Advertisement

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

  • 306 Accesses

Correction to: Landslides

Fig. 1
figure1

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.

Author information

Correspondence to Marco Mulas.

Additional information

The online version of the original article can be found at https://doi.org/10.1007/s10346-019-01248-x

Rights and permissions

Reprints and Permissions

About this article

Verify currency and authenticity via CrossMark

Cite this article

Mulas, M., Marnas, M., Ciccarese, G. et al. Correction to: Sinusoidal wave fit indexing of irreversible displacements for crackmeters monitoring of rockfall areas: test at Pietra di Bismantova (Northern Apennines, Italy). Landslides 17, 241–242 (2020). https://doi.org/10.1007/s10346-019-01281-w

Download citation