<?xml version="1.0" encoding="utf-8" standalone="yes"?><rss version="2.0" xmlns:atom="http://www.w3.org/2005/Atom" xmlns:content="http://purl.org/rss/1.0/modules/content/"><channel><title>Volcanoes on Karpoke - Just Another Blog</title><link>http://karpoke.ignaciocano.com/tags/volcanoes/</link><description>Recent content in Volcanoes on Karpoke - Just Another Blog</description><generator>Hugo -- 0.167.0</generator><language>es</language><lastBuildDate>Fri, 29 May 2026 12:00:00 +0100</lastBuildDate><atom:link href="http://karpoke.ignaciocano.com/tags/volcanoes/index.xml" rel="self" type="application/rss+xml"/><item><title>When Volcanoes Die: The Science Explained</title><link>http://karpoke.ignaciocano.com/2026/05/29/when-volcanoes-die-the-science-explained/</link><pubDate>Fri, 29 May 2026 12:00:00 +0100</pubDate><guid>http://karpoke.ignaciocano.com/2026/05/29/when-volcanoes-die-the-science-explained/</guid><description>&lt;blockquote&gt;
&lt;p&gt;This video from MinuteEarth explains the three main ways volcanoes
eventually “die.” Some lose their magma supply when tectonic activity
stops, some drift away from underground hotspots like the one that
created Hawaii, and others literally clog themselves shut with cooled…&lt;/p&gt;
&lt;/blockquote&gt;
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