Vanuatu Geohazards Observatory (VGO) reported that observations of Aoba’s Lake Voui on 22 and 29 November confirmed that activity had declined, characterized by less frequent explosions, steam emissions, and decreased seismicity. On 7 December the Alert level was reduced to 2 (on a scale of 0-5) and residents and tourists were reminded to stay outside of the Danger Zone defined as a 2-km radius around the active vent in Lake Voui.

Geological Summary. The island of Ambae, also known as Aoba, is a massive 2,500 km3 basaltic shield that is the most voluminous volcano of the New Hebrides archipelago. A pronounced NE-SW-trending rift zone with numerous scoria cones gives the 16 x 38 km island an elongated form. A broad pyroclastic cone containing three crater lakes (Manaro Ngoru, Voui, and Manaro Lakua) is located at the summit within the youngest of at least two nested calderas, the largest of which is 6 km in diameter. That large central edifice is also called Manaro Voui or Lombenben volcano. Post-caldera explosive eruptions formed the summit craters about 360 years ago. A tuff cone was constructed within Lake Voui (or Vui) about 60 years later. The latest known flank eruption, about 300 years ago, destroyed the population of the Nduindui area near the western coast.

Source: Vanuatu Meteorology and Geohazards Department (VMGD)