: Mt. Eruption (As of 14 February 2014)

Kelud (Kelut) is a volcano located in East . Kelud is known for large explosive eruptions throughout its history. Following the increase of Mt. Kelud activity for the past few days, the PVMBG increased its alert status to level 4 on 13 February. The mount erupted on 13 February at 22.50 and 23.30.

SEMARANG WEST JAVA CENTRAL JAVA

SEMARANG TEMANGGUNG WONOSOBO GARUT MAGELANG BOYOLALI NGAWI TASIKMALAYA CIAMIS MAGELANG CILACAP MADIUN KEBUMEN PURWOREJO SLEMAN KLATEN SUKOHARJO MAGETAN

KULON PROGO KOTA KEDIRI BANTUL WONOGIRI PONOROGO ! GUNUNG KIDUL DI YOGYAKARTA PACITAN TULUNGAGUNG BLITAR TRENGGALEK MALANG

A ected by volcano ash fall

The boundaries and names shown and the designations used on this map do not imply official endorsement or acceptance by the United Nations

Creation date: 14 February 2014 BANGKALAN Sources: OCHA, BNPB, BPS, PVMBG and BIG www.indonesia.humanitarianresponse.info www.unocha.org www.reliefweb.int

LAMONGAN SURABAYA GRESIK BOJONEGORO

NGAWI SIDOARJO

JOMBANG MOJOKERTO MADIUN NGANJUK HIGHLIGHTS

PASURUAN

KOTA KEDIRI KEDIRI BATU 3 Casualties PONOROGO

! 5 Km

10 Km KOTA MALANG 76,388 IDPs in Kediri, Blitar, Malang, Tulungagung districts and Batu . TRENGGALEK KOTA BLITAR TULUNGAGUNG BLITAR LUMAJANG East Java Governor declared an emergency situation untill 12 March 2014 Governor of Yogyakarta declared an emergency situation untill 20 February 2014 MALANG

Legend

! Mt. Kelud In million 5 Km Hazard Zone Indonesia: Province Population Potentially affected by heavy ash fall, hot mad and < 1,5 1,5 - 3,5 3,5 - 7 7 - 12 12 - 43 Hazard Zone I ejected rocks fragments Potentially affected by rain lahar and possibility affected by 10 Km incandescent eruption lahar Potentially affected by ash fall and possibility affected Kawasan Rawan Bencana II by incandescent ejected rocks fragments Potentially affected by pyroclastic flows, lava flows, eruption lahar and rain lahars Admin Boundaries Kawasan Rawan Bencana III Prvince Boundary Sub-District Boundary Always threatened by pyroclastic flows, toxic gases, eruption District Boundary lahar, and possibility lava flows