Downloaded from http://sp.lyellcollection.org/ at Simon Fraser University on January 26, 2016 New insights into the Kawah Ijen hydrothermal system from geophysical data CORENTIN CAUDRON1,2,3*, GUILLAUME MAURI4,5, GLYN WILLIAMS-JONES5, THOMAS LECOCQ2, DEVY KAMIL SYAHBANA6, RAPHAEL DE PLAEN7, LOIC PEIFFER8, ALAIN BERNARD3 & GINETTE SARACCO9 1Earth Observatory of Singapore, Nanyang Technological University, 50 Nanyang Avenue, Block N2-01a-15, Singapore 639798 2Royal Observatory of Belgium, Seismology Section, 3 avenue Circulaire, 1180 Uccle, Belgium 3Department of Earth and Environmental Sciences, Universite´ Libre de Bruxelles, 50 Avenue 9 Roosevelt, 1050 Brussels, Belgium 4Center for Hydrogeology and Geothermics, University of Neuchtel, Neuchtel, Switzerland 5Department of Earth Sciences, Simon Fraser University, 8888 University Drive, Burnaby, British Columbia, V5A 1S6, Canada 6Centre for Volcanology and Geological Hazard Mitigation, Geological Agency, Ministry of Energy and Mineral Resources, Jalan Diponegoro 57, Bandung 40122, Indonesia 7University of Luxembourg, Faculte´ des Sciences, de la Technologie et de la Communication, 6 rue Richard Coudenhove-Kalergi, L-1359 Luxembourg 8Instituto de Energı´as Renovables, Universidad Nacional Auto´noma de Me´xico, Privada Xochicalco s/n, Centro, 62580 Temixco, Morelos, Mexico 9CNRS-UMR7330, Centre Europeen de Recherche et d’Enseignement en Geosciences de l’Environnement (CEREGE), Equipe Modelisation, Aix-Marseille Universite´ (AMU), Europole de l’Arbois, BP 80, 13545 Aix-en-Provence cedex 4, France *Corresponding author (e-mail:
[email protected]) Abstract: The magmatic–hydrothermal system of Kawah Ijen volcano is one of the most exotic on Earth, featuring the largest acidic lake on the planet, a hyper-acidic river and a passively degas- sing silicic dome.