Hotspot Volcanism

Most volcanoes happen where plates meet, but some come from a "hot spot" deep underground that stays in one place. As the plate moves over the hot spot, it creates a chain of islands, like Hawaii. It's like moving a piece of paper over a steady candle flame.

Even when everything else is moving, there are steady "sources" of power that stay exactly where they are to create something new.

Hotspot Volcanism (Mantle Plumes) provides a "fixed" reference frame for plate motion. Unlike boundary volcanism, hotspots are intraplate phenomena. They create volcanic "age-progressive" chains (like the Hawaiian-Emperor seamount chain), allowing geologists to calculate the absolute velocity and direction of tectonic plates over millions of years. Certain people act as "hotspots" in history β€” they stay fixed in their truth while the plate of humanity moves over them, creating chains of new ideas and islands of progress.

SOUND: The "hiss" of steam escaping a tea kettle.

SMELL: The smoky, burnt smell of a campfire.

TASTE: A spicy chili pepper β€” a "hot spot" on your tongue!

TOUCH: Feel the warmth of a heating pad in one specific spot on your back.

SIGHT: Watch a line of bubbles rising in a glass of soda.

BODY: Imagine walking across a hot beach; you keep moving, but the heat stays in the sand.

Music: Watching the Wheels by John Lennon

HotspotHawaiian Islands

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Hotspot Volcanism

The Steady Flame Below

Most volcanoes happen where plates meet, but some come from a "hot spot" deep underground that stays in one place. As the plate moves over the hot spot, it creates a chain of islands, like Hawaii. It's like moving a piece of paper over a steady candle flame.