Berkeleyan
Sinking coastline may precede large subduction-zone quakes
Area residents may not notice the subsidence, but instruments can. The hope is to pinpoint the chronological relationship between subsidence and a large quake — the better to plan for temblors and resulting tsunamis
| 02 February 2005
 Signs in Crescent City, near the Oregon border, reflect the lessons learned in the aftermath of the killer 1964 Alaska earthquake, when a tsunami hit the city, killing 11. (Photo courtesy david.sampson.id.au/photos/) |
“In areas along subduction zones, like the Northwest coast of the United States, we should look to see where the land has subsided and put instruments there to monitor it,” said Jere Lipps, a professor of integrative biology and study co-author. “If the land continues to subside instead of relaxing back to normal, it could indicate a big earthquake and a tsunami might occur some time in the next few years.”
Subduction zones are areas where one of the Earth’s tectonic plates slips under another, raising mountain ranges along the margin sprinkled with volcanoes. Quakes occur when the edge of the overlying plate sticks to the subducting plate, causing a slight dip nearest the zone and a slight bulge farther away. Eventually, the stuck edge lets go in a massive quake, after which the margin relaxes to pre-quake levels. Because plates thrust over one another in these zones, the quakes are referred to as megathrust earthquakes. They often generate tsunamis.
A tiltmeter can tell
“What we think happens is, two to five years before a quake, the plate boundary starts to drag down ever so slightly before it fractures,” said David Scott, the Killam Professor of Earth Sciences at Dalhousie University in Halifax. “Before that, you’ve got subsidence that is almost undetectable to the people living there. But you could detect it with a tiltmeter. We have shown that we can detect it in the paleoenvironment.”
A paper describing their findings will be published in the May/June issue of the Geological Society of America Bulletin.
The team surveyed salt marshes along the Pacific coast from Alaska to Northern California, taking 12-foot deep cores to look for signs of past subsidence coinciding with evidence of a major quake, such as soil liquefaction and sand deposited by a tsunami. Subsidence is indicated by a temporary change in the types of microscopic organisms with shells — specifically foraminifera and thecamoebians — in the mud, as the formerly freshwater marshes sink and become brackish or saltwater marshes.
One marsh in Alaska apparently sank about half a foot starting perhaps 15 years before the devastating 1964 Alaska quake, which measured 9.2 on the Richter scale and generated a tsunami that killed dozens of people along the Pacific coast, including 11 in the Northern California town of Crescent City. Similarly, a core from a marsh in Oregon showed evidence of four large quakes over the past 3,000 years, each preceded by subsidence.
Planning for a hard-to-plan-for quake
Seismologists estimate that the period between megathrust quakes along the Cascadia Subduction Zone, where the Pacific, Juan de Fuca, and Gorda Oceanic plates creep under the North American plate, ranges from hundreds to thousands of years. This makes them hard to plan for, Scott noted. Precursory subsidence detected by tiltmeters would at least allow people along the coast to plan for a major quake and probable tsunami.
The indicator marshes are typically freshwater marshes within inches of the high-tide mark, so that subsidence of a few inches increases slightly the saltiness of the marsh, either through salt spray or intrusion of salt water at high tide, and shifts the species of foraminifera living there. Marshes like those sampled in this study would be ideal sites for installation of tiltmeters, the researchers said, because of their past history of earthquake precursors.
In the past, Scott has looked in sediments for foraminifera and thecamoebians — essentially amoebas with microscopic shells — deposited by past hurricanes along the Atlantic coast and into the Arctic. He was intrigued, however, by the efforts of other researchers to use diatoms or pollen to chart the history of quake-related subsidence in marshes along the Pacific coast. The big 1964 Alaskan quake, for example, temporarily dropped some coastal land six feet, drowning towns and forests, the latter becoming standing “ghost forests.” Scott thought that forams and thecamoebians might be able to give more precise dates for precursory subsidence, since they are more sensitive than diatoms to elevation changes. Thecamoebians, for example, live only in fresh water.
Looking initially at a core from Girdwood Flat, a marsh at Turnagain Arm in Cook Inlet, the site of the 1964 Alaska quake, he spotted an obvious precursor event just prior to that quake.
“About a centimeter below the quake itself, I saw this phenomenal change in the fauna, going from a bunch of species that live in the forest to a slightly brackish fauna with only one species,” he said. Teaming up with Lipps, Scott said, “We started looking at other sequences to make sure that wasn’t just a one-off thing. It turned out we were able to see an 1,800-year event from the same area and, of course, we went down to Oregon and found the same thing.”
Four of the cores from Girdwood Flat showed evidence of subsidence as much as 15 years prior to the 1964 quake, and one contained evidence of a quake with precursory subsidence 1,800 years ago. The subsidence is distinct from the much larger drop that occurs during the quake itself.
In a core from Netarts Bay, Ore., just north of Tillamook, the species of foraminfera present indicated three repeating sequences of high marsh transitioning to low marsh as the land began to sink, then tsunami sand without foraminifera, followed by a return to high marsh as the land relaxed after the earthquake. (Sand deposited by tsunamis can be distinguished from storm-deposited sand because the former scours the deep bottom where there are few forams, while storms carry sand from shallow waters that contain many forams.)
The three sequences corresponded to megathrust quakes and tsunamis 3,000 years ago, 1,840 years ago and 1,670 years ago, though the core revealed a fourth event 300 years ago not accompanied by a tsunami but showing precursory subsidence as well as sudden subsidence due to a quake. Stems, twigs, and driftwood embedded in the sand and mud were used to carbon-date the core sections. Independent evidence of these past quakes exists only for the 300-year-old event.
Scott noted that more than a dozen estuaries between Clayoquot Sound, British Columbia, and the Eel River in California record evidence of buried marsh or forest soils, and may be good sites for future monitoring. Whether suitable coastal marshes can be found near all subduction zones is a big question, however, and not all subduction zones may act the same.
“It could be that subduction zones don’t look the same everywhere — there may not be subsidence before a quake,” said Lipps, whose main interest is the evolution of forams and other ancient life forms. Lipps and Scott have sampled similar situations around the Pacific Rim and found evidence of quakes and tsunamis in cores from New Zealand, Mexico, and Tahiti. They plan to do the same in the Indian Ocean to look for evidence of precursors to megathrust quakes and to document the history of tsunamis there. They also will attempt to pinpoint more precisely the time between land subsidence and earthquakes along the Pacific Northwest coast.