Historical tsunamis · Jan 28, 2020, 7:10 PM UTC

2020 Off SE Coast of Cuba tsunami

Cuba

The tsunami of Jan 28, 2020, 7:10 PM UTC originated near Off SE Coast of Cuba (Cuba).

Key facts

Date
Jan 28, 2020, 7:10 PM UTC
Cause
Earthquake
Magnitude
M7.7
Depth
15 km
Maximum documented water height
0.11 m
Houses destroyed
1
Damage
moderate (about US$ 1–5 million)
Observation records
2
Countries affected
2

It was triggered by a magnitude 7.7 earthquake at a depth of 15 km.

The highest documented water height was 0.11 m (George Town, Cayman Islands (UK Territory)).

2 observation sites in 2 countries are recorded.

Outside the source country, the earliest documented arrival was at George Town (Cayman Islands (UK Territory)) after 0:11 h.

Houses destroyed: 1.

Damage is estimated at moderate (about US$ 1–5 million).

Map of observation sites

2

Each dot is a documented observation site; colour and size show the observed water height. The triangle marks the source.

Tsunami arrival times

Documented arrival times from the NOAA/NCEI database, showing the earliest recorded location per country. Coverage is incomplete: a country without an entry was not necessarily spared.

  1. 0:00 hEarthquake (origin) · Jan 28, 2020, 7:10 PM UTC
  2. 0:11 hCayman Islands (UK Territory) · George Town · 0.11 m

1 places with a documented arrival time

Observations by country

CountryObservation recordsMaximum documented water heightDeathsEarliest arrival
Cayman Islands (UK Territory)10.11 m
George Town
—0:11 h
Mexico1———

Highest documented water heights

2 / 2

Individual documented observations for this event. Heights come from different measurement types and sources; not every location has a measured height.

Location / stationObserved heightDistance from sourceCountry
George Town0.11 m276 kmCayman Islands (UK Territory)
Puerto Morelos · Quintana Roo—863 kmMexico

Source: NOAA National Centers for Environmental Information (NCEI), Global Historical Tsunami Database. Confirmed events only. Deaths and damage are database estimates; older records are incomplete. Water heights come from different types of observation.