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Sismo minore mag. 1.3 - Northern Colombia, lunedì, 30 gen 2023 09:41 (GMT -5) -

Sismo minore magnitudine 1.3 a 19 km di profondità

30 Jan 20:28 UTC: Primo a segnalare: RaspberryShake dopo 6 ore.

Dettagli del sismo

Data e ora	30 Jan 2023 14:41:31 UTC -
Ora locale all'epicentro	lunedì, 30 gen 2023 09:41 (GMT -5)
Status	Confermato
Magnitudine	1.3
Prof.	19.0 km
Epicentro latitudine / longitudine	7.193°N / 75.847°W (Colombia)
Antipodo	7.193°S / 104.153°E
Intensità di scuotimento	Non sentito
Sentito
Fonte dati primaria	RaspberryShake (RaspberryShake)
Vulcano più vicino	San Diego (198 km / 123 mi)
Luoghi vicini	9 km ONO da Ituango (pop: 10,800) \| Mappa \| Sismi nelle vicinanze 37 km NNO da San Andres (pop: 3,150) \| Mappa \| Sismi nelle vicinanze 51 km ENE da Dabeiba (pop: 11,500) \| Mappa \| Sismi nelle vicinanze 54 km ONO da Yarumal (pop: 22,400) \| Mappa \| Sismi nelle vicinanze 99 km SSO da Montelibano (pop: 85,000) \| Mappa \| Sismi nelle vicinanze 100 km NNO da Bello (pop: 392,900) \| Mappa \| Sismi nelle vicinanze 115 km SE da Apartado (pop: 86,400) \| Mappa \| Sismi nelle vicinanze 347 km NO da Bogotá (pop: 7,674,400) \| Mappa \| Sismi nelle vicinanze
Meteo all'epicentro al momento del sismo
Energia sismica rilasciata stimata	5.6 x 10⁶ joules (1.56 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
1.3	19 km	Northern 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: 117 km / 73 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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