Mount Melbourne is a ice-covered stratovolcano in Victoria Land, Antarctica, between Wood Bay and Terra Nova Bay. It is an elongated mountain with a summit caldera filled with ice with numerous parasitic vents; a volcanic field surrounds the edifice. Mount Melbourne has a volume of about and consists of tephra deposits and lava flows; tephra deposits are also found encased within ice and have been used to date the last eruption of Mount Melbourne to . The volcano is fumarolically active. The volcano is part of the McMurdo Volcanic Group, and together with The Pleiades, Mount Overlord, Mount Rittmann and the Malta Plateau forms a subprovince, the Melbourne volcanic province. The volcanism is related both to the West Antarctic Rift and to local tectonic structures such as faults and grabens. Mount Melbourne has mainly erupted trachyandesite and trachyte, which formed within a magma chamber; basaltic rocks are less common. Geothermal heat flow on Mount Melbourne has created a unique ecosystem formed by mosses and liverworts that grow between fumaroles, ice towers, and ice hummocks. This type of vegetation is found at other volcanoes of Antarctica and develops when volcanic heat generates meltwater from snow and ice, thus allowing plants to grow in the cold Antarctic environment. These mosses are particularly common in a protected area known as Cryptogam Ridge within and south of the summit caldera. Description Mount Melbourne lies in North Victoria Land, facing Wood Bay of the Ross Sea. To the southeast lies Cape Washington and due south lies Terra Nova Bay; Campbell Glacier runs west from the volcano and Tinker Glacier lies north of the volcanic field. The seasonal Italian Mario Zucchelli Station lies from the volcano; the 5th Chinese station in Antarctica (due to be completed in 2022), the Korean Jang Bogo Station, the German Gondwana Station and a neutrino detector are also in the area. Mount Melbourne was discovered and first recognized as a volcano by James Ross in 1841 and named after William Lamb, 2nd Viscount Melbourne, who was then the prime minister of the United Kingdom. The volcano and its surroundings were investigated by New Zealand-based parties in the 1960s, by German ones in the 1970s and 1980s and by Italian-based parties in the 1980s and 1990s. The volcano and its summit can be accessed from the stations by helicopter. Volcano Mount Melbourne is an elongated stratovolcano formed by lava flows and tephra