Scholarlink

At several localities on Samosir Island, viscous rhyolitic magma oozed to the surface and produced small, steep-sided piles of lava known as lava domes. Clusters of lava domes occur near lake level at Tuk-Tuk and Batu-Batu east of the Samosir Fault, as well as on the uplifted portion of Samosir at Sigornang and Janji Mariatoruan.

错误：搜索内容不能为空，请输入英文关键词
错误：关键词超出字数限制，请精简
高级检索

The Samosir Lava Domes—Remnant YTT Magma Oozes to the Surface

  • 章节

  • 发表日期：

    2025年

查看全文
  • Craig A. Chesner

摘要

At several localities on Samosir Island, viscous rhyolitic magma oozed to the surface and produced small, steep-sided piles of lava known as lava domes. Clusters of lava domes occur near lake level at Tuk-Tuk and Batu-Batu east of the Samosir Fault, as well as on the uplifted portion of Samosir at Sigornang and Janji Mariatoruan.