A Kingdom's Seismic Memory
In Gyeongju, the ancient capital of the Silla Kingdom, history is recorded in monuments, but in the earth itself. For nearly two millennia, court scribes and royal astrologers of Korea's successive dynasties meticulously documented seismic events. They viewed earthquakes as potent omens related to the monarch's reign, and so their descriptions were detailed. These records, found in texts like the Samguk Sagi (History of the Three Kingdoms) and the Annals of the Joseon Dynasty, are one of the longest continuous earthquake archives in the world.
The oldest known record of an earthquake in Korea dates to 2 AD. A particularly destructive event appears in the Samguk Sagi from March of 779 AD, describing a quake in the capital (modern Gyeongju) that "collapsed houses and more than 100 people died". This event is estimated to have had a magnitude between 6.7 and 7.0. Over the centuries, scribes logged more than 1,800 seismic incidents, noting the shaking but also the locations, damage to buildings, and even associated sounds. This level of detail, recorded consistently over centuries, is a dataset for modern science.
From Ancient Texts to Fault Lines
For many years, the Korean peninsula was considered a region of low seismic activity. This perception was challenged on September 12, 2016, when a magnitude 5.8 earthquake struck Gyeongju. It was the largest instrumentally recorded earthquake in South Korea at the time. The event prompted seismologists to look again at the ancient texts. By correlating the locations and described intensities of historical quakes with modern geological mapping, scientists gained new insights into the region's tectonics.
The research confirmed significant seismic activity along the Yangsan Fault system, a major NNE-SSW striking fault that runs for about 200 kilometers across the peninsula, passing near Gyeongju. Analysis of the historical data helps scientists understand the fault's behavior over a much longer timescale than instrumental records allow. Paleoseismic trenching studies along the fault have found evidence of large, surface-rupturing earthquakes with magnitudes potentially around Mw 7. By matching these geological signs with the written accounts, researchers can better estimate the recurrence intervals of major quakes and improve seismic hazard models, turning ancient omens into modern warnings.