Terremoto moderado mag. 4.3 - Norwegian Sea, 561 km SSW of Longyearbyen, Spitsbergen, Svalbard, miércoles, 13 ene. 2021 -

Terremoto moderado mag. 4.3 - Norwegian Sea, 561 km SSW of Longyearbyen, Spitsbergen, Svalbard, miércoles, 13 ene. 2021

Terremoto moderado magnitud 4.3 at 10 km depth

13 Jan 22:56 UTC: Primero en informar: GFZ después de 9 minutos.
14 Jan 06:48: Ubicación del epicentro corregida 35 km (22 mi) al O.
Fecha & hora: 13 Jan 2021 22:47:34 UTC -
Hora local al epicentro: miércoles, 13 ene 2021 23:47 (GMT +1)
Magnitud: 4.3
Profundidad: 10.0 km
Epicentro latitud / longitud: 73.61°N / 7.12°E (Norwegian Sea, Svalbard y Jan Mayen)
Nearby towns and cities:
543 km al SSO de Sveagruva (pop: 300) --> ¡Vea sismos cercanos!
561 km al SSO de Longyearbyen (pop: 2,060) --> ¡Vea sismos cercanos!
587 km al NNO de Gryllefjord (Noruega) (pop: 439) --> ¡Vea sismos cercanos!
591 km al NO de Ersfjord (Noruega) (pop: 306) --> ¡Vea sismos cercanos!
603 km al NO de Tromsø (Noruega) (pop: 52,400) --> ¡Vea sismos cercanos!
640 km al NO de Lyngseidet (Noruega) (pop: 821) --> ¡Vea sismos cercanos!
646 km al NO de Storsteinnes (Noruega) (pop: 890) --> ¡Vea sismos cercanos!
Weather at epicenter at time of quake:
Overcast Clouds -0.6°C (31 F), humidity: 91%, wind: 5 m/s (10 kts) from WNW
Fuente primaria de datos: GFZ (German Research Centre for Geosciences)
Energía liberada estimada: 1.8 x 1011 joules (49.4 megawatt hours, equivalent to 42.5 tons of TNT) More info
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Data for the same earthquake reported by different agencies

Info: The more agencies report about the same quake and post similar data, the more confidence you can have in the data. It takes normally up to a few hours until earthquake parameters are calculated with near-optimum precision.
MagnitudProfundidadUbicaciónFuente
M 4.310 kmGreenland Sea, Svalbard & Jan MayenGFZ
M 4.410 km4.4 GREENLAND SEA, Svalbard & Jan MayenEMSC

User reports for this quake

User reports estimate the perceived ground shaking intensity according to the MMI (Modified Mercalli Intensity) scale.
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