- Cascadia subduction zone
Cascadia subduction zoneis a subduction zone, a type of convergent plate boundary that stretches from northern Vancouver Islandto northern California.
The zone separates the Juan de Fuca, Explorer, Gorda and the
North American Plates. Here, the oceanic crustof the Pacific Oceansinks beneath the continent at a rate of 40 mm/yr. [cite web|url=http://vulcan.wr.usgs.gov/Volcanoes/JuanDeFucaRidge/description_juan_de_fuca.html|title=Juan de Fuca Volcanics|accessdate=2008-05-06 USGS]
The width of the Cascadia subduction zone fault varies along its length, depending on the temperature of the subducted oceanic plate, which heats up as it is pushed deeper beneath the continent. As it becomes hotter and more molten, it eventually loses the ability to store mechanical stress and generates
The Cascadia subduction zone presents a challenge to current tectonic theory which generally holds that subduction occurs as a plate becomes older, denser and thicker with distance from the ridge which contributes new material to it. In the case of Cascadia, its associated ridge is just a few hundred miles (and in places less) distant from the subduction zone. This puzzle is a matter of ongoing research and discussion. The current hypothesis which attempts to explain it is that once subduction begins, it continues by the process of slab-pull, i.e. the weight of the previously subducted segment exerts a force behind it on the remaining slab above the subduction zone, regardless of its density, pulling it downward.
The Cascadia subduction zone runs from triple junctions at its north and south ends. On the north just south of
Queen Charlotte Island, it intersects the Queen Charlotte Faultand the Explorer Ridge. On the south, just off of Cape Mendocinoin California, it intersects the San Andreas Faultand the Mendocino fault zone at the Mendocino Triple Junction.
The Cascadia subduction zone can produce very large earthquakes, magnitude 9.0 or greater, if rupture occurs over its whole area. When the "locked" zone stores up energy for an earthquake, the "transition" zone, although somewhat plastic, can rupture. Thermal and deformation studies indicate that the locked zone is fully locked for 60 kilometers (about 40 miles) downdip from the deformation front. Further downdip, there is a transition from fully locked to aseismic sliding.cite journal | author=Nedimovic MR, Hyndman RD, Ramachandran K, Spence GD | title=Reflection signature of seismic and aseismic slip on the northern Cascadia subduction interface | journal=Nature | volume=424 | issue=6947 | year=2003 | pages=416–20 | pmid=12879067 | doi=10.1038/nature01840]
In 1999, a group of Continuous
Global Positioning Systemsites registered a brief reversal of motion of approximately 2 centimeters (0.8 inches) over a 50 kilometer by 300 kilometer (about 30 mile by 200 mile) area. The movement was the equivalent of a 6.7 magnitude earthquake.cite journal | author=Dragert H, Wang K, James TS | title=A silent slip event on the deeper Cascadia subduction interface | journal=Science | volume=292 | issue=5521 | year=2001 | pages=1525–8 | pmid=11313500 | doi=10.1126/science.1060152] The motion did not trigger an earthquake and was only detectable as silent, non-earthquake seismic signatures.cite journal | author=Rogers G, Dragert H | title=Episodic tremor and slip on the Cascadia subduction zone: the chatter of silent slip | journal=Science | volume=300 | issue=5627 | year=2003 | pages=1942–3 | pmid=12738870 | doi=10.1126/science.1084783]
The last known great earthquake in the northwest was in January of 1700, the
Cascadia Earthquake. Geological evidence indicates that great earthquakes may have occurred at least seven times in the last 3,500 years, suggesting a return time of 300 to 600 years. There is also evidence of accompanying tsunamis with every earthquake, and one line of evidence for these earthquakes is tsunami damage, and through Japanese records of tsunamis.cite web|url=http://pubs.usgs.gov/pp/pp1707/pp1707.pdf|title=The Orphan Tsunami of 1700—Japanese Clues to a Parent Earthquake in North America|accessdate=2008-05-06 USGS Professional Paper 1707]
A future rupture of the Cascadia Subduction Zone would cause widespread destruction throughout the
Other similar subduction zones in the world usually have such earthquakes every 100–200 years; the longer interval here may indicate unusually large stress buildup and subsequent unusually large earthquake slip.
an Andreas Quake Connection
Studies of past earthquake traces on both the northern San Andreas Fault and the southern Cascadia Subduction Zone indicate a correlation in time which may be evidence that quakes on the Cascadia Subduction Zone may have triggered most of the major quakes on the northern San Andreas during at least the past 3,000 years or so. The evidence also shows the rupture direction going from north to south in each of these time-correlated events. The
1906 San Francisco Earthquakeseems to have been a major exception to this correlation, however, as it was not preceded by a major Cascadia quake, and the rupture moved mostly from south to north. [ [http://www.sciencedaily.com/releases/2008/04/080403131923.htm Science Daily, April 3, 2008] ]
The volcanoes within the subduction zone include:
Mount St. Helens
Medicine Lake Volcano
1700 Cascadia earthquake
Geology of the Pacific Northwest
North Cascades National Park
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