May 7, 2007 Tsunami: Black Sea, Bulgaria
A tsunami caused by a landslide began at Black Sea, Bulgaria on May 7, 2007. The water rose as high as 3 meters. Its effects were recorded at 2 places.
Where the waves reached
The source (white) and every runup with a place, colored by the water height recorded there. A ring is a runup NCEI marks doubtful.
- Under 1 m
- 1 to 3 m
- 3 to 10 m
- 10 to 30 m
- 30 m and more
- Height not recorded
The tsunami
- Date
- May 7, 2007
- Source
- Black Sea, Bulgaria
- Cause
- Landslide
- Maximum water height
- 3 m (9.8 ft)
- Runups recorded
- 2
- Waters
- Ocean
- How certain
- Questionable tsunami
- Source location
- 43.000° N, 29.000° E
The toll
- Damage
- Limited (under about $1 million)
Where the literature gives no number, NCEI records a description on a scale of 1 to 4, printed here in its words. Damage is in millions of US dollars of the year of the event, not adjusted for inflation.
What the record says
NCEI’s account, from the sources it cites.
A tsunami-like sea disturbance of nonseismic origin
was observed on 7 May 2007 on the Bulgarian Black Sea
coast. The maximum wave amplitude was three meters, and
the sea oscillations lasted for several hours. The anomalous
behaviour was seen in many places of the coast of Bulgaria
and was stronger in the north. Several accounts of
eyewitnesses as well as reports of local port authorities
and three tide-gauge recordings are available and have been
collected and analysed. The tsunami could have been
produced by a submarine landslide or by atmospheric
pressure pulses. Here, we explore the former hypothesis,
i.e., the possibility that the tsunami was induced by a
landslide that may have occurred on the shelf margin off
Bulgaria. By making use of numerical modelling we find
that submarine mass movements taking place within a
certain delimited source area off Bulgaria may have
generated tsunamis compatible with the observations... The anomalous behaviour of the sea started around 9:00-9:30 am (Local Time) on 7 May 2007 and lasted with progressive attenuation for about 5 hours. Direct observations were made mostly in the two biggest towns of the coast - Balchik and Kavarna (about 13000 inhabitants each). The port authorities reported similar effects to the north, near Kaliakra cape and the village of Shabla. Slightly more to the south, the observations were documented by observers at the Varna port and the Galata oil and gas platform. The oscillations were recorded by two sea level analogue mareographs, one in Varna and one in Ahtopol (the southernmost point of the Bulgarian Black Sea coast) operated by NIGiF (Scientific Research for Geodesy and Photogrammetry, Sofia).
The tsunami caused only slight damage in the affected
areas. In Kavarna, a 25-30 ton tourist boat was rotated
violently according to his captain and was damaged near the
anchor holes and in some other parts, including the rudder.
Many small fishing boats were cast onto the beach in
Kavarna and Balchik Marinas. Debris was deposited on
the shore. Some large tetrapodes (1.2 tons each) fell into the sea from the breakwater of the Kavarna Harbour.
(above from reference #4176)
Every runup
Nearest the source first. Heights are above sea level at the time; a tide gauge reads half the wave’s full height.
| Where | Country | Km from source | Water height, m | Inland, m | Measured by | First wave, UTC | Deaths |
|---|---|---|---|---|---|---|---|
| Kavarna | Bulgaria | 70 | 0.9 | Eyewitness observation of water height | |||
| Balchik | Bulgaria | 81 | 1.2 | Eyewitness observation of water height |
More
Every tsunami in 2007The 2000sTsunamis of BulgariaThis day in weather historyAlerts in force
Sources
Tsunami events and runups from NOAA’s National Centers for Environmental Information, Global Historical Hazard Database, cited as NCEI/WDS, doi:10.7289/V5PN93H7. Public domain. Read 2026-09-24. NCEI tsunami event 4311.