Assessing qualitative long-term volcanic hazards at Lanzarote Island (Canary Islands)

Becerril, Laura; Martí, Joan; Bartolini, Stefania; Geyer, Adelina

doi:https://doi.org/10.5194/nhess-17-1145-2017

Articles | Volume 17, issue 7

https://doi.org/10.5194/nhess-17-1145-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/nhess-17-1145-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 17, issue 7

Research article

|

11 Jul 2017

Research article |

| 11 Jul 2017

Assessing qualitative long-term volcanic hazards at Lanzarote Island (Canary Islands)

Laura Becerril, Joan Martí, Stefania Bartolini, and Adelina Geyer

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Final revised paper (published on 11 Jul 2017)
Preprint (discussion started on 16 Jan 2017)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC1: 'nhess-2017-2 review JL Macias', José Luis Macías, 13 Feb 2017
- AC1: 'Reply to José Luis Macías', Laura Becerril, 25 Apr 2017
RC2: 'review', Sophie Mossoux, 21 Feb 2017
- AC3: 'Reply to Sophie Mossoux', Laura Becerril, 25 Apr 2017
AC2: 'Reply to Sophie Mossoux', Laura Becerril, 25 Apr 2017

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

ED: Publish subject to minor revisions (further review by Editor) (03 May 2017) by Giovanni Macedonio

AR by Laura Becerril on behalf of the Authors (11 May 2017) Author's response

ED: Publish as is (15 May 2017) by Giovanni Macedonio

AR by Laura Becerril on behalf of the Authors (25 May 2017) Author's response Manuscript

Short summary

Lanzarote is an island (Canaries, Spain), that has hosted the largest and longest eruption in the archipelago (Timanfaya 1730–36). It brought severe economic losses and forced local people to migrate. We have developed the first comprehensive hazard assessment for the island. New eruptions will take place close to the last one and will be characterised by Strombolian activity, with ash emission towards the S, medium-length lava flows and hydromagmatic activity only close to the coastal areas.