Tsunamis in 1861

February 16, 1861 Tsunami: SW. Sumatra, Indonesia

February 16, 1861 · 7 m · 1,105 deaths · Definite tsunami

A tsunami caused by a magnitude 8.5 earthquake began at SW. Sumatra, Indonesia on February 16, 1861. The water rose as high as 7 meters. Its effects were recorded at 17 places. It killed 1,105 people.

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

Tsunami warnings in force

The tsunami

Date
February 16, 1861
Source
SW. Sumatra, Indonesia
Cause
Earthquake
Maximum water height
7 m (23.0 ft)
Runups recorded
17
Tsunami intensity (Soloviev-Imamura)
3
Waters
Ocean
How certain
Definite tsunami
Source location
1.000° S, 97.500° E

The toll

Deaths
1,105
Damage
Moderate (about $1 to $5 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.

Ref #414:

1861, Feb 16 about 19:00 [local Time], 1 S, 97.5 E, depth 70 km, magnitude 8.5 MS. There was an earthquake of exceptional strength and great duration, accompanied by a tsunami, on the entire western coast of Sumatra.

A seaquake was felt by the American ship "Humboldt" at the latitude of the Pagai Islands. At Singapore, the oscillations lasted 2 minutes; cases of sea sickness were observed. The earthquake...was felt at Dacca and caused seiches in ponds on the east of India. An unusual trembling of level, ascribed by A. Wagner to this earthquake, was noted at the Pulkovo astronomical observatory during observations of 16.II.1861.

At Ajerbangis, the sea became agitated during the earthquake. From time to time, the river dried up completely, and then the sea "rushed" on shore, advancing with great force. These oscillations in the level of the river repeated until noon on the 17th; the duration of one oscillation was 15 minutes.

At Pulu Tello, seven hundred residents drowned.

At Singkel, about 20 people died.

At Fort Laundi, on the south coast of Nias Island, about 50 people died.

At Gunugsitoli on the northeastern shore of Nias island, many local residents died.

Lapau island, to the north of Nias Island, was almost completely destroyed. Hundreds of residents died.

On the coast of Atjeh, the water rose 1 1/2 m. According to other sources, the entire coast of Atjeh was devastated as a result of a sudden invasion of the sea, which penetrated inland, uprooted trees, destroyed crops and homes, and in retreating carried off a multitude of residents. In Analaboo port alone, 135 people drowned.

Ref #42:

1861, Feb 16. Sumatra. A wave of great force reported from Anjer Bangis and the south coast of Pulau Nias and Padang. The Pulau Pulau Batu (Batu Islands 0ol0'S, 98o25'E) were inundated. The wave was noted by several vessels at sea, (Heck, 1947).

Ref #132:

1861, Feb 16. Sumatra. A tidal wave of great force at Anjer Bangis. Great wave on south coast of Nias Island. Batu Island inundated. Some damage at other islands. Strong at Padang. Wave noted by several vessels at sea.

Ref #1188:

1861, Feb 16. Tsunami was observed at Singkil, Nias and Tello.

Ref #8795:

This earthquake appears to have taken place between the trench and the islands of the trench slope break, since the tsunami devastated towns on the seaward side of the Batu Islands, and a town on the southwest shore of Nias experienced a tsunami height of 7 m. Evidence for coseismic uplift exists on the north and west coasts of Nias, where piers of rock and reefs became exposed; a small island became connected to Nias. On Java, more than 1400 km away, seiches were reported in six different bodies of water, and the quake was felt as far as 1600 km from Nias.

Ref #2725:

the disturbance in the Malacca Strait [...] in 1861 started 5 h prior to the occurrence of the earthquake. Thus, the evidence for tsunami hazard to the Malacca Strait associated with earthquakes off the Indian Ocean coast of Sumatra is not compelling.

Every runup

Nearest the source first. Heights are above sea level at the time; a tide gauge reads half the wave’s full height.

WhereCountryKm from sourceWater height, mInland, mMeasured byFirst wave, UTCDeaths
Simuk Is. SumatraIndonesia111Eyewitness observation of water height
Palau Telo, SumatraIndonesia135Eyewitness observation of water height700
Batu Islands, SumatraIndonesia142Eyewitness observation of water height
Fort Laudi, Nias I., SumatraIndonesia1747Eyewitness observation of water height50
Pandjang (Panjang), SE. SumatraIndonesia241Eyewitness observation of water height
Ajerbangis, SumatraIndonesia248Eyewitness observation of water height
Natal, SumatraIndonesia249Eyewitness observation of water height
Gunungsitoli, Nias IslandIndonesia251Eyewitness observation of water height
Lapau Island, SumatraIndonesia278Eyewitness observation of water height200
Padang, SumatraIndonesia317Eyewitness observation of water height
Sibolga, SumatraIndonesia334Eyewitness observation of water height
Barus, SumatraIndonesia3471Eyewitness observation of water height
Singkil, SumatraIndonesia364Eyewitness observation of water height20
Analaboo, Sumatra, IndonesiaIndonesia5901.5Eyewitness observation of water height135
Bengkulu, SumatraIndonesia6121Eyewitness observation of water height
Banda Aceh (Atjeh Island), SumatraIndonesia759Eyewitness observation of water height
Krawang, JavaIndonesia1,2361.5Eyewitness observation of water height

More

Every tsunami in 1861The 1800sTsunamis of IndonesiaThe 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 904.