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Sismo minore mag. 0.9 - Colombia, lunedì, 30 gen 2023 09:29 (GMT -5) -

Sismo minore magnitudine 0.9 a 38 km di profondità

30 Jan 20:16 UTC: Primo a segnalare: RaspberryShake dopo 6 ore.

Dettagli del sismo

Data e ora	30 Jan 2023 14:29:19 UTC -
Ora locale all'epicentro	lunedì, 30 gen 2023 09:29 (GMT -5)
Status	Confermato
Magnitudine	0.9
Prof.	38.0 km
Epicentro latitudine / longitudine	5.726°N / 75.886°W (Colombia)
Antipodo	5.726°S / 104.114°E
Intensità di scuotimento	Non sentito
Sentito
Fonte dati primaria	RaspberryShake (RaspberryShake)
Vulcano più vicino	Romeral (82 km / 51 mi)
Luoghi vicini	8 km N da Andes (pop: 16,400) \| Mappa \| Sismi nelle vicinanze 21 km SE da Ciudad Bolivar (pop: 16,200) \| Mappa \| Sismi nelle vicinanze 49 km SO da Caldas (pop: 65,600) \| Mappa \| Sismi nelle vicinanze 60 km SSO da Envigado (pop: 163,000) \| Mappa \| Sismi nelle vicinanze 60 km SSO da Itagui (pop: 281,900) \| Mappa \| Sismi nelle vicinanze 69 km SSO da Medellín (pop: 2,000,000) \| Mappa \| Sismi nelle vicinanze 84 km NNO da Manizales (pop: 357,800) \| Mappa \| Sismi nelle vicinanze 235 km ONO da Bogotá (pop: 7,674,400) \| Mappa \| Sismi nelle vicinanze
Meteo all'epicentro al momento del sismo
Energia sismica rilasciata stimata	1.4 x 10⁶ joules (0.392 kWh) \| about seismic energy

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Data for the same earthquake reported by different agencies

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Mag.	Prof.	Ubicazione	Fonte
0.9	38 km	Colombia	RaspberryShake

Most recent quakes Top 20 past 24 hrs Terremoti in Colombia

Seismograms

Seismic station: Santa Helena, Medellin, Colombia (HEL/CM network) | Distance from quake: 65 km / 40 mi | Show on map | Station Info

Seismic station Santa Helena, Medellin, Colombia: vertical movement plot around time of quake (source: IRIS/BUD)

Seismogram (vertical component) around time of quake. Thin dotted red line indicates time of quake. Seismic waves arrive some time later, depending on distance. Bandpass filter applied: 0.5-10.0 Hz. Source: IRIS Buffer of Uniform Data (BUD) webtool

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User reports for this quake

Terremoti di questa magnitudo non possono essere normalmente percepiti dagli esseri umani, ma sono registrati dai moderni sismometri.

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