Figure - PMC

Skip to main content

An official website of the United States government

Here's how you know

Here's how you know

Official websites use .gov
A .gov website belongs to an official government organization in the United States.

Secure .gov websites use HTTPS
A lock ( ) or https:// means you've safely connected to the .gov website. Share sensitive information only on official, secure websites.

View full-text article in PMC

. 2021 Aug 3;11:15703. doi: 10.1038/s41598-021-94866-2

Search in PMC
Search in PubMed
View in NLM Catalog
Add to search

© The Author(s) 2021

Open AccessThis article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.

PMC Copyright notice

Projection of energy line model along the southeast profile of Taal Volcano Island where observation and calculation points for velocity are located from the vent center to the projected maximum runout distance. Velocities calculated using different methods (vC) and velocities calculated using the energy line model (vEL) for each of the four observation points are shown. (A) Location of southeast profile and observation points. (B) Image from timelapse video at 36 seconds showing 500–600 m open area within the southeast inner crater. (C) Image from time-lapse video at 46 seconds showing the area from B being covered by a moving base surge.