The Leirbotnar field, where IDDP-01 is situated consists of an upper liquid dominated zone to 1000-1400 m depth, 190-220 degrees C, sulphate major anion, and a lower two phase zone, 300 degrees C chloride main anion. The IDDP-01 fluid is dry steam, local origin, pH 3. The major anion is chloride (20-166 mg/kg), probably of magmatic origin. The major metallic cations, Fe (5-100 mg/kg), Cr (0-6 mg/kg), Ni (0-5 mg/kg) and Mn (0.1-0.8 mg/kg) seem to be derived from the well casing and sampling equipment. The gas content is low (about 0.1%) and the gas is apparently not directly emitted from magma. (C) 2013 Elsevier Ltd. All rights reserved.