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    <title>Qualla: The 1833 Shonai Earthquake: When the Sea of Japan Rose</title>
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    <description><![CDATA[On December 7, 1833, a magnitude 7.5-7.7 earthquake ruptured the seafloor off Yamagata Prefecture, sending tsunami waves up to eight meters high crashing into the coast of Edo-period Japan and killing 150 people.]]></description>
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    <itunes:summary><![CDATA[On December 7, 1833, a magnitude 7.5-7.7 earthquake ruptured the seafloor off Yamagata Prefecture, sending tsunami waves up to eight meters high crashing into the coast of Edo-period Japan and killing 150 people.]]></itunes:summary>
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      <title>Qualla: The 1833 Shonai Earthquake: When the Sea of Japan Rose</title>
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      <title>The 1833 Shonai Earthquake: When the Sea of Japan Rose: Introduction</title>
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      <description><![CDATA[At two o'clock in the afternoon on December 7, 1833 -- the twenty-sixth day of the tenth month of Tenpo 4 by the Japanese calendar -- the Sea of Japan heaved. The seafloor off the coast of Yamagata Prefecture ruptured along the eastern margin of the basin, sending shockwaves through Akita, Yamagata, and Niigata prefectures. Within minutes, the ocean withdrew from the shoreline. Then it returned. Tsunami waves reached eight meters at Kamomoya, roughly the height of a three-story building. Along the Shonai coast, fishing boats were swept inland, houses dissolved into debris, and 150 people lost their lives in a disaster that would reshape how the Tokugawa shogunate understood the seismic dangers of Japan's western shore.]]></description>
      <content:encoded><![CDATA[<p>At two o'clock in the afternoon on December 7, 1833 -- the twenty-sixth day of the tenth month of Tenpo 4 by the Japanese calendar -- the Sea of Japan heaved. The seafloor off the coast of Yamagata Prefecture ruptured along the eastern margin of the basin, sending shockwaves through Akita, Yamagata, and Niigata prefectures. Within minutes, the ocean withdrew from the shoreline. Then it returned. Tsunami waves reached eight meters at Kamomoya, roughly the height of a three-story building. Along the Shonai coast, fishing boats were swept inland, houses dissolved into debris, and 150 people lost their lives in a disaster that would reshape how the Tokugawa shogunate understood the seismic dangers of Japan's western shore.</p>
<p><strong>Read more:</strong> <a href="https://qualla.com/1833-sh-nai-earthquake/">The 1833 Shonai Earthquake on Qualla</a></p>]]></content:encoded>
      <pubDate>Tue, 17 Feb 2026 00:00:00 GMT</pubDate>
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      <title>The 1833 Shonai Earthquake: When the Sea of Japan Rose: A Fault Line in Waiting</title>
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      <description><![CDATA[Japan sits at the collision of four tectonic plates: the Pacific, Philippine Sea, Okhotsk, and Amurian. Most attention goes to the eastern coast, where the Pacific Plate dives beneath Japan at the Japan Trench -- the same subduction zone responsible for the devastating 2011 Tohok...]]></description>
      <content:encoded><![CDATA[<p>Japan sits at the collision of four tectonic plates: the Pacific, Philippine Sea, Okhotsk, and Amurian. Most attention goes to the eastern coast, where the Pacific Plate dives beneath Japan at the Japan Trench -- the same subduction zone responsible for the devastating 2011 Tohok...</p>
<p><strong>Read more:</strong> <a href="https://qualla.com/1833-sh-nai-earthquake/">The 1833 Shonai Earthquake on Qualla</a></p>]]></content:encoded>
      <pubDate>Tue, 17 Feb 2026 00:00:00 GMT</pubDate>
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      <title>The 1833 Shonai Earthquake: When the Sea of Japan Rose: Two Faults, One Afternoon</title>
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      <description><![CDATA[The 1833 earthquake ruptured two segments of the convergent boundary faults along the eastern margin of the Sea of Japan. The rupture zone partially overlapped that of the 1964 Niigata earthquake, though parts extended farther north. Seismologists have estimated the earthquake's ...]]></description>
      <content:encoded><![CDATA[<p>The 1833 earthquake ruptured two segments of the convergent boundary faults along the eastern margin of the Sea of Japan. The rupture zone partially overlapped that of the 1964 Niigata earthquake, though parts extended farther north. Seismologists have estimated the earthquake's ...</p>
<p><strong>Read more:</strong> <a href="https://qualla.com/1833-sh-nai-earthquake/">The 1833 Shonai Earthquake on Qualla</a></p>]]></content:encoded>
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      <title>The 1833 Shonai Earthquake: When the Sea of Japan Rose: The Wave and Its Toll</title>
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      <description><![CDATA[The tsunami struck the Shonai coast with devastating force. At Kamomoya in Yamagata Prefecture, waves reached seven to eight meters. Large waves battered a 30-to-50-kilometer stretch of coastline. Farther afield, the tsunami measured five to six meters at Wajima on the Noto Penin...]]></description>
      <content:encoded><![CDATA[<p>The tsunami struck the Shonai coast with devastating force. At Kamomoya in Yamagata Prefecture, waves reached seven to eight meters. Large waves battered a 30-to-50-kilometer stretch of coastline. Farther afield, the tsunami measured five to six meters at Wajima on the Noto Penin...</p>
<p><strong>Read more:</strong> <a href="https://qualla.com/1833-sh-nai-earthquake/">The 1833 Shonai Earthquake on Qualla</a></p>]]></content:encoded>
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      <title>The 1833 Shonai Earthquake: When the Sea of Japan Rose: Echoes Along the Margin</title>
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      <description><![CDATA[The 1833 Shonai earthquake was neither the first nor the last major event along this boundary. It belongs to a sequence of powerful earthquakes and tsunamis that have periodically ruptured the eastern margin of the Sea of Japan over the past three centuries. The 1964 Niigata eart...]]></description>
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<p><strong>Read more:</strong> <a href="https://qualla.com/1833-sh-nai-earthquake/">The 1833 Shonai Earthquake on Qualla</a></p>]]></content:encoded>
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