Available Weekly Reports
| Burney, Monte |

There are no activity reports for Burney, Monte.
Summary of eruption dates and Volcanic Explosivity Indices (VEI).
| Start Date | Stop Date | Eruption Certainty | VEI | Evidence | Activity Area or Unit |
|---|---|---|---|---|---|
| 1910 Mar | Unknown | Confirmed | 2 | Historical | |
| 90 BCE ± 100 years | Unknown | Confirmed | Radiocarbon (corrected) | ||
| 800 BCE ± 500 years | Unknown | Confirmed | Tephrochronology | ||
| 2320 BCE ± 100 years | Unknown | Confirmed | 5 | Radiocarbon (corrected) | MB2 tephra |
| 3740 BCE ± 10 years | Unknown | Confirmed | Radiocarbon (corrected) | ||
| 7390 BCE ± 200 years | Unknown | Confirmed | Tephrochronology | ||
| 7450 BCE ± 500 years | Unknown | Confirmed | 5 | Radiocarbon (corrected) | MB1 tephra |
Monte Burney, a large volcano in the Patagonian region of Chile, is the southernmost of a chain of stratovolcanoes of the Australandean arc. The 1758-m-high, ice-covered volcano lies about 200 km NW of the town of Punta Arenas. Monte Burney was constructed on the western rim of a 6-km-wide caldera, which is partially filled with and surrounded by an unglaciated pyroclastic-flow deposit. Flank vents produced andesitic-dacitic lava flows and pyroclastic material. Collapse of the edifice produced a major debris avalanche that traveled to the SSW. Two large plinian eruptions have been documented from Monte Burney during the Holocene. The only known historical eruption of Monte Burney took place in 1910.