地震发生区域
国家地震灾害模型,2023 年
纽约市的地震
您知道自己生活在“地震带”吗?这是真 的。纽约市等地过去曾发生过地震,将来 还会发生。如果您感到地面在震动,请确 保知道怎么做:趴下、掩护和稳住!
如果您感觉到地面在震动
趴下 掩护 稳住
规模最大的地震 - 纽约市 - 1884年8月10日 - 震级 5.2
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地震发生区域
国家地震灾害模型,2023 年
纽约市的地震
您知道自己生活在“地震带”吗?这是真 的。纽约市等地过去曾发生过地震,将来 还会发生。如果您感到地面在震动,请确 保知道怎么做:趴下、掩护和稳住!
如果您感觉到地面在震动
趴下 掩护 稳住
规模最大的地震 - 纽约市 - 1884年8月10日 - 震级 5.2
地震发生区域
国家地震灾害模型,2023 年
纽约市的地震
您知道自己生活在“地震带”吗?这是真 的。纽约市等地过去曾发生过地震,将来 还会发生。如果您感到地面在震动,请确 保知道怎么做:趴下、掩护和稳住!
如果您感觉到地面在震动
趴下 掩护 稳住
规模最大的地震 - 纽约市 - 1884年8月10日 - 震级 5.2
CÁC TRẬN ĐỘNG ĐẤT XẢY RA Ở ĐÂU
Theo Mô Hình Cảnh Báo Nguy Hiểm Động Đất Toàn Quốc, 2023
ĐỘNG ĐẤT TẠI THÀNH PHỐ NEW YORK
CÁC TRẬN ĐỘNG ĐẤT XẢY RA Ở ĐÂU
Theo Mô Hình Cảnh Báo Nguy Hiểm Động Đất Toàn Quốc, 2023
ĐỘNG ĐẤT TẠI THÀNH PHỐ NEW YORK
ГДЕ БЫВАЮТ ЗЕМЛЕТРЯСЕНИЯ
Общенациональная модель сейсмической опасности 2023 г.
ЗЕМЛЕТРЯСЕНИЯ В НЬЮ-ЙОРКЕ
ГДЕ БЫВАЮТ ЗЕМЛЕТРЯСЕНИЯ
Общенациональная модель сейсмической опасности 2023 г.
ЗЕМЛЕТРЯСЕНИЯ В НЬЮ-ЙОРКЕ
LÀ OÙ LES SÉISMES SE PRODUISENT
Modèle de l’aléa sismique au niveau national, 2023
LES SÉISMES DANS LA VILLE DE NEW YORK
LÀ OÙ LES SÉISMES SE PRODUISENT
Modèle de l’aléa sismique au niveau national, 2023
LES SÉISMES DANS LA VILLE DE NEW YORK
DÓNDE SE PRODUCEN LOS TERREMOTOS
Modelo Nacional de Riesgo Sísmico, 2023
TERREMOTOS EN LA CIUDAD DE NUEVA YORK
DÓNDE SE PRODUCEN LOS TERREMOTOS
Modelo Nacional de Riesgo Sísmico, 2023
TERREMOTOS EN LA CIUDAD DE NUEVA YORK
KOTE GEN TRANBLEMANNTÈ
(Modèl risk tranblemanntè nan nivo nasyonal, 2023)
TRANBLEMANNTÈ NAN VIL NEW YORK
KOTE GEN TRANBLEMANNTÈ
(Modèl risk tranblemanntè nan nivo nasyonal, 2023)
TRANBLEMANNTÈ NAN VIL NEW YORK
TITLE: WHERE EARTHQUAKES OCCUR
MAP: National Seismic Hazard Model, 2023
HEADING: EARTHQUAKES IN NYC
TITLE: WHERE EARTHQUAKES OCCUR
MAP: National Seismic Hazard Model, 2023
HEADING: EARTHQUAKES IN NYC
This hazard map is a simplified 2% in 50-year probability of exceedance map for fixed VS30 760 m/s.
This hazard map is a simplified 2% in 50-year probability of exceedance map for fixed VS30 760 m/s.
Annual number of earthquakes with a magnitude of 3.0 or larger in the central and eastern United States, 1973–2022. The long-term rate of approximately 25 earthquakes per year increased sharply starting around 2009.
Annual number of earthquakes with a magnitude of 3.0 or larger in the central and eastern United States, 1973–2022. The long-term rate of approximately 25 earthquakes per year increased sharply starting around 2009.
Photograph of Mendenhall Postdoctoral Fellow and Research Geologist Sylvia R. Nicovich for their staff profile. Nicovich is looking into a hole in the ice.
Photograph of Mendenhall Postdoctoral Fellow and Research Geologist Sylvia R. Nicovich for their staff profile. Nicovich is looking into a hole in the ice.
From the 2003 NSHM by Mueller et al., 2010, the distribution of spectral acceleration (SA in %g) is shown for Puerto Rico and the U.S. Virgin Islands.
From the 2003 NSHM by Mueller et al., 2010, the distribution of spectral acceleration (SA in %g) is shown for Puerto Rico and the U.S. Virgin Islands.
Global view of three locations: Commonwealth of the Northern Mariana Islands (CNMI), Guam, and American Samoa. J.A. Herrick (2023)
Global view of three locations: Commonwealth of the Northern Mariana Islands (CNMI), Guam, and American Samoa. J.A. Herrick (2023)
EARTHQUAKES: WHAT YOU FEEL
EARTHQUAKE INTENSITY
EARTHQUAKES: WHAT YOU FEEL
EARTHQUAKE INTENSITY
Map showing distribution of average annualized earthquake loss by region. The high concentration of loss in California and the West Coast is consistent with that region’s high seismic hazard, significant population, and building exposure.
Map showing distribution of average annualized earthquake loss by region. The high concentration of loss in California and the West Coast is consistent with that region’s high seismic hazard, significant population, and building exposure.
Although most economic loss is concentrated along the west coast, the distribution of relative earthquake risk, as measured by the Annualized Earthquake Loss Ratio (AELR), is spread throughout the country and it reinforces the fact that earthquakes are a national problem.
Although most economic loss is concentrated along the west coast, the distribution of relative earthquake risk, as measured by the Annualized Earthquake Loss Ratio (AELR), is spread throughout the country and it reinforces the fact that earthquakes are a national problem.
The large HTHH volcanic explosion created fast low-frequency pressure waves that penetrated about 3.1 miles/5 kilometers into the shallow crust (shown in yellow). Wind and small explosions (shown in blue) create shorter pressure waves that only penetrate down about 328 feet/100 meters.
The large HTHH volcanic explosion created fast low-frequency pressure waves that penetrated about 3.1 miles/5 kilometers into the shallow crust (shown in yellow). Wind and small explosions (shown in blue) create shorter pressure waves that only penetrate down about 328 feet/100 meters.
The waveforms of the ground motion recording and the pressure sensor recording from a station with both types of instruments (see second image above) match up, indicating that the pressure waves are causing the ground (crust) to deflect.
The waveforms of the ground motion recording and the pressure sensor recording from a station with both types of instruments (see second image above) match up, indicating that the pressure waves are causing the ground (crust) to deflect.
GSN field engineers from the Albuquerque Seismic Lab visited the northernmost town in the world Longyearbyen (Svalbard, Norway) on their way north to GSN station IU-KBS for a station upgrade. GSN station IU-KBS is located in Svalbard, a Norwegian archipelago. Tyler Storm packs up for a shipment back home.
GSN field engineers from the Albuquerque Seismic Lab visited the northernmost town in the world Longyearbyen (Svalbard, Norway) on their way north to GSN station IU-KBS for a station upgrade. GSN station IU-KBS is located in Svalbard, a Norwegian archipelago. Tyler Storm packs up for a shipment back home.
GSN field engineers from the Albuquerque Seismic Lab visited the northernmost town in the world Longyearbyen (Svalbard, Norway) on their way north to GSN station IU-KBS for a station upgrade. GSN station IU-KBS is located in Svalbard, a Norwegian archipelago. This taxidermied polar bear was just inside the doors to the chow hall.
GSN field engineers from the Albuquerque Seismic Lab visited the northernmost town in the world Longyearbyen (Svalbard, Norway) on their way north to GSN station IU-KBS for a station upgrade. GSN station IU-KBS is located in Svalbard, a Norwegian archipelago. This taxidermied polar bear was just inside the doors to the chow hall.
GSN field engineers from the Albuquerque Seismic Lab visited the northernmost town in the world Longyearbyen (Svalbard, Norway) on their way north to GSN station IU-KBS for a station upgrade. GSN station IU-KBS is located in Svalbard, a Norwegian archipelago. Tyler Storm drilling a hole in the concrete pier for a new accelerometer installation.
GSN field engineers from the Albuquerque Seismic Lab visited the northernmost town in the world Longyearbyen (Svalbard, Norway) on their way north to GSN station IU-KBS for a station upgrade. GSN station IU-KBS is located in Svalbard, a Norwegian archipelago. Tyler Storm drilling a hole in the concrete pier for a new accelerometer installation.
In October 2022 GSN field engineers from the Albuquerque Seismic Lab visited the northernmost town in the world, Longyearbyen (Svalbard, Norway) on their way north to GSN station IU-KBS for a station upgrade. GSN station IU-KBS is located in Svalbard, a Norwegian archipelago.USGS contractor, Jared Anderson, relieving the bell jar pressure to remove STS-1 seismo
In October 2022 GSN field engineers from the Albuquerque Seismic Lab visited the northernmost town in the world, Longyearbyen (Svalbard, Norway) on their way north to GSN station IU-KBS for a station upgrade. GSN station IU-KBS is located in Svalbard, a Norwegian archipelago.USGS contractor, Jared Anderson, relieving the bell jar pressure to remove STS-1 seismo