Bringing the Submarine Mariana Arc and Backarc Basin to Life for Undergraduates and the Public

IF 1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY Island Arc Pub Date : 2024-09-18 DOI:10.1111/iar.12533
Robert J. Stern
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Abstract

This paper aims to better teach about submarine arc and backarc basin volcanic and hydrothermal activity using the ~1400 km long Mariana convergent margin as an example. Four US National Oceanographic and Atmospheric Administration (NOAA) expeditions (2004–2016) equipped with a remotely operated vehicle (ROV) have discovered and explored many of submarine volcanoes and associated hydrothermal fields and generated many short (~1 min long) videos about them. Some of these videos would be very useful for teaching about these processes if they were organized and context provided, which is done here. Eighteen short videos about nine sites generated by NOAA are presented and discussed here. These are organized into three categories: volcanic eruptions, magmatic degassing, and hydrothermal activity. Volcanic eruption videos include two about glassy pillow lavas erupted in 2013–2015 and a rare example of a submarine eruption. Four videos about magmatic degassing include an example of sulfur produced by disproportionation of magmatic sulfur dioxide associated with a submarine eruption, two rare examples of molten sulfur lakes, and liquid carbon dioxide venting. Four videos about hydrothermal activity are provided. Suggestions for how this material might be used in the classroom are also given.

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让本科生和公众了解马里亚纳海底弧和后弧盆地
本文旨在以约 1400 公里长的马里亚纳汇聚边缘为例,更好地介绍海底弧和弧后盆地的火山和热液活动。美国国家海洋和大气管理局(NOAA)的四次探险(2004-2016 年)配备了遥控潜水器(ROV),发现并探索了许多海底火山和相关热液场,并制作了许多有关它们的视频短片(约 1 分钟长)。如果对其中一些视频进行整理并提供背景信息,将对这些过程的教学非常有用。这里介绍并讨论了由 NOAA 制作的有关 9 个站点的 18 个视频短片。这些视频分为三类:火山爆发、岩浆脱气和热液活动。火山喷发视频包括两个关于 2013-2015 年喷发的玻璃枕状熔岩的视频,以及一个罕见的海底喷发实例。四段关于岩浆脱气的视频包括一个与海底喷发有关的岩浆二氧化硫比例失调产生硫磺的实例、两个罕见的熔融硫湖实例以及液态二氧化碳喷口。还提供了四段有关热液活动的视频。此外,还就如何在课堂上使用这些资料提出了建议。
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来源期刊
Island Arc
Island Arc 地学-地球科学综合
CiteScore
2.90
自引率
26.70%
发文量
32
审稿时长
>12 weeks
期刊介绍: Island Arc is the official journal of the Geological Society of Japan. This journal focuses on the structure, dynamics and evolution of convergent plate boundaries, including trenches, volcanic arcs, subducting plates, and both accretionary and collisional orogens in modern and ancient settings. The Journal also opens to other key geological processes and features of broad interest such as oceanic basins, mid-ocean ridges, hot spots, continental cratons, and their surfaces and roots. Papers that discuss the interaction between solid earth, atmosphere, and bodies of water are also welcome. Articles of immediate importance to other researchers, either by virtue of their new data, results or ideas are given priority publication. Island Arc publishes peer-reviewed articles and reviews. Original scientific articles, of a maximum length of 15 printed pages, are published promptly with a standard publication time from submission of 3 months. All articles are peer reviewed by at least two research experts in the field of the submitted paper.
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