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    <title>Qualla: 2002 Sandaun Earthquake</title>
    <link>https://qualla.com/2002-sandaun-earthquake</link>
    <description><![CDATA[Just before dawn on 9 September 2002, the ground off the Sandaun coast lurched so violently that the sea itself surged ashore - a magnitude 7.6 reverse-faulting earthquake followed by a five-metre tsunami, the largest quake to hit mainland Papua New Guinea since 1938.]]></description>
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    <itunes:author>Qualla</itunes:author>
    <itunes:summary><![CDATA[Just before dawn on 9 September 2002, the ground off the Sandaun coast lurched so violently that the sea itself surged ashore - a magnitude 7.6 reverse-faulting earthquake followed by a five-metre tsunami, the largest quake to hit mainland Papua New Guinea since 1938.]]></itunes:summary>
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      <itunes:name>Qualla</itunes:name>
      <itunes:email>support@bendyline.com</itunes:email>
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      <title>Qualla: 2002 Sandaun Earthquake</title>
      <link>https://qualla.com/2002-sandaun-earthquake</link>
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      <title>2002 Sandaun Earthquake: Introduction</title>
      <link>https://qualla.com/2002-sandaun-earthquake/</link>
      <description><![CDATA[Photo credit Carport, CC BY-SA 3.0. At 04:44:23 local time on 9 September 2002, people in Wewak were still asleep when the Pacific plate slipped. A magnitude 7.6 earthquake ruptured the sea floor off Sandaun Province, shallow enough to push the water above it. In coastal Wewak, buildings collapsed; in villages near Ubidnim, water and sand erupted from the ground in fountains five metres high as the saturated soil liquefied. Then the sea came. A five-metre wave rolled into East Sepik, swept homes from their foundations, and killed a child and another person by drowning. Six people had already died in the earthquake itself. Seventy were injured. It was the largest earthquake to strike mainland Papua New Guinea since 1938.]]></description>
      <content:encoded><![CDATA[<p>Photo credit Carport, CC BY-SA 3.0. At 04:44:23 local time on 9 September 2002, people in Wewak were still asleep when the Pacific plate slipped. A magnitude 7.6 earthquake ruptured the sea floor off Sandaun Province, shallow enough to push the water above it. In coastal Wewak, buildings collapsed; in villages near Ubidnim, water and sand erupted from the ground in fountains five metres high as the saturated soil liquefied. Then the sea came. A five-metre wave rolled into East Sepik, swept homes from their foundations, and killed a child and another person by drowning. Six people had already died in the earthquake itself. Seventy were injured. It was the largest earthquake to strike mainland Papua New Guinea since 1938.</p>
<p><strong>Read more:</strong> <a href="https://qualla.com/2002-sandaun-earthquake/">2002 Sandaun Earthquake on Qualla</a></p><p><em>Image: Carport | CC BY-SA 3.0</em></p>]]></content:encoded>
      <pubDate>Thu, 09 Apr 2026 00:00:00 GMT</pubDate>
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      <itunes:episode>1</itunes:episode>
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      <title>2002 Sandaun Earthquake: Where Plates Collide</title>
      <link>https://qualla.com/2002-sandaun-earthquake/</link>
      <description><![CDATA[Photo credit Mikenorton, CC BY-SA 3.0. New Guinea lies in one of the busiest tectonic intersections on Earth, where the Australian and Pacific plates grind past and into each other along a long, complicated boundary. Along its northern coast, the action is concentrated in the collision of the Huon-Finisterre island ar...]]></description>
      <content:encoded><![CDATA[<p>Photo credit Mikenorton, CC BY-SA 3.0. New Guinea lies in one of the busiest tectonic intersections on Earth, where the Australian and Pacific plates grind past and into each other along a long, complicated boundary. Along its northern coast, the action is concentrated in the collision of the Huon-Finisterre island ar...</p>
<p><strong>Read more:</strong> <a href="https://qualla.com/2002-sandaun-earthquake/">2002 Sandaun Earthquake on Qualla</a></p><p><em>Image: Mikenorton | CC BY-SA 3.0</em></p>]]></content:encoded>
      <pubDate>Thu, 09 Apr 2026 00:00:00 GMT</pubDate>
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      <title>2002 Sandaun Earthquake: Signs Before the Shock</title>
      <link>https://qualla.com/2002-sandaun-earthquake/</link>
      <description><![CDATA[Photo credit Mikenorton, CC BY-SA 3.0. The Sandaun earthquake did not arrive without warning, though no one reads the warnings clearly until afterward. Thirty-six foreshocks preceded the main rupture, including a magnitude 6.2 event in October 2001 and a magnitude 6.7 near Aitape in January 2002 that killed one person...]]></description>
      <content:encoded><![CDATA[<p>Photo credit Mikenorton, CC BY-SA 3.0. The Sandaun earthquake did not arrive without warning, though no one reads the warnings clearly until afterward. Thirty-six foreshocks preceded the main rupture, including a magnitude 6.2 event in October 2001 and a magnitude 6.7 near Aitape in January 2002 that killed one person...</p>
<p><strong>Read more:</strong> <a href="https://qualla.com/2002-sandaun-earthquake/">2002 Sandaun Earthquake on Qualla</a></p><p><em>Image: Mikenorton | CC BY-SA 3.0</em></p>]]></content:encoded>
      <pubDate>Thu, 09 Apr 2026 00:00:00 GMT</pubDate>
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      <title>2002 Sandaun Earthquake: The Wave in the Dark</title>
      <link>https://qualla.com/2002-sandaun-earthquake/</link>
      <description><![CDATA[Photo credit Mikenorton, CC BY-SA 3.0. The U.S. Geological Survey estimated a maximum Modified Mercalli intensity of X - extreme - near the epicentre, tapering to strong shaking of intensity VI in Wewak, Kairiru, Ambunti, Angoram, and Aitape. Even Keerom and Jayapura across the Indonesian border felt moderate tremors....]]></description>
      <content:encoded><![CDATA[<p>Photo credit Mikenorton, CC BY-SA 3.0. The U.S. Geological Survey estimated a maximum Modified Mercalli intensity of X - extreme - near the epicentre, tapering to strong shaking of intensity VI in Wewak, Kairiru, Ambunti, Angoram, and Aitape. Even Keerom and Jayapura across the Indonesian border felt moderate tremors....</p>
<p><strong>Read more:</strong> <a href="https://qualla.com/2002-sandaun-earthquake/">2002 Sandaun Earthquake on Qualla</a></p><p><em>Image: Mikenorton | CC BY-SA 3.0</em></p>]]></content:encoded>
      <pubDate>Thu, 09 Apr 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>2002 Sandaun Earthquake: Aftermath on a Moving Coast</title>
      <link>https://qualla.com/2002-sandaun-earthquake/</link>
      <description><![CDATA[Photo credit Mikenorton, CC BY-SA 3.0. The strongest aftershock, a magnitude 6.3, struck on 16 September southwest of the mainshock. Another magnitude 6.2 hit Marienberg Rural LLG in February 2003. Hundreds of homes and buildings across Sandaun and East Sepik were damaged or destroyed, mostly in Wewak. The toll could ...]]></description>
      <content:encoded><![CDATA[<p>Photo credit Mikenorton, CC BY-SA 3.0. The strongest aftershock, a magnitude 6.3, struck on 16 September southwest of the mainshock. Another magnitude 6.2 hit Marienberg Rural LLG in February 2003. Hundreds of homes and buildings across Sandaun and East Sepik were damaged or destroyed, mostly in Wewak. The toll could ...</p>
<p><strong>Read more:</strong> <a href="https://qualla.com/2002-sandaun-earthquake/">2002 Sandaun Earthquake on Qualla</a></p><p><em>Image: Mikenorton | CC BY-SA 3.0</em></p>]]></content:encoded>
      <pubDate>Thu, 09 Apr 2026 00:00:00 GMT</pubDate>
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      <itunes:episode>5</itunes:episode>
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      <title>2002 Sandaun Earthquake: A Coastline That Keeps Rising</title>
      <link>https://qualla.com/2002-sandaun-earthquake/</link>
      <description><![CDATA[Photo credit Mikenorton, CC BY-SA 3.0. The small uplifts measured after the quake - 30 to 40 centimetres across stretches of the Momase Region coastline - are the geological signature of what happens every time a reverse fault ruptures offshore here. Over geologic time, these small jumps add up to the terraces and rai...]]></description>
      <content:encoded><![CDATA[<p>Photo credit Mikenorton, CC BY-SA 3.0. The small uplifts measured after the quake - 30 to 40 centimetres across stretches of the Momase Region coastline - are the geological signature of what happens every time a reverse fault ruptures offshore here. Over geologic time, these small jumps add up to the terraces and rai...</p>
<p><strong>Read more:</strong> <a href="https://qualla.com/2002-sandaun-earthquake/">2002 Sandaun Earthquake on Qualla</a></p><p><em>Image: Mikenorton | CC BY-SA 3.0</em></p>]]></content:encoded>
      <pubDate>Thu, 09 Apr 2026 00:00:00 GMT</pubDate>
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