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Landslides

, Volume 17, Issue 1, pp 241–242 | Cite as

Correction to: Sinusoidal wave fit indexing of irreversible displacements for crackmeters monitoring of rockfall areas: test at Pietra di Bismantova (Northern Apennines, Italy)

  • Marco MulasEmail author
  • Martin Marnas
  • Giuseppe Ciccarese
  • Alessandro Corsini
Correction
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Correction to: Landslides
Fig. 1

a Geological setting: AVV Argille varicolori Formation (Upper Cretaceous-Lower Eocene); RAN3 Ranzano Formation (Upper Eocene-Lower Oligocene); CTG, CTG1 Contignaco Formation (Lower Miocene); PAT5 Pantano Formation—Pietra di Bismantova Member (Mid-Lower Miocene). b Wireless sensor node composed of the crackmeter and control unit for power and communication. c Position of installed crackmeters

  https://doi.org/10.1007/s10346-019-01248-x

The published version of this article, unfortunately, contained error. The corresponding author found out that in the published version, Figure 1c lacks the level regarding the crack meters position and labeling that was asked to edit during the proofreading. Given in this article is the correct figure.

The original article has been corrected.

Copyright information

© Springer-Verlag GmbH Germany, part of Springer Nature 2019

Authors and Affiliations

  • Marco Mulas
    • 1
    Email author
  • Martin Marnas
    • 2
  • Giuseppe Ciccarese
    • 1
  • Alessandro Corsini
    • 1
  1. 1.Department of Chemical and Geological SciencesUniversity of Modena and Reggio EmiliaModenaItaly
  2. 2.Ecole des Mines de NancyUniversité de LorraineNancy cedexFrance

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