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
Tadjourah Region road of the region, providing a circuitous, up and down route to the capital city compared to the sea route which is approximately a fifth of the distance. It also provides the only proper road of the region into Ethiopia. This is the largest forest in the country, a semi-arid surrounded by semi-desert, with four dominant species: "Juniperus procera", "Olea africana", "Buxus hildebrantii", and "Tarchonanthus camphoratus". Elevations play a major factor in temperature, with the escarpments and plateaus on average 11°C (52°F) cooler, day or night. The climate of the coastal strip is influenced by warm ocean waters, keeping the