of the Barberton Greenstone Belt. The Barberton Greenstone Belt is a geologic formation situated on the eastern edge of the Kaapvaal Craton in South Africa.It is known for its gold mineralisation and for its komatiites, an unusual type of ultramafic volcanic rock named after the Komati River that flows through the belt.
The Makhonjwa Mountains or Barberton Makhonjwa Mountains are a range of small mountains and hills that covers an area of 120 by 60 kilometres (75 by 37 mi), about 80% in Mpumalanga, a province of South Africa, and the remainder in neighbouring Eswatini. [2] It constitutes 40% of the Barberton Greenstone Belt. [3]
English: This is a simplified geologic map of the Barberton Greenstone belt, South Africa, showing three of the major Groups and their interactions as well as the Kaap Valley Craton. Date 10 October 2013, 15:38:59
The R40 is a provincial route in South Africa that connects the Eswatini border at Bulembu via Barberton, Mbombela, Bushbuckridge, Acornhoek and Hoedspruit with Phalaborwa. The route spans two provinces and passes through several private game reserves. [1]
[2]: 30 The R38 joins the R40 and they are one road south-east for 7 kilometres (Dikbas Avenue), bypassing Emjindini, up to a junction with Sheba Road north of the town centre of Barberton. [2]: 31 At this junction, the R40 remains on Dikbas Avenue while the R38 becomes the road northwards (Sheba Road).
Sheba is a rural settlement northeast of Barberton in the Mpumalanga province of South Africa. It is situated in the De Kaap Valley and is fringed by the Makhonjwa Mountains. It is 35 kilometres (22 mi) south of Nelspruit and 360 kilometres (220 mi) to the east of Johannesburg.
The Barberton Greenstone Belt is located on the Kaapvaal craton, which covers much of the southeastern part of Africa, and was formed by the emplacement of granitoid batholiths. [7] The Kaapvaal craton was once part of a supercontinent geologists term Vaalbara that also included the Pilbara craton of western Australia. [ 7 ]