Japan Geoscience Union Meeting 2024

Presentation information

[J] Poster

S (Solid Earth Sciences ) » S-VC Volcanology

[S-VC26] Active Volcanism

Tue. May 28, 2024 5:15 PM - 6:45 PM Poster Hall (Exhibition Hall 6, Makuhari Messe)

convener:Yuta Maeda(Nagoya University), Takahiro Miwa(National research institute for earth science and disaster prevention), Takeshi Matsushima(Institute of Seismology and Volcanology, Faculty of Science, Kyushu University)

5:15 PM - 6:45 PM

[SVC26-P12] Deformations Detected by Precise Levelling and GNSS Campaign Surveys in the Hakone volcano (2015-2023)

*Masayuki Murase1, Kazutaka Mannen2, Takeshi Matsushima3, Jun Oikawa4, Kazuya Uchida3, Tatsunosuke Shimeno3, Rion Ikuta3, Yusei Nukaga1, Kazuki Hosoya1, Yuji Miyashita2, Yuki Abe2, RYOTA NINOMIYA2, Kotaro Toyama2, Ryo Kurihara2, Yutaka Nagaoka2 (1.Department of Earth and Environmental Sciences, College of Humanities and Sciences, NIHON University, 2.Hot Springs Research Institute of Kanagawa Prefecture, 3.Faculty of Sciences, Kyushu University, 4.Earthquake Research Institute, The University of Tokyo)

Keywords:Hakone Volcano, Precise Leveling Survey, GNSS, Deformation

The precise leveling and the GNSS campaign surveys were conducted due to discuss the deformations in the Hakone volcano in the period from 2015 to 2021.
The leveling routes of about 11 km with 41 benchmarks were established on the northern flank of central cone of Hakone volcano in 2015. The main route was extended from GEONET Hakone (Ninodaira) to the Togendai ropeway station. In order to improve the spatial layout of the benchmarks, a branched leveling route extended to Owakudani was established. We conducted the precise leveling surveys in December 2015, September 2016, December 2017, December 2018, December 2019, December 2020, December 2021 and December 2023.
The GNSS campaign surveys were conducted on the four observation points around the leveling route in December 2017, December 2018, December 2019, December 2020, December 2021 and December 2023. Deformations of not only the four campaign sites but also continuous GNSS station (GEONET Hakone) were calculated using the RTKLIB (Takasu et al.,2007).
In the period of December 2021- December 2023, the subsidence of 12mm was detected with respect to the GEONET Hakone on the Owakudani, and the small uplift of 3mm was detected around the junction of Owakudani.
As the total deformaion in the period between December 2015 and December 2021, the subsidence of 76mm and the uplift of 15mm were detected in the Owakludani and the junction of Owakudani, respectively.
Since GEONET Hakone is too close to accept as a reference point for the vertical deformation in Hakone volcano, we used GEONET Atsugi as the reference point. The GEONET Hakone showed the uplift of 7mm with respect to the GEONET Atsugi in the period from December 2021 to December 2023. Therefore, the uplift of 10mm was detected with respect to the GEONET Atsugi around the junction of Owakudani in this period.
In the period from December 2021 to December 2023, slight increases of seismic activity were observed in December 2021, March 2023 and October 2023.
A In the junction of Owakudani, horizontal deformation of 8mm with East-Southeast direction was calculated with respect to the GEONET Atsugi in the period of 2017-2020. In other stations, no significant deformations over 5mm were detected.
Acknowledgement: This work was supported by the 2023 Hakone-Geopark Grant.