Malta are uninhabited. The islands of the archipelago lie on the Malta plateau, a shallow shelf formed from the high points of a land bridge between Sicily and North Africa that became isolated as sea levels rose after the last Ice Age. The archipelago is therefore situated in the zone between the Eurasian and African tectonic plates. Malta was considered an island of North Africa for centuries. Numerous bays along the indented coastline of the islands provide good harbours. The landscape consists of low hills with terraced fields. The highest point in Malta is Ta' Dmejrek, at , near Dingli. Although
Climate of Malta Climate of Malta Malta has a Mediterranean climate according to the Köppen climate classification ("Csa"), with very mild winters and warm to hot summers. Rain occurs mainly in winter, with summer being generally dry. According to the Troll-Paffen climate classification and the Siegmund/Frankenberg climate classification, Malta lies within the subtropical zone, being at 35ºN latitude. The average yearly temperature is around during the day and at night (one of the warmest temperature averages in Europe). In the coldest month – January – the typical maximum temperature ranges from during the day and the minimum from at night. In the warmest