Lava lakes occur in a variety of volcanic systems, ranging from the basaltic Erta Ale lake in Ethiopia and the basaltic andesite volcano of Villarrica, Chile, to the unique phonolitic lava lake at Mt. Erebus, Antarctica.Lava lakes have been observed to exhibit a range of behaviours. A "constantly circulating, apparently steady-state" lava lake was observed during the 1969-1971 Mauna Ulu.. This active lava lake was drained by the vigorous eruption at the lower East Rift Zone that ended the long-lasting summit eruption, and caused collapse and subsidence in the summit caldera. Halema'uma'u has also hosted active lava lakes during short eruptions during 1967-1968, 1952, the early 1930s, and the 1920s..
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A lava lake represents a latent threat for the populations living nearby, as it can drain suddenly through fissures and generate dangerously fast lava flows.. based on this diagram, families of lava lakes and a common trend associated with the formation and maturation of the three new lava lakes that have appeared over the last 2 decades. We.. Basalt lava is more fluid (less viscous) than andesite lava and a single flow can cover an area up to >300 km 2 (115 mi 2). Due to greater viscosity, andesite and basaltic andesite lava flows are typically limited in length to less than 12 km (7.5 mi) and cover areas less than 25 km 2 (9.6 mi 2.