Geography of South Africa ore from the interior. South Africa is largely a dry country, with most of its western regions being semi-desert. The rainfall increases in the east, (the Highveld, KwaZulu-Natal, and the Eastern Midlands), and falls primarily in summer. The narrow southern coastal strip receives all-year rainfall in the east (the Garden Route), and winter rainfall in the west (on the Cape Peninsula and its surrounds). The summers are warm to hot, while the winter temperatures can vary, depending on locality from bitterly cold to cool. Thus the Karoo, which occupies a large part of the western Central Plateau, has a climate
Kazakh semi-desert in livestock numbers in Kazakhstan is allowing the native plants a greater opportunity to regenerate. The Kazakh semi-desert is an ecotone between the Kazakh Steppe to the north and the Central Asian northern desert to the south, running in a band across central Kazakhstan. The climate here is semi-arid and highly continental. Precipitation averages between and annually. Mean temperatures in January range from and , while July means are between and . Annual average temperatures are around . The region's topography consists of vast, flat plains and salt flats broken by dissected plateaus (known locally as ""melkosopochniki""). As a transition