PVMBG reported that at 0747 on 14 January an eruption at Lewotolok produced a white-and-gray ash plume that rose around 400 m above the summit and drifted E. At 2055 on 16 January a white-and-gray ash plume of variable density rose around 400 m above the summit and drifted SE. A photo posted with the report showed incandescence emanating from the summit, possibly from ejected material. The Alert Level remained at 2 (on a scale of 1-4) and the public was warned to stay 2 km away from the summit crater.

Geological Summary. The Lewotolok (or Lewotolo) stratovolcano occupies the eastern end of an elongated peninsula extending north into the Flores Sea, connected to Lembata (formerly Lomblen) Island by a narrow isthmus. It is symmetrical when viewed from the north and east. A small cone with a 130-m-wide crater constructed at the SE side of a larger crater forms the volcano's high point. Many lava flows have reached the coastline. Eruptions recorded since 1660 have consisted of explosive activity from the summit crater.

Source: Pusat Vulkanologi dan Mitigasi Bencana Geologi (PVMBG, also known as CVGHM)