Japan: a country full of geologic activity

Jay and I arrived in Japan on 27 August and will be traveling in the country for 6 weeks. There are many reasons to travel here. The culture and history are fascinating and—wow!—who doesn’t enjoy the high quality food. For two earth scientists, learning more about the country’s geologic makeup is another big draw. In Japan, no one is immune from the potential geologic action of earthquakes, volcanic eruptions, or both. Weather can be very active too, as typhoons (i.e., hurricanes) regularly impact the islands during this time of year. In the six days since we’ve been here, typhoon Shanshan arrived, stalled and pounded southern Japan with high wind and rains, causing destructive landsliding and flooding.

When we flew into Tokyo on 27 August (photo from the air), typhoon Shanshan was still located offshore. Fortunately for us, it moved very slowly and our only impact was some rain in Tokyo that did not cancel our flight to Sapporo on the 30th.

Let’s think about subduction zones

The purpose of this first post is to introduce the islands’ tectonic setting. The primary theme is subduction tectonics, where oceanic plates slide beneath continental plates. Those of us who live in the Pacific Northwest, adjacent to the Cascadia Subduction Zone, are familiar with this type of tectonics. These are the places on Earth where the largest earthquakes and most of the dangerous volcanic eruptions occur. Japan has experienced subduction tectonics for 500 million years, so it has a long and complicated history of continual geologic activity.

This Google Earth image shows the location of Japan between the Pacific Ocean and mainland Asia. The shades of blue indicate water depth—light blue is shallow and dark blue is deep. Japan consists of many islands. We will visit Hokkaido, the northernmost island, and Honshu, the main island. Today, we left Sapporo to travel around Hokkaido for nearly two weeks. After that, we will return to Honshu.

Inevitably, subduction zones produce earthquakes and volcanoes. Earthquakes occur when the oceanic plate slips along a fault and sinks farther beneath the continental plate. Volcanoes occur because the down-going oceanic plate causes rocks to melt and ascend all of the way to Earth’s surface where the magma erupts. See my post about converging plates for more details: https://landscapes-revealed.net/plate-tectonics-101-what-happens-when-plates-move-toward-each-other/.

Twenty-three million years ago, Japan was attached to mainland China. But changes in the subduction zone caused Japan to pull away from the rest of Asia to form the Japan Sea. This sea is called a back-arc basin because it is on the backside of the subduction zone. Although this side of Japan doesn’t have the super-large earthquakes like the east side does, damaging earthquakes are still common. For example, on January 1 of this year, a magnitude 7.5 earthquake occurred on the Noto Peninsula. Figure is from Wikipedia: https://en.wikipedia.org/wiki/Geology_of_Japan.

In Sapporo and heading east to national parks

After two days in Sapporo, we today headed eastward to explore some of Japan’s finest national parks.

This view from our hotel window in Sapporo shows mountains west of Sapporo that are inactive, eroded volcanoes. We did a lovely hike to the top of Maruyama, the prominent mountain on the left side of the photo. [yama=mountain]
This view is back eastward over Sapporo from Maruyama. The mountains in the distance are more now-inactive volcanoes.

Next we’ll visit some national parks with still-active volcanoes. Still tuned!

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4 Comments

  1. Lynn on September 2, 2024 at 6:21 am

    What a slew of active volcanos in Japan! Looking forward to learning more about the geography of Japan from you two.

    • Landscapes Revealed on September 2, 2024 at 3:55 pm

      We’re off to see a whole string of them today!

  2. John Penny on September 2, 2024 at 8:21 am

    Great piece… you must be in seismic heaven! Have a wonderful time in the best travel destination on the planet.

    • Landscapes Revealed on September 2, 2024 at 3:54 pm

      We’ll exchange note in October!

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