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The rains are almost entirely limited to summer downpours between December and March, which also mark the season for plowing and planting.
Cyclic droughts, often lasting up to five or six years in every two decades, can limit or eliminate harvests and reduce livestock to starvation.
Geologic exploration has been limited by the depth and extent of Kalahari sand covering the surface geology.
The rock groups underlying most of the sandveld are therefore the least-known but appear to be the youngest, belonging to the , formed 290 to 208 million years ago.
In summer, which lasts from October to March, temperatures rise to about 93 °F (34 °C) in the extreme north and southwest, the warmest parts of the country.
In winter, which lasts from April to September, there is frequent frost at night, and temperatures may fall to near freezing in some high-altitude areas during the day.
The Kalahari sandveld has often been called “thirstland” to distinguish it from true desert.
The Molopo River and its Ramatlhabama tributary, on the southern border of Botswana with a course flowing into the Orange River, today rarely flood more than 50 miles (80 km) from their sources.
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The territory is roughly triangular—approximately 600 miles (965 km) from north to south and 600 miles from east to west—with its eastern side protruding into a sharp point.
Croton and Combretum tree savanna is found on the rocky hills of the eastern hardveld.
Acacia tree savanna merges northward into mopane (African ironwood) savanna woodland.
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The country is divided into three main environmental regions.