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gatheringsunbeams:
“Mt. Fuji | 2017 (x)
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gatheringsunbeams:

Mt. Fuji | 2017 (x)

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Timelapse of the webcam watching the Icelandic lava flow today. Watch for the people that walk along the flow front and the helicopters that fly overhead!

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After several weeks of earthquakes indicating magma migration on the Reykjanes peninsula on the southwest corner of Iceland, an eruption has begun with lava at the surface and glow from it visible on this webcam.

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Is waiting for a volcano better than watching paint dry?

The Reykjanes Peninsula in Iceland runs off to the southwest side of the island. It’s the point at which the Mid-Atlantic Ridge comes onshore, and it is above the ocean surface because of the interaction between volcanism on that ridge and the nearby Iceland Plume. The rocks, therefore, are recent volcanic rocks, and the peninsula is resurfaced by volcanism every few thousand years.

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tirsostudios

Feliz noche desde Mirador del Fuego, Acatenango, El volcán de fuego demostrando el esplendor de nuestro país

Fuego volcano, behind Acatenango, erupting at night.

(Source: instagram.com)

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explaurmore:

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Climbing the second highest peak in Washington (Mount Adams) this past weekend.

(Source: instagram.com)

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aladlammu:
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Large eruption column above an eruption in Indonesia

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A tour of the volcanic landscape of Kamchatka

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The Emperor’s Head
Our modern thinking behind hotspots is that they are generated by mantle plumes. A huge plume of extra warm mantle rises up to the surface, triggering formation of a large igneous province – a huge pile of igneous rocks somewhere...

The Emperor’s Head

Our modern thinking behind hotspots is that they are generated by mantle plumes. A huge plume of extra warm mantle rises up to the surface, triggering formation of a large igneous province – a huge pile of igneous rocks somewhere on the surface. That is followed by a long chain of volcanoes, produced by warm mantle continuing to rise up the pipe formed by the plume.

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(Source: business.facebook.com)