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・ 2001 New York Mets season
・ 2001 New York Underground Film Festival
・ 2001 New York Yankees season
・ 2001 New Zealand National Soccer League
・ 2001 New Zealand NBL season
・ 2001 New Zealand rugby league season
・ 2001 New Zealand rugby union tour
・ 2001 New Zealand Warriors season
・ 2001 NFL draft
・ 2001 NFL Europe season
・ 2001 NFL season
・ 2001 NHK Trophy
・ 2001 NHL Entry Draft
・ 2001 Nights
・ 2001 Nippon Professional Baseball season
2001 Nisqually earthquake
・ 2001 NLL season
・ 2001 Nobel Peace Prize
・ 2001 Nokia Brier
・ 2001 Nokia New Zealand Film Awards
・ 2001 Nordic Figure Skating Championships
・ 2001 North Carolina Tar Heels football team
・ 2001 North Dakota Fighting Sioux football team
・ 2001 North Indian Ocean cyclone season
・ 2001 North Queensland Cowboys season
・ 2001 Northeast Conference Men's Basketball Tournament
・ 2001 Northern Ford Premiership
・ 2001 Northern Illinois Huskies football team
・ 2001 Northwestern Wildcats football team
・ 2001 Norwegian Figure Skating Championships


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2001 Nisqually earthquake : ウィキペディア英語版
2001 Nisqually earthquake

The Nisqually earthquake (also commonly referred to as "The Ash Wednesday Quake") was an intraslab earthquake, occurring at 10:54 am PST (18:54 UTC) on February 28, 2001. One of the largest recorded earthquakes in Washington state history, it measured 6.8 on the moment magnitude scale and lasted approximately 45 seconds. The epicenter of the earthquake was Anderson Island, about northeast of Olympia. The focus was at a depth of . Tremors were felt as far away as Scio, Oregon, across the border in Vancouver, British Columbia, Canada, and east in Pasco, Washington. There were also reports that it was felt as far away as Spokane, Washington and Sandpoint, Idaho.
The quake caused some property damage in Seattle and surrounding areas. Although there were no reports of deaths directly from the earthquake, local news outlets reported that there was one death from a heart attack at the time of the earthquake.〔
==Geological origins==
The Puget Sound area, where this earthquake occurred, is prone to deep earthquakes due to the Juan de Fuca tectonic plate's subduction under the North American Plate at 3.5 to 4.5 cm. a year as part of the Cascadia subduction zone, which causes stress in the former as it sinks into the mantle. As an intraslab earthquake, it was produced by a change in volume as rock changed from one form to another. Similar significant earthquakes occurred in the same general region on April 29, 1965 (magnitude 6.5, depth ), and April 13, 1949 (magnitude 7.1, depth ).

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