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To the east it is bordered by the Limpopo River and its tributaries, the Ngotwane (Notwani), Marico (Madikwe), and Shashe.
Elsewhere, Precambrian rock formations predominate. The surface geology of the eastern hardveld, exposed in its hill ranges, largely consists of basement complex rocks (more than 2.5 billion years old) intruding from northern South Africa and southern Zimbabwe.
This complex is known to extend into younger rock formations (2.5 to 1.2 billion years old) in the extreme southern sandveld, while rocks of the Ghanzi and Damara groups (1.2 billion to 570 million years old) extend across the northwest corner of the country into northern Namibia.
The country is divided into three main environmental regions.
The hardveld region consists of rocky hill ranges and areas of shallow sand cover in eastern Botswana.