No abstract

Lava flow simulations are valuable tools for forecasting and assessing the areas potentially affected by new eruptions, interpreting past volcanic events, and understanding the lava flow behaviour's controls. Q-LavHA (v 2.0) plugin of Mossoux et al. (2016) combines and improves existing deterministic (FLOWGO) and probabilistic ("Maximum Length" and "Decreasing Probability") codes which allow calculating the probability of lava flow spatial propagation and terminal length. We investigate the Q-LavHA algorithm's effectiveness in twenty Holocene ʻaʻā lava flows of Gran Canaria (Canary Islands). Pre-eruptive and updated digital elevation models (DEMs) (25 m of resolution) and associated topographic and morphometric parameters have been used as essential input data to simulate the lava flows. Besides, thermorheological properties of the studied Holocene lavas have also been provided in the deterministic approach. The probabilistic lava flow maps produced by Q-LavHA and the fitness indexes calculated for assessing the simulated lava flow' accuracy indicate that the probabilistic "Maximum Length" constraint provides the best simulations. By Manuscript 2 using this method, many of the simulations in Gran Canaria almost overlap the real lava flow entirely even if overestimated areas are, in some cases, relatively high. By contrast, underestimated areas are generally low. The best results are those in which the highest inundation probability is observed within the main channel where the actual lava flow is emplaced, and even if overestimated areas are high, they are associated with low pixel inundation.

<p>Ten informative panels were designed to organize an exhibition of the LAJIAL project results about the recent volcanism of El Hierro Island and the 2021 eruption in La Palma Island. The format was self-rolling panels (roll-ups) 1 m wide by 2 m high, easily transportable, and highly protective. This exhibition was entitled 'Volcanoes in motion: El Hierro and La Palma' and allows us to understand that the volcanic phenomenon is very dynamic and capable of quickly changing the forms of relief, the water network, or the land use. The presentation in all these panels always keeps the same content: an upper strip including the titles of the exhibition, the thematic block, and the panel, as well as its numbering and logos of the promoting entities; a central part with much visual information in the form of maps, figures and photos accompanied by concise and easy-to-read texts; and a lower strip with the credits of the authors and logos of their institutions.</p><p>The first block of panels, 'A sea of volcanoes', deals with the generation of intraplate volcanic islands, with the example of the Canary Islands (Panel 1: The Canary Islands, that is how it all began) and the geological evolution of the island of El Hierro (Panel 2: And El Hierro was born). The second block, 'Volcanic landscapes of El Hierro', focuses on geological structures on a large scale (Panel 3: Megastructures) and a small scale (Panel 4: Structures on the ground). The third block, 'Explore your volcanic paradise', pays homage to the geological maps and the last eruption on El Hierro island. Panel 5: Walking among volcanoes shows the Gorona del Lajial eruption, a true paradise of volcanic structures but a geological puzzle solved within the framework of the LAJIAL project. Panel 6: 'The last volcano' is dedicated to the eruption of the Tagoro submarine volcano. The fourth block, 'Living among volcanoes', focuses on the islander's adaptation to the volcanic territory through the rational exploitation of groundwater (Panel 7: Water on El Hierro), volcanic materials as construction elements, or the figure of the UNESCO Geopark of El Hierro (Panel 8: What the land tells us), which brings together the geology of the island with its inhabitants, promoting the sustainable development, its agricultural techniques or knowledge of its archaeological remains. The last block of two panels, 'La Palma: the pretty island' is devoted to the geological evolution of La Palma island (Panel 9: And La Palma was born) and the 2021 eruption of Tajogaite volcano (Panel 10: The eruption of 2021) that represent the last volcanic activity in the archipelago.</p><p>Financial support was provided by Project LAJIAL, Grant PGC2018-101027-B-I00 funded by MCIN/AEI/10.13039/ 501100011033 and by "ERDF A way of making Europe", by the "European Union". CPT acknowledges the PhD Grant 2021 FISDU 00347, Departament de Recerca i Universitats, Generalitat de Catalunya. This study was carried out in the framework of the Research Consolidated Groups GEOVOL (Canary Islands Government, ULPGC) and GEOPAM (Generalitat de Catalunya, 2017 SGR 1494).</p>

Recent subaerial volcanism at El Hierro Island (Canary Islands, Spain) consists of monogenetic volcanic fields. This volcanism generated cinder cones, tephra air-fall deposits, and lava flows. The lava flows reach several kilometres in length extending through shore platforms and, sometimes, penetrating under the sea level. The volcanic landforms of El Hierro convert it into a natural laboratory for topographic and morphometric modelling and lava flow simulations. We perform the modelling and simulation of the Montaña de Aguarijo eruption, a cinder cone at the NE rift. The associated lava flow channelled through a V-shaped ravine until reaching a cliff, where formed cascades. The flow spread at the cliff base over a platform before reaching the sea modifying the coastline. Different maps were designed to show the results, including the geomorphologic reconstruction of the area affected by this eruption and the lava flow simulations obtained with the Q-LavHA plugin.

We explain, through a collection of ten panels distribuited in five thematic blocks, the geological history of the El Hierro and La Palma islands in the framework of intraplate volcanic islands evolution. In the first two panels we explain how the Canary Islands were formed and evolved, and the birth of El Hierro, the youngest island of the archipelago. Next, we observe the landscapes of El Hierro as a response to macro-scale, such as giant landslides and rifts, and micro-scale phenomena (volcanic cones, lava fields and shore platforms). The last eruption of the El Hierro island in 2011-12 that gave rise to the Tagoro submarine volcano is also exposed. In addition, we present how the Herreños have adapted to the territory, knowing how to take advantage of its scarce water resources and adapt their way of life to the volcanic landscape, achieving that the entire island was declared in 2000 a UNESCO World Biosphere Reserve and Geopark in 2015. In the last two panels we expose the geological evolution of the island of La Palma and its last eruption of the Tajogaite volcano in 2021. THEMATIC BLOCK I. A SEA OF VOLCANOES:“Origin of the Canary islands”, “And El Hierro was born”. THEMATIC BLOCK II. VOLCANIC LANDSCAPES:"Megaestructures", “Structures on the ground”. THEMATIC BLOCK III. EXPLORE THE VOLCANIC PARADISE:“Walking among volcanoes”, "The last volcano of El Hierro" THEMATIC BLOCK IV. LIVING AMONG VOLCANOES:"The water in El Hierro",“What the land tell us” THEMATIC BLOCK V. LA PALMA: THE PRETTY ISLAND: "And La Palma was born",“The 2021 eruption”.