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Yonaguni Monument

earth science Maturity 11-13 Next article →

The Yonaguni Monument is a mysterious submerged rock formation. It sits off the coast of Yonaguni, which is the southernmost island in the Ryukyu Islands of Japan. The site is located about 100 kilometres east of Taiwan. This underwater site is famous because people disagree about what it actually is. Some believe it was built by humans long ago. Other scientists argue that nature created these shapes through geological processes. This debate makes the monument a very important subject for study.

The discovery of the monument happened by accident in 1986. Kihachiro Aratake was a director for the Yonaguni-Cho Tourism Association. He was diving in the area to find hammerhead sharks. The sea near Yonaguni is very popular for diving during winter months. While looking for sharks, Aratake noticed seabed formations that looked like architectural structures. Soon after, a team of scientists led by Masaaki Kimura visited the site. Kimura is a marine geologist from the University of the Ryukyus. He claims the formations are man-made stepped monoliths, which are large single stones.

To understand the site, we must look at its geology. The formation is located below the Arakawabana cliff. This cliff is at the southern tip of Yonaguni island. The rocks are made of medium to very fine sandstones and mudstones. These belong to the Early Miocene Yaeyama Group. Geologists believe these rocks were deposited about 20 million years ago. Most of the rocks are connected to the underlying rock mass. They are not separate, freestanding rocks piled together.

Many experts believe the shapes are purely natural. Geologist Robert M. Schoch explains how the rock behaves. He observed that the sandstones contain many parallel bedding planes. These are flat layers where the rock can easily separate. The rocks also have many sets of parallel, vertical joints. Joints are natural fractures or cracks in the stone. Because Yonaguni is in an earthquake-prone region, these cracks can be very regular. Schoch suggests that the "walls" are just horizontal platforms. These platforms fell into a vertical position when the rock below them eroded.

There is a significant scientific debate regarding the history of the site. Masaaki Kimura once estimated the formation was at least 10,000 years old. He thought it might be part of a lost continent called Mu. In 2007, he revised this estimate to 2,000 or 3,000 years old. He believes tectonic activity caused the structures to be submerged. He claims to see a pyramid, roads, and even a stadium. However, archaeologist Richard J. Pearson believes this is unlikely. Other researchers, like Wolf Wichmann, also concluded the site was formed by natural processes.

Modern technology has provided more evidence for the natural theory. In 2019, Takayuki Ogata and other researchers used a digital elevation model. This is a computer tool used to map the shape of the land or sea floor. They also conducted geological field investigations of the rocks. They studied three specific locations called "geosites": Tindabana, Kube Ryofurishi, and Sanninudai. Their research showed the monument is a natural feature. It was formed by weathering and erosion acting on the bedding and joints. They found similar features at the Sanninudai geosite on the island.

Despite the scientific consensus, the monument remains a popular place for divers. The ocean currents at the site can be very strong. Famous freediver Jacques Mayol visited the site and wrote a book about his dives. Supporters of the artificial theory, like Graham Hancock, still argue the site is unique. They say it is unlikely to find so many strange shapes in one small area. They also note a lack of loose blocks on the flat areas. However, Schoch points out that strong currents likely sweep the rocks clean.

The study of the Yonaguni Monument connects to many different fields. It involves marine geology to understand the rock layers. It involves archaeology to debate human history. It also involves oceanography to study how currents and erosion work. Whether the site was built by hands or by nature, it shows how much we can learn from the sea.

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