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Geotourism on an active volcanic island (La Palma, Canary Islands, Spain)

Javier Dóniz-Páez

Javier Dóniz-Páez

Geoturvol-Department of Geography and History, University of La Laguna, Canarian Volcanological Institute (INVOLCAN)Canary Islands,
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Dóniz-Páez, Javier
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Nemesio M. Pérez

Nemesio M. Pérez

Canarian Volcanological Institute (INVOLCAN), Environmental Research Division, ITERCanary Islands,
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Pérez, Nemesio M.
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Rafael Becerra-Ramírez

Rafael Becerra-Ramírez

Geovol-Department of Geography and Territorial Planning, University of Castilla-La Mancha, Canarian Volcanological Institute (INVOLCAN)Canary Islands,
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Becerra-Ramírez, Rafael
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William Hernández-Ramos

William Hernández-Ramos

Geoturvol-Department of Geography and History, University of La Laguna, Canarian Volcanological Institute (INVOLCAN)Canary Islands,
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Hernández-Ramos, William
  
30 kwi 2024
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Data publikacji: 30 kwi 2024
Zakres stron: 47 - 53
Otrzymano: 08 mar 2024
Przyjęty: 05 kwi 2024
DOI: https://doi.org/10.2478/mgrsd-2023-0032
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© 2024 Javier Dóniz-Páez et al., published by Sciendo
This work is licensed under the Creative Commons Attribution 4.0 International License.

Figure 1.

A – Location of Canary Islands. B – Canarian Archipelago. C – La Palma study areaSource: prepared by the authors, based on Grafcan
A – Location of Canary Islands. B – Canarian Archipelago. C – La Palma study areaSource: prepared by the authors, based on Grafcan

Figure 2.

Tajogaite monogenetic eruption, 2021, La PalmaSource: authors
Tajogaite monogenetic eruption, 2021, La PalmaSource: authors

Figure 3.

Evolution of the number of visitors to La Palma.Source: IS-185 Istac, 2023 Prepared by the authors
Evolution of the number of visitors to La Palma.Source: IS-185 Istac, 2023 Prepared by the authors

Figure 4.

Sites of geotourism interest, natural and urban, in the Aridane Valley and its surroundingsSource: prepared by the authors based on Grafcan
Sites of geotourism interest, natural and urban, in the Aridane Valley and its surroundingsSource: prepared by the authors based on Grafcan

Figure 5.

Geoforms generated by the Tajogaite eruption. A – cinder cone. B – hornitos spatter. C – effusive fissure. D – pahoehoe lava flows. D – aa lava channel. F – lava delta. G – lapilli field. H – beaches. I – lapilli dunesSource: authors and R. Gosálvez (photo F)
Geoforms generated by the Tajogaite eruption. A – cinder cone. B – hornitos spatter. C – effusive fissure. D – pahoehoe lava flows. D – aa lava channel. F – lava delta. G – lapilli field. H – beaches. I – lapilli dunesSource: authors and R. Gosálvez (photo F)
Język:
Angielski
Częstotliwość wydawania:
4 razy w roku
Dziedziny czasopisma:
Nauki o Ziemi, Geografia, Nauki o Ziemi, inne
Kanał RSS czasopisma