July 24, 1985 Tsunami: Ubekendt Island, Greenland
A tsunami caused by a magnitude 3 earthquake began at Ubekendt Island, Greenland on July 24, 1985 at 11:00 UTC. Its effects were recorded at 1 place.
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
Travel times
How long the first wave took to reach each part of the ocean, one line for each hour up to 24, estimated from the source and the depth of the sea.
The travel times are computed in your browser, which needs JavaScript.
- 1 to 4 hours
- 5 to 6 hours
- 7 to 14 hours
- 15 hours and more
Computed in your browser the way NOAA’s own travel time maps are: the wave travels at the square root of gravity times the depth, over NOAA’s ETOPO1 depths averaged to a 10 arc-minute grid. Checked against NOAA NCEI’s maps for 21 tsunamis over the first 24 hours, these lines fall within 10 minutes of NCEI’s at half the points compared and within 52 minutes at 9 in 10. They give when the first wave could arrive, not how high it is; bays, harbors and island chains finer than the grid can see it later. Not for use in a warning: see tsunami.gov.
The tsunami
- Date
- July 24, 1985, 11:00 UTC
- Source
- Ubekendt Island, Greenland
- Cause
- Earthquake
- Earthquake
- Magnitude 3
- Runups recorded
- 1
- Waters
- Ocean
- How certain
- Probable tsunami
- Source location
- 71.317° N, 52.250° W
The toll
The record gives no deaths, injuries or damage for this tsunami.
What the record says
NCEI’s account, from the sources it cites.
Reference #3935:
A light tremor felt by one person of two-person geological team, very shortly followed by at least four pulses of a small tsunami observed by three persons.
From letter from Michael W. Milner (Geologist): “As we went down to the beach, having signaled the outboard to pick us up and return us to the M/V MASIK, we witnessed the tide go out. I considered warning the boatman, but he was almost at the beach and had turned off the motor. The first wave carried him up onto the beach leaving him high and dry; the next wave brought him further . As we disliked the idea of trying to move the boat into the water after the oscillation ceased, we took advantage of the next two waves to free the boat , got in and went to the mother ship . We did not observe the waves after that as we quickly moved out to a distance where the waves seemed unimpressive. The time lapsed between the vibration and the tidal events, as recalled by my assistant upon our discussion regarding an earthquake versus an iceberg cause of the waves, was three minutes (probably a minimum time). I feel quite strongly that it was a tidal wave rather than a calving iceberg because I had experienced the latter at the previous stop in the fjord north and east from this site. The frequency of the waves from the calving berg was greater perhaps one every 3 or 5 seconds while that from the tidal wave was 10 to 15 seconds. The power boat had a draft of 3 dm. Probably the wave carried it two or three times that distance vertically onto the sandy delta….”
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 |
|---|---|---|---|---|---|---|---|
| Ubekendt Island | Greenland | 54 | Eyewitness observation of water height |
More
Every tsunami in 1985The 1900sTsunamis of GreenlandThe earthquakeThis 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 6150.