At approximately 9 p.m. Pacific Standard Time, Jan. 26, 1700, a magnitude 8 or 9 earthquake occurred on the Cascadia Subduction Zone, a 600-mile stretch between Vancouver Island, British Columbia and Cape Mendocino, California.
Oral traditions of native people living in the Cascadia region reference , but those stories can鈥檛 be dated to specific calendar years.
Scientists are well aware of the destructive power of other subduction zone quakes 鈥� like the 1960 magnitude 9.5 and the 1964 magnitude 鈥� so they were eager to chart the history of plate activity in the Cascadia Subduction Zone.
In the 1980s and 1990s, scientists conducting fieldwork found evidence that coastal lands in the Northwest dropped suddenly and were inundated by tsunami waves and mud. All along the Oregon and Washington coast, the rapid advance of seawater had buried delicate marsh plants that were still alive and killed Sitka spruce, leaving behind rotting stumps. Rot-resistant western red cedar survived longer and their remnants became known as 鈥済host forests.鈥�
These sudden changes in the coastal landscape pointed heavily to an earthquake and tsunami.
American researchers used carbon dating on the spruce, peat and fossilized plants. Sitka spruce as far apart as southern Washington and Northern California 鈥� some time between 1695 and 1720. Their rings were wide right up through the last ring, proving that a sudden event rather than slow sea level rise was the culprit.
After the American scientists published their work, Japan鈥檚 Kenji Satake that summarized meticulous records from multiple locations in Japan describing high waves on Jan. 27 and 28.
It was called because there was no earthquake locally that could have triggered it. There is also no evidence of a large earthquake in South America or Alaska at that time. The signs pointed to a quake from the Cascadia Subduction Zone.
Satake explained that it would have taken a tsunami about 10 hours to travel from Cascadia to Japan, thus pinpointing the earthquake to about 9 p.m., Jan. 26. Because of the extent of the damage recorded in Japan, Satake estimated that it was approximately a magnitude 9 quake.
In 1997, scientists used dendrochronology 鈥� a method of dating trees by comparing ring patterns to samples of known age 鈥� on the ghost forest trees. They were able to determine the trees had stopped growing after completing the 1699 growing season, dating their death to somewhere between September 1699 and May 1700, further confirming the date independently of Japanese records.
More evidence is on the ocean floor. Paleoseismologists have . This data indicate a large earthquake with a lot of shaking was going on during this period 鈥� and that it was happening off the Oregon coast.
And remember the native stories? Scholarly analysis of nine stories with sufficient details to assign date ranges narrowed the timeline to approximately 1701, remarkably close to the accepted date for the event.
Over its 10,000-year rupture history, earthquakes around magnitude 9 have occurred along the length of the Cascadia Subduction Zone 19 times 鈥� about every 526 years. The southern section of the CSZ has seen 19 additional quakes of 8 or higher. Here, very close to home, the average recurrence is every 234 years. With the last major event placed at 315 years ago, we鈥檙e due.
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Cover of "The Orphan Tsunami of 1700" by Brian Atwater. The book outlines how scientists were able to pinpoint an earthquake along the Cascadia Subduction Zone in 1700 from evidence of a tsunami along Japan's coast.
A ghost forest of tree stumps emerges at low tide near Neskowin in Tillamook County. The trees are believed to be the remnants of forests growing before the last major earthquake and tsunami hit.