Mount Erebus
Erebus
Stratovolcano · Antarctica · 3794m

- Type
- Stratovolcano
- Country
- Antarctica
- Region
- Antarctic-Scotia Volcanic Regions / McMurdo Volcanic Province
- Elevation
- 3794m
- Coordinates
- -77.530, 167.170
- Last eruption
- 2026
- Tectonic setting
- Intraplate / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Phonolite
Geological summary
Mount Erebus overlooks the McMurdo research station on Ross Island and is the largest of three major volcanoes forming the roughly triangular Ross Island. The summit of the dominantly phonolitic volcano has been modified by one or two generations of caldera formation. A summit plateau at about 3,200 m elevation marks the rim of the youngest caldera, which formed during the late-Pleistocene and within which the modern cone was constructed. An elliptical 500 x 600 m, 110-m-deep crater truncates the summit and contains an active lava lake within a 250-m-wide, 100-m-deep inner crater; other lava lakes are sometimes present. The glacier-covered volcano was erupting when first sighted by Captain James Ross in 1841. A persistent lava-lake, with minor explosions punctuated by occasional larger Strombolian explosions that eject bombs onto the crater rim, has been documented since 1972, but nearly continuous activity has probably been occurring for much longer.
From Wikipedia
Mount Erebus is the southernmost active volcano on Earth, located on Ross Island in the Ross Dependency in Antarctica. With a summit elevation of 3,792 metres (12,441 ft), it is the second most prominent mountain in Antarctica and the second-highest volcano in Antarctica. It is the highest point on Ross Island, which is also home to three inactive volcanoes: Mount Terror, Mount Bird, and Mount Terra Nova. It makes Ross Island the sixth-highest island on Earth by highest point.
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Eruption history
Detailed timeline
- 1972VEI 1Observed1972-01-03 – Ongoing
- 1972VEI 2Observed1972-12-16 – 2026-03-17
- 1963VEI 0Observed1963-11-16 – Ongoing
- 1957VEI ?Geological estimate1957-07-02 – 1958-07-02
- 1955VEI 2Observed1955-07-02 – Ongoing
- 1947VEI 2Observed1947-02 – Ongoing
- 1915VEI 2Observed1915-03-22 – Ongoing
- 1915VEI 2Observed1915-08 – Ongoing
- 1912VEI 2Observed1912-12-12 – Ongoing
- 1911VEI 2Observed1911-04 – 1911-06
- 1911VEI 2Observed1911-10 – Ongoing
- 1908VEI 2Observed1908-03 – 1908-11
- 1903VEI 0Observed1903-01-01 – Ongoing
- 1900VEI 2Geological estimate1900-02 – Ongoing
- 1841VEI 1Observed1841-01-28 – 1841-02
- 950 (±4000 yrs)VEI 0Geological estimate950 – Ongoing
- 2050 BCE (±3000 yrs)VEI 0Geological estimateBCE 2050 – OngoingWestern Crater (Upper Ice Tower flow)
- 2950 BCE (±300 yrs)VEI 0Geological estimateBCE 2950 – OngoingNorth flank (Lower Hut lava flow)
- 4050 BCE (±500 yrs)VEI 0Geological estimateBCE 4050 – OngoingLower Ice Tower Ridge, S lava flows
- 4550 BCE (±500 yrs)VEI 0Geological estimateBCE 4550 – OngoingNE flank
- 7050 BCE (±2000 yrs)VEI 0Geological estimateBCE 7050 – OngoingNW flank
- 8050 BCE (±5000 yrs)VEI 0Geological estimateBCE 8050 – OngoingNNW flank
External links
⚠ For reference only. Not for emergency response.