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United States

地震帯: High North America
総地震回数
2,709
最大マグニチュード
4.9
地震帯
High

United StatesはNorth Americaに位置し、Highの地震リスク分類に指定されています。同国の地震史では合計2709回の地震が記録されています。 同国で記録された最大の地震はマグニチュード4.9に達しました。 人口340,110,988人、国土面積9,525,067 km²の同国では、地震が社会基盤と公共安全に重大な影響を及ぼす可能性があります。

地震概要

The United States sits astride some of the most geologically complex and hazardous terrain on Earth, exposing virtually every populated coastal and inland region to some degree of seismic risk. Three major tectonic systems dominate the picture. Along the Pacific Coast, the boundary between the North American Plate and the Pacific Plate creates the right-lateral [[fault]] system anchored by the 1,300-kilometre San Andreas Fault in California. To the north, the Cascadia [[subduction-zone]] carries the Juan de Fuca Plate beneath Oregon, Washington, and British Columbia in a slow-motion collision that builds stress toward rare but catastrophic megathrust ruptures. In the continental interior, ancient rift structures buried beneath thick sediments — most notably the New Madrid Seismic Zone in the central Mississippi Valley — remind geologists and emergency managers that seismic hazard is not confined to plate edges. Alaska occupies a separate seismic world, sitting squarely on the Pacific Ring of Fire where the Pacific Plate dives beneath North America and the Aleutian Arc curves westward for more than 3,000 kilometres. Hawaii faces a different hazard entirely, generated by hotspot volcanism rather than plate boundary friction.

The historical record of major earthquakes on United States soil is both long and sobering. The New Madrid sequence of 1811 and 1812 produced three events likely exceeding [[magnitude]] 7.5, temporarily reversing flow in the Mississippi River and ringing church bells as far away as Boston. The 1906 San Francisco earthquake (magnitude 7.9) killed between 3,000 and 6,000 people and destroyed much of the city through both shaking and subsequent fire; the [[epicenter]] lay near the offshore segment of the San Andreas Fault, which ruptured nearly 480 kilometres. Alaska delivered the second-largest earthquake ever recorded on instruments when the Good Friday earthquake struck Prince William Sound on 28 March 1964 at magnitude 9.2, generating a [[tsunami]] that killed people as far south as California and Oregon and levelling the coastal town of Valdez. The 1971 San Fernando earthquake (magnitude 6.6) prompted sweeping reforms to California's building codes after hospital collapses killed patients. The 1989 Loma Prieta earthquake (magnitude 6.9) killed 63 people during evening rush hour on the San Francisco Bay Area's infrastructure. The 1994 Northridge earthquake (magnitude 6.7) caused 57 deaths and over 20 billion dollars in damage, exposing critical weaknesses in steel-frame construction. More recently, the 2011 Virginia earthquake (magnitude 5.8) was felt by more people simultaneously than any other quake in U.S. history owing to the efficiency with which seismic waves travel through old, cold Eastern crust. Washington State faces a once-every-200-to-500-year Cascadia megathrust threat capable of producing magnitude 8.5 to 9.2 ruptures and catastrophic [[tsunami]]s along the entire Pacific Northwest coast.

The tectonic architecture of the contiguous United States reflects the assembly and subsequent deformation of the North American continent over hundreds of millions of years. The ancient Precambrian craton of the continental interior — stable basement rock more than one billion years old — forms the relatively aseismic heartland of the country. Around this stable nucleus, younger orogenic belts record successive phases of mountain building along former plate margins. The Rocky Mountains reflect Laramide-era compression; the Basin and Range province records ongoing extension as the continent is being pulled apart between the Colorado Plateau and the Sierra Nevada, producing a landscape of alternating mountain ranges and valleys riddled with normal [[fault]]s. The Pacific Plate boundary is one of the most intensively monitored [[fault]] systems in the world, tracked by the Southern California Seismic Network, the Pacific Northwest Seismic Network, and the USGS Advanced National Seismic System. The [[early-warning]] system ShakeAlert now delivers alerts ahead of damaging [[seismic-wave]]s to millions of residents in California, Oregon, and Washington, providing seconds to tens of seconds of warning before strong shaking arrives.

最近の地震

規模 場所 時刻
2.0 12 km WSW of Stanton, Texas 42分 前
1.7 16 km SSW of Jal, New Mexico 1時間, 31分 前
1.5 9 km S of Westbrook, Texas 1時間, 53分 前
1.5 13 km SSW of Jal, New Mexico 2時間, 13分 前
1.8 13 km SSW of Jal, New Mexico 5時間, 7分 前
1.6 13 km SSW of Jal, New Mexico 7時間, 38分 前
1.2 20 km NW of Stanton, Texas 16時間, 48分 前
1.1 19 km NW of Stanton, Texas 16時間, 48分 前
1.9 14 km SSW of Jal, New Mexico 18時間, 14分 前
2.0 13 km SSW of Jal, New Mexico 18時間, 37分 前

Earthquakes Near Major Cities in United States

よくある質問

United States is located in a high seismic risk zone, meaning earthquakes are frequent and can be destructive. A total of 2,709 earthquakes have been recorded in United States's seismic history.

The largest recorded earthquake in United States had a magnitude of 4.9. Earthquakes of this size can cause significant damage depending on depth, location, and local building standards.

United States has had 2,709 recorded earthquakes. This count includes events of all magnitudes detected by seismic monitoring networks. The actual number of earthquakes may be higher, as smaller events can go undetected.

United States is classified in the "High" seismic zone, located in North America. Seismic zones indicate the relative level of earthquake hazard based on historical activity, geological conditions, and proximity to tectonic plate boundaries.

地震の最中は「まず低く、頭を守り、動かない」。丈夫な机やテーブルの下に入り、頭と首を守り、揺れが収まるまで動かないでください。窓や重い物体から離れてください。地震の後は、怪我がないか確認し、余震に備えてください。

国の地震リスクは、プレート境界への近接性、歴史的な地震活動(過去の地震の頻度とマグニチュード)、地質条件、地震帯の人口密度、建築基準法の施行状況など、複数の要因を用いて評価されます。QuakeFYIはこれらの要因に基づき、0(リスクなし)から4(非常に高い)までの地震帯を割り当てています。

地震帯とは、地震の危険度によって分類された地理的領域です。ゾーン0はリスクが無視できる程度、ゾーン1は低リスク、ゾーン2は中程度のリスク、ゾーン3は高リスク、ゾーン4は非常に高いリスクを示します。これらのゾーンは、歴史的な地震データ、テクトニクスの状況、地質条件によって決定されます。

環太平洋火山帯(リング・オブ・ファイア)沿いの国々が最も多くの地震を経験しています。日本、インドネシア、チリ、フィリピン、イランは常に最も高い地震活動を記録しています。アメリカ合衆国(特にアラスカとカリフォルニア)、トルコ、メキシコも地震活動が非常に活発な国々です。

人口密度が高いと、より多くの人々やインフラが潜在的な被害にさらされるため、地震リスクが増大します。人口密集都市でのマグニチュード7.0の地震は数千人の犠牲者を出す可能性がありますが、無人地帯で同じ地震が発生しても被害は生じないかもしれません。建築基準法と防災対策は、人口密集地域のリスクを大幅に低減します。

地震密度は、国土面積に対する地震活動の集中度を測定するもので、1,000平方キロメートルあたりの地震回数で表されます。地震密度が高いことは、単位面積あたりの地震活動が頻繁であることを示し、異なる面積の国々間で地震リスクを比較するのに役立ちます。

地震指標

地震密度
0.28
1,000 km²あたりの地震回数
地震暴露度
7.97
百万人あたりの地震回数

近隣の地震活動

年別サマリー

地震の安全対策

United Statesは高い地震リスクゾーンに位置しています。地震への備えが強く推奨されます。

  • 揺れの際は「伏せて、隠れて、つかまる」を実行
  • 水、食料、救急用品を備えた非常用持ち出し袋を準備
  • 各部屋で窓や重い物から離れた安全な場所を確認
  • 沿岸部にいる場合は津波避難経路を確認