Quick Look Inside The Volcano

Þríhnúkagígur-which roughly translates to “try to pronounce that you English-speaking sucker” (or to be pedantic “three peak volcano”)-is a geological oddity. When magma cools after an eruption, it solidifies and fills the volcano’s cone. But after Þríhnúkagígur erupted, the magma simply disappeared as though someone had pulled out the plug, leaving a uniquely preserved cavity, ready to be explored by wannabe spelunkers like myself...
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