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    <title>Qualla: Hawaii Hotspot</title>
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    <description><![CDATA[A plume of magma rising from deep in Earth's mantle has been building volcanoes for at least 80 million years, leaving a 6,200-kilometer trail of seamounts, atolls, and islands across the Pacific -- with the Big Island of Hawaii as its latest creation.]]></description>
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    <copyright>© 2026 Bendyline</copyright>
    <lastBuildDate>Mon, 20 Jul 2026 10:21:09 GMT</lastBuildDate>
    <itunes:author>Qualla</itunes:author>
    <itunes:summary><![CDATA[A plume of magma rising from deep in Earth's mantle has been building volcanoes for at least 80 million years, leaving a 6,200-kilometer trail of seamounts, atolls, and islands across the Pacific -- with the Big Island of Hawaii as its latest creation.]]></itunes:summary>
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      <itunes:name>Qualla</itunes:name>
      <itunes:email>support@bendyline.com</itunes:email>
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      <title>Qualla: Hawaii Hotspot</title>
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      <title>Hawaii Hotspot: Introduction</title>
      <link>https://qualla.com/hawaii-hotspot/</link>
      <description><![CDATA[Photo credit Joel E. Robinson, USGS., Public domain. Trace a line on a map from the Big Island of Hawaii northwest across the Pacific, and it runs through a chain of progressively older, smaller, more eroded islands before disappearing beneath the waves as a string of submerged seamounts. Follow it far enough -- 6,200 kilometers -- and it reaches the Aleutian Trench near Russia. This entire chain, from the youngest active volcanoes on the Big Island to coral atolls so ancient they are being swallowed back into the Earth, was built by a single source: the Hawaii hotspot, a plume of magma rising from deep in the mantle that has been producing volcanoes for at least 80 million years.]]></description>
      <content:encoded><![CDATA[<p>Photo credit Joel E. Robinson, USGS., Public domain. Trace a line on a map from the Big Island of Hawaii northwest across the Pacific, and it runs through a chain of progressively older, smaller, more eroded islands before disappearing beneath the waves as a string of submerged seamounts. Follow it far enough -- 6,200 kilometers -- and it reaches the Aleutian Trench near Russia. This entire chain, from the youngest active volcanoes on the Big Island to coral atolls so ancient they are being swallowed back into the Earth, was built by a single source: the Hawaii hotspot, a plume of magma rising from deep in the mantle that has been producing volcanoes for at least 80 million years.</p>
<p><strong>Read more:</strong> <a href="https://qualla.com/hawaii-hotspot/">Hawaii Hotspot on Qualla</a></p><p><em>Image: Joel E. Robinson, USGS. | Public domain</em></p>]]></content:encoded>
      <pubDate>Thu, 12 Mar 2026 00:00:00 GMT</pubDate>
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      <itunes:duration>0:06</itunes:duration>
      <itunes:episode>1</itunes:episode>
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      <title>Hawaii Hotspot: Wilson&apos;s Moving Plate</title>
      <link>https://qualla.com/hawaii-hotspot/</link>
      <description><![CDATA[Photo credit G.E. Ulrich, USGS. Cropping by Hike395 (talk · contribs), Public domain. In 1963, Canadian geophysicist J. Tuzo Wilson proposed an idea that would reshape the understanding of volcanic island chains. Most volcanoes form at the boundaries of tectonic plates, where plates collide, separate, or grind past each other. Hawaii sits in the middle of the Paci...]]></description>
      <content:encoded><![CDATA[<p>Photo credit G.E. Ulrich, USGS. Cropping by Hike395 (talk · contribs), Public domain. In 1963, Canadian geophysicist J. Tuzo Wilson proposed an idea that would reshape the understanding of volcanic island chains. Most volcanoes form at the boundaries of tectonic plates, where plates collide, separate, or grind past each other. Hawaii sits in the middle of the Paci...</p>
<p><strong>Read more:</strong> <a href="https://qualla.com/hawaii-hotspot/">Hawaii Hotspot on Qualla</a></p><p><em>Image: G.E. Ulrich, USGS. Cropping by Hike395 (talk · contribs) | Public domain</em></p>]]></content:encoded>
      <pubDate>Thu, 12 Mar 2026 00:00:00 GMT</pubDate>
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      <itunes:episode>2</itunes:episode>
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      <title>Hawaii Hotspot: The Life and Death of a Hawaiian Volcano</title>
      <link>https://qualla.com/hawaii-hotspot/</link>
      <description><![CDATA[Photo credit Dave Bunnell, CC BY-SA 3.0. Hawaiian volcanoes follow a remarkably consistent life cycle. Each begins as a submarine seamount, fed by the hotspot plume. Lava output gradually increases until the volcano breaches the ocean surface, becoming an island. Height and eruptive activity peak when the volcano is aro...]]></description>
      <content:encoded><![CDATA[<p>Photo credit Dave Bunnell, CC BY-SA 3.0. Hawaiian volcanoes follow a remarkably consistent life cycle. Each begins as a submarine seamount, fed by the hotspot plume. Lava output gradually increases until the volcano breaches the ocean surface, becoming an island. Height and eruptive activity peak when the volcano is aro...</p>
<p><strong>Read more:</strong> <a href="https://qualla.com/hawaii-hotspot/">Hawaii Hotspot on Qualla</a></p><p><em>Image: Dave Bunnell | CC BY-SA 3.0</em></p>]]></content:encoded>
      <pubDate>Thu, 12 Mar 2026 00:00:00 GMT</pubDate>
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      <title>Hawaii Hotspot: The Emperor&apos;s Bend</title>
      <link>https://qualla.com/hawaii-hotspot/</link>
      <description><![CDATA[Photo credit G.E. Ulrich, USGS. Cropping by Hike395 (talk · contribs), Public domain. The Hawaiian-Emperor seamount chain does not run in a straight line. About 47 million years ago, the chain makes a sharp bend, shifting from a nearly due-north trend to the northwest orientation visible today. This bend was long interpreted as evidence of a major change in the di...]]></description>
      <content:encoded><![CDATA[<p>Photo credit G.E. Ulrich, USGS. Cropping by Hike395 (talk · contribs), Public domain. The Hawaiian-Emperor seamount chain does not run in a straight line. About 47 million years ago, the chain makes a sharp bend, shifting from a nearly due-north trend to the northwest orientation visible today. This bend was long interpreted as evidence of a major change in the di...</p>
<p><strong>Read more:</strong> <a href="https://qualla.com/hawaii-hotspot/">Hawaii Hotspot on Qualla</a></p><p><em>Image: G.E. Ulrich, USGS. Cropping by Hike395 (talk · contribs) | Public domain</em></p>]]></content:encoded>
      <pubDate>Thu, 12 Mar 2026 00:00:00 GMT</pubDate>
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      <itunes:duration>0:06</itunes:duration>
      <itunes:episode>4</itunes:episode>
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      <title>Hawaii Hotspot: Fire Below, and Still Rising</title>
      <link>https://qualla.com/hawaii-hotspot/</link>
      <description><![CDATA[Photo credit G.E. Ulrich, USGS. Cropping by Hike395 (talk · contribs), Public domain. The hotspot is not finished. Kamaʻehuakanaloa Seamount, formerly known as Loihi, is the newest volcano in the chain. It sits about 20 miles off the southeast coast of the Big Island, its summit still roughly 3,000 feet below the ocean surface. Geologists estimate it will breach t...]]></description>
      <content:encoded><![CDATA[<p>Photo credit G.E. Ulrich, USGS. Cropping by Hike395 (talk · contribs), Public domain. The hotspot is not finished. Kamaʻehuakanaloa Seamount, formerly known as Loihi, is the newest volcano in the chain. It sits about 20 miles off the southeast coast of the Big Island, its summit still roughly 3,000 feet below the ocean surface. Geologists estimate it will breach t...</p>
<p><strong>Read more:</strong> <a href="https://qualla.com/hawaii-hotspot/">Hawaii Hotspot on Qualla</a></p><p><em>Image: G.E. Ulrich, USGS. Cropping by Hike395 (talk · contribs) | Public domain</em></p>]]></content:encoded>
      <pubDate>Thu, 12 Mar 2026 00:00:00 GMT</pubDate>
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      <itunes:duration>0:06</itunes:duration>
      <itunes:episode>5</itunes:episode>
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