POST-ERUPTION LAVA DOME EMPLACEMENT MEASURED BY UAV PHOTOGRAMMETRY: AN INVESTIGATION ONE YEAR AFTER THE 2017–2019 MT. AGUNG ERUPTIONS

We present an observation of morphological changes at Mt. Agung lava dome one year after the 2017–2019 eruption crisis using UAV-photogrammetry method. Five time-series UAV datasets involve the images collected during the crisis period and the newest data collection (July 16, 2020) were used to prov...

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Main Authors: R. Andaru, J.-Y. Rau, D. K. Syahbana, H. D. Purnamasari
Format: Article
Language:English
Published: Copernicus Publications 2022-05-01
Series:The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
Online Access:https://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XLIII-B2-2022/517/2022/isprs-archives-XLIII-B2-2022-517-2022.pdf
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author R. Andaru
R. Andaru
J.-Y. Rau
D. K. Syahbana
H. D. Purnamasari
author_facet R. Andaru
R. Andaru
J.-Y. Rau
D. K. Syahbana
H. D. Purnamasari
author_sort R. Andaru
collection DOAJ
description We present an observation of morphological changes at Mt. Agung lava dome one year after the 2017–2019 eruption crisis using UAV-photogrammetry method. Five time-series UAV datasets involve the images collected during the crisis period and the newest data collection (July 16, 2020) were used to provide a detailed investigation of the changes in morphology inside the crater and land cover on the surrounding slopes. The digital surface models (DSMs) generated by structure-from-motion (SfM) with multi-view stereo (MVS) algorithm were used to quantify the dome growth, the surface emplacement, and the actual remaining deposited material eruption surrounding the summit. Analysis of the last two series orthoimages indicates that the crater surface's texture remarkably unchanged one year after the eruption crisis (the dome still presents rough surfaces that resemble small stones and sand). According to the DSMs difference, it is evident that there were no considerable surface displacements inside the dome. It implies that no significant magma pressure accumulation occurring the dome. However, we found a small-scale growth in the central dome, which has increased the dome height up to 2 m and inflate the dome with a volume of 45,950 m<sup>3</sup>. We have also observed a new lava lake (e.g., compound lava) with an area of 9,166 m<sup>2</sup> in the southeast of the dome edge. This new lava lake uplifts the surface up to 29 m and translated to a 79,623 m<sup>3</sup> additional volume. Meanwhile, the depression areas surrounding the central dome were observed with a depth between 0.5 and 4 m. The amount of material deposited on the volcano’s summit was identified with a total volume of 2.93 &times; 10<sup>6</sup> m<sup>3</sup>. This remaining deposited volume could be a potential lahar in the future. The ability to measure spatial and time-series of the lava dome changes from SfM-UAV, therefore, provides effective, detailed, and sometimes sole means of observing and quantifying dome surface emplacement in the period of before, during and after eruptions.
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spelling doaj.art-c0cbb9b390ee422a84e8315d90f0eb572022-12-22T03:36:06ZengCopernicus PublicationsThe International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences1682-17502194-90342022-05-01XLIII-B2-202251752210.5194/isprs-archives-XLIII-B2-2022-517-2022POST-ERUPTION LAVA DOME EMPLACEMENT MEASURED BY UAV PHOTOGRAMMETRY: AN INVESTIGATION ONE YEAR AFTER THE 2017–2019 MT. AGUNG ERUPTIONSR. Andaru0R. Andaru1J.-Y. Rau2D. K. Syahbana3H. D. Purnamasari4Department of Geodetic Engineering, Gadjah Mada University, IndonesiaDepartment of Geomatics, National Cheng Kung University, TaiwanDepartment of Geomatics, National Cheng Kung University, TaiwanCenter for Volcanology and Geological Hazard Mitigation, Geological Agency, Ministry of Energy and Mineral Resources, IndonesiaCenter for Volcanology and Geological Hazard Mitigation, Geological Agency, Ministry of Energy and Mineral Resources, IndonesiaWe present an observation of morphological changes at Mt. Agung lava dome one year after the 2017–2019 eruption crisis using UAV-photogrammetry method. Five time-series UAV datasets involve the images collected during the crisis period and the newest data collection (July 16, 2020) were used to provide a detailed investigation of the changes in morphology inside the crater and land cover on the surrounding slopes. The digital surface models (DSMs) generated by structure-from-motion (SfM) with multi-view stereo (MVS) algorithm were used to quantify the dome growth, the surface emplacement, and the actual remaining deposited material eruption surrounding the summit. Analysis of the last two series orthoimages indicates that the crater surface's texture remarkably unchanged one year after the eruption crisis (the dome still presents rough surfaces that resemble small stones and sand). According to the DSMs difference, it is evident that there were no considerable surface displacements inside the dome. It implies that no significant magma pressure accumulation occurring the dome. However, we found a small-scale growth in the central dome, which has increased the dome height up to 2 m and inflate the dome with a volume of 45,950 m<sup>3</sup>. We have also observed a new lava lake (e.g., compound lava) with an area of 9,166 m<sup>2</sup> in the southeast of the dome edge. This new lava lake uplifts the surface up to 29 m and translated to a 79,623 m<sup>3</sup> additional volume. Meanwhile, the depression areas surrounding the central dome were observed with a depth between 0.5 and 4 m. The amount of material deposited on the volcano’s summit was identified with a total volume of 2.93 &times; 10<sup>6</sup> m<sup>3</sup>. This remaining deposited volume could be a potential lahar in the future. The ability to measure spatial and time-series of the lava dome changes from SfM-UAV, therefore, provides effective, detailed, and sometimes sole means of observing and quantifying dome surface emplacement in the period of before, during and after eruptions.https://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XLIII-B2-2022/517/2022/isprs-archives-XLIII-B2-2022-517-2022.pdf
spellingShingle R. Andaru
R. Andaru
J.-Y. Rau
D. K. Syahbana
H. D. Purnamasari
POST-ERUPTION LAVA DOME EMPLACEMENT MEASURED BY UAV PHOTOGRAMMETRY: AN INVESTIGATION ONE YEAR AFTER THE 2017–2019 MT. AGUNG ERUPTIONS
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
title POST-ERUPTION LAVA DOME EMPLACEMENT MEASURED BY UAV PHOTOGRAMMETRY: AN INVESTIGATION ONE YEAR AFTER THE 2017–2019 MT. AGUNG ERUPTIONS
title_full POST-ERUPTION LAVA DOME EMPLACEMENT MEASURED BY UAV PHOTOGRAMMETRY: AN INVESTIGATION ONE YEAR AFTER THE 2017–2019 MT. AGUNG ERUPTIONS
title_fullStr POST-ERUPTION LAVA DOME EMPLACEMENT MEASURED BY UAV PHOTOGRAMMETRY: AN INVESTIGATION ONE YEAR AFTER THE 2017–2019 MT. AGUNG ERUPTIONS
title_full_unstemmed POST-ERUPTION LAVA DOME EMPLACEMENT MEASURED BY UAV PHOTOGRAMMETRY: AN INVESTIGATION ONE YEAR AFTER THE 2017–2019 MT. AGUNG ERUPTIONS
title_short POST-ERUPTION LAVA DOME EMPLACEMENT MEASURED BY UAV PHOTOGRAMMETRY: AN INVESTIGATION ONE YEAR AFTER THE 2017–2019 MT. AGUNG ERUPTIONS
title_sort post eruption lava dome emplacement measured by uav photogrammetry an investigation one year after the 2017 2019 mt agung eruptions
url https://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XLIII-B2-2022/517/2022/isprs-archives-XLIII-B2-2022-517-2022.pdf
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