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cc-by (c) Janeras Casanova, Marc et al., 2015
Please use this identifier to cite or link to this item: https://hdl.handle.net/2445/163102

Using several monitoring techniques to measure the rock mass deformation in the Montserrat Massif

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Montserrat Mountain is located near Barcelona in Catalonia, at the north-east corner of Spain, and its massif is formed by conglomerate interleaved by siltstone/sandstone with steep slopes very prone to rock falls. The increasing visitor's number in the monastery area, reaching 2.4 million per year, has pointed out the risk derived from rock falls for this building area and also for the terrestrial accesses, both roads and rack railway. A risk mitigation plan is currently been applied for 2014-2016 that contains monitoring testing and implementation as a key point. The preliminary results of the pilot tests carried out during 2014 are presented, also profiting from previous sparse experiences and data, and combining 4 monitoring techniques under different conditions of continuity in space and time domains, which are: displacement monitoring with Ground-based Synthetic Aperture Radar and characterization at slope scale, with an extremely non uniform atmospheric phase screen because of the stepped topography and atmosphere stratification; Terrestrial Laser Scanner surveys quantifying frequency for unnoticed activity of small rock falls, and monitoring rock block displacements over 1cm; monitoring of rock joints with a wireless net of sensors; and tentative surveying for singular rocky needles with Total Station.

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JANERAS CASANOVA, Marc, et al. Using several monitoring techniques to measure the rock mass deformation in the Montserrat Massif. IOP Conference Series: Earth and Environmental Science. 2015. Vol. 26, num. 1-19. ISSN 1755-1307. [consulted: 15 of June of 2026]. Available at: https://hdl.handle.net/2445/163102

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