“…Tiltmeters, and in particular long‐base tiltmeters, have been primarily designed for monitoring deformation in various contexts [ Agnew , 1986], such as volcanoes (for a review, see, e.g., Dzurisin [2003]), gas fields [e.g., Sleeman et al , 2000], tunnelling [e.g., Feldman et al , 1998], mining [e.g., Chrzanowski et al , 1986], Earth tide studies [e.g., Melchior , 1983; Zürn et al , 1986], postglacial rebound [e.g., Kääriäinen , 1979] and tectonic crustal deformation [e.g., Wyatt et al , 1994; Anderson et al , 1997]. However, some instruments have achieved very low noise levels in a wide frequency range, allowing observations in the normal mode frequency band [e.g., Zürn et al , 1999, 2000; d'Oreye and Zürn , 2005; Braitenberg et al , 2006]. These instruments are relatively inexpensive since they do not require a sophisticated mechanical design.…”