Notice

1 Mar. 2024
Registration for participation in the symposium is closed
1 Mar. 2024
Timetable for the symposium is updated
1 Mar. 2024
Guide Map is updated
20 Feb. 2024
Timetable for the symposium is published
20 Feb. 2024
Access Map is updated
9 Jan. 2024
Deadline for modification of abstract has passed
Application to poster presentation is closed
Registration without presentation is still open
14 Nov. 2023
Application to oral presentation and travel grant is closed
Application to poster presentation and registration for participation are still open
2 Nov. 2023
Flyer for the symposium is updated (PDF)
30 Oct. 2023
Deadline for application to presentation and travel grant is extended to 14 Nov. 2023
30 Oct. 2023
Application to field trip is closed (the number of applicants reaches the limit)
19 Oct. 2023
Flyer for the symposium is published (PDF)
16 Oct. 2023
Subsidizers information updated
12 Sep. 2023
Open for aplication to presentation and registration for participation , travel grant, and field trip
21 Jun. 2023
Homepage Open

Application/Registration

Registration is closed.
Aplication to Poster presentations is closed.
Deadline for modification of abstract has passed.

Introduction

The submarine caldera eruption produces a significant amount of pyroclastics/volcaniclastics and give rise to associated tsunamis, exerting a profound and far-reaching impact on human existence, societal infrastructure, and the natural environment (e.g., the Kikai-Akahoya eruption of Kikai, Japan; the Minoan eruption of Santorini, Greece). Understanding the eruption styles/mechanisms, marine tephra records, magma properties/storage, and the magma supply systems leading to these eruptions poses significant challenges due to their inaccessibility. Nonetheless, recent comprehensive studies utilizing marine seafloor observations, seafloor sampling, and scientific drilling have greatly advanced our understanding of these volcanic systems. The purpose of this symposium is to share the latest advancements in understanding submarine caldera volcanoes through various research approaches, discuss the results, and foster future investigations with international collaborations. Contributions on submarine eruptions, including non-caldera events, as well as on-land eruptions, are also welcomed and encouraged.

Schedule

12.Sep 2023
Open for aplication to presentation and registration for participation , travel grant, and field trip
31 Oct. 2023
Deadline for application to presentation, travel grant, and field trip
14 Nov. 2023
Deadline for application to presentation, travel grant (extended)
9 Jan. 2024
Deadline for modification of abstract
Deadline for application to poster presentation and modification of abstract
28 Feb. 2024
Deadline for registration for participation in the symposium (no presentation)
5 Mar. 2024
Icebreaker at Kobe University
Time 16:00 - 18:00
6-7 Mar. 2024
Symposium at Kobe University Centennial Hall

Day1
Reception opens at 8:15
Time 9:00-18:10
Welcome dinner ( at Kobe University, Time 18:30 - )
Day2
Reception opens at 8:00
Time 8:40-15:55

Timetable for the symposium (PDF)

8-10 Mar. 2024
Field trip at Kikai Caldera in southern Kyushu, Japan

Travel grant

Application is closed.

A limited number of travel-grants up to $1000 per individual coming from abroad and some support per domestic individual, for students and post-doctoral fellows or early career scientists are available. Priority will be given to individuals from developing countries. An oral or poster presentation is required to qualify.

Field trip

Application is closed.

Kikai caldera: a large silicic magmatic system beneath the sea

The Kikai caldera was formed by the youngest large-scale caldera-forming eruptions. We will observe products of the Kikai-Akahoya eruption at various distances from near to the source area to southern Kyushu. We will also compare the deposits with other large-scale pyroclastic-flow deposits in southern Kyushu including Quaternary non-welded Ito pyroclastic-flow deposit and the densely welded Ata pyroclastic- flow deposit.

*Please be careful that the number of participants is limited.


Locations:
Satsuma Iwo-jima Island, Ibusuki region, southeast of Satsuma Peninsula, and Minami-Osumi region, southwest Japan.
Itinerary:
7 Mar. 2024
Move to Kagoshima city after symposium.
8 Mar. 2024
Move to Satsuma Iwo-jima Island by Ferry Mishima in the morning.
Field trip for observation of Kikai-Akahoya eruptive products within the island.
Stay at Satsuma Iwo-jima.
9 Mar. 2024
Observation of the Kikai deposit from the boat “Mishima-II” in the early morning.
Move to Kagoshima city by Ferry Mishima in the morning.
Field trip for Kikai-Akahoya eruptive deposit in southeast of Satusma Peninsula.
Stay at Ibusuki.
10 Mar. 2024
Move to Osumi Peninsula by ferry.
Field trip for Kikai eruptive deposit in South Osumi Peninsula and middle Osumi Pninsula,and Ito ignimbrite and Ata ignimbrite at Tarumizu region.
Stay at Kagoshima city.

*The itinerary is subject to change, depending on the ferryboat schedule under bad marine conditions.

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If you encounter an error , please contact us ,'calderasymp2024@gsuite.kobe-u.ac.jp'.