On February 28, 2001 at 10:54 a.m., the Capitol shook from the seismic power of the 6.8 magnitude Nisqually earthquake. The magnitude of hydrologic response to earthquakes is inherently site-specific due to local geological conditions such as the presence of unconsolidated or liquefiable deposits. Quite the same Wikipedia. February 28, 2001: The Nisqually Earthquake, at 6.8 magnitude, was centered to the south in Nisqually, but caused some structural damage all the way in Seattle. Produced by Michael B. Fearnehough. Documentary of impacts to the Seattle area following a 6.8 magnitude earthquake later named the Nisqually Earthquake. The magnitude 6.8 quake brought down brick facades, damaged Seattle’s waterfront viaduct and split the Capitol dome in Olympia. The Nisqually Earthquake shook much of western Washington State on the morning of February 28, 2001, and caused widespread damage, much of which resulted from ground failure. The 6.8 magnitude Nisqually earthquake shook the Pacific Northwest on February 28, 2001 at 10:54 a.m. Shallow events are black. It was centered about 11 miles north of Olympia.

The 2001 Nisqually earthquake was a large magnitude (6.8 Mw) quake that yielded relatively mild ground shaking. April 29, 1965: A 6.5 magnitude, deep earthquake in the south Sound area was felt as far away as Montana and British Columbia, and knocked down thousands of chimneys in the Puget Sound. Centered a mere 17.8 kilometers northeast of Olympia, at a depth of 52 kilometers, the earthquake caused considerable damage to the Legislative Building and surrounding structures.

California’s 1994 Northridge earthquake had a similar moment magnitude (6.7 Mw) but was only 18 … This event, named the Nisqually earthquake for a river delta near its epicenter at the southern end of Puget Sound, was actually slightly larger than the Northridge earthquake. The 2001 Nisqually earthquake occurred at 10:54:32 local time on February 28, 2001. The Nisqually mainshock was followed by There was more shaking in the Northridge earthquake because the earthquake occurred closer to the surface (3-11 miles), as opposed to the Nisqually earthquake's deeper hypocenter (30-36 miles). If you were in Western Washington on Feb. 28, 2001, chances are you remember what you were doing that morning.

2001 Nisqually earthquake. The biggest surprise about the Nisqually earthquake was that it wasn’t worse.

But our findings indicate that local near-surface strain and response to strong ground shaking can explain streamflow response to the Nisqually earthquake. 2001-02-28 18:54:32 (UTC) | 47.149°N 122.727°W | 51.8 km depth The fact that a relatively mild earthquake can yield such significant losses may be the most important lesson Nisqually … Magnitude is expressed in whole numbers and decimal fractions. At 10:54 a.m., there was a magnitude 6.8 … The Nisqually quake was the last major earthquake to strike the area, which has researchers concerned. Image showing the location and depth of the Northridge and Nisqually earthquakes.

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