Karoo Ice Age Karoo Ice Age The Karoo Ice Age, more commonly referred to as the Late Paleozoic Ice Age, from 360–260 million years ago (Mya) was the second major ice age of the Phanerozoic Eon. It is named after the tillite (Dwyka Group) found in the Karoo Basin of South Africa, where evidence for this ice age was first clearly identified in the 19th century. The tectonic assembly of the continents of Euramerica (later with the Uralian orogeny, into Laurasia) and Gondwana into Pangaea, in the Hercynian-Alleghany Orogeny, made a major continental land mass within the Antarctic region, and the closure of
Hydraulic fracturing in South Africa reserve in the world. These figures, however, were based on desktop research and would only be refined through an extensive exploration programme In the present day, the Karoo is a semi-desert stretching over 400,000 square kilometers and home to a population of around 1 million people. The Karoo is divided into two regions: the Little Karoo, which is wet, and the Great Karoo, which is mainly desert. Because of certain exclusions, including topography and townships, around 28% of the Karoo has been estimated to be accessible to commercial development. Unique to the Karoo shale reserves is the presence of dolerite