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Santorini Volcano

Updated: May 1, 2025 17:25 GMT -
Caldera (complex stratovolcano)
Cyclades, Greece, 36.4°N / 25.4°E
Summit height: 329 m (on caldera rim) / 128 m (top of most recent lava shield, Nea Kameni)
Current status: restless (2 out of 5)
Last update: 26 Feb 2025
View of the caldera of Santorini from Fira town, with the young volcanic island of Nea Kameni in the background.
View of the caldera of Santorini from Fira town, with the young volcanic island of Nea Kameni in the background.

Santorini is a volcanic Island group at the central south end of the Cyclades in the Aegean Sea (Greece). As a popular tourist destination in Greece, it is renowned for its spectacular sea-filled volcanic caldera sourrounded by steep colorful cliffs, the beauty of its villages and fields.

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Typical eruption style: Dominantly explosive, with effusive activity during intervals. Powerful explosive, so-called Plinian eruptions appear to occur every 10-30,000 years. Construction of lava shields and minor to irregularly spaced subplinian explosive activity during interval times.
Santorini volcano eruptions: 1613 BC +-7 years (the so-called "Minoan eruption", one of the largest plinian eruptions during the past 10,000 years on earth)
historic eruptions: 197 BC, 46/47 AD, 726, 1570-1573, 1707-1711, 1866-1870, 1925-1928, 1939-1941, 1950

Latest nearby earthquakes

Date and TimeMag / DepthDistance / Location
May 1, 07:45 pm (GMT +3)
2.4

35 km
27 km (17 mi) to the NE Aegean Sea, 23 km northeast of Santorini Island, Cyclades, South Aegean, Greece Info
May 1, 02:36 pm (GMT +3)
1.8

5.5 km
29 km (18 mi) to the NE Santorini Isl. - S. Greece Info
May 1, 02:35 pm (GMT +3)
1.9

7.2 km
29 km (18 mi) to the NE 26 km ENE From Oia Info
May 1, 09:17 am (Universal Time)
2.0

10 km
28 km (18 mi) to the NE Aegean Sea, 22 km southeast of Ios Island, Cyclades, South Aegean, Greece Info
May 1, 09:43 am (GMT +3)
1.7

10 km
28 km (17 mi) to the NE Santorini Isl. - S. Greece Info
May 1, 02:55 am (Universal Time)
0.0

3.1 km
14 km (8.9 mi) to the NE Santorini Isl. - S. Greece Info
May 1, 05:01 am (GMT +3)
1.8

7.3 km
29 km (18 mi) to the NE Santorini Isl. - S. Greece Info
Wednesday, April 30, 2025 GMT (1 quake)
Apr 30, 07:29 pm (Universal Time)
2.3

29 km
19 km (12 mi) to the S Santorini Isl. - S. Greece Info
Saturday, April 26, 2025 GMT (1 quake)
Apr 26, 12:53 pm (Athens)
2.4

10 km
16 km (10 mi) to the N Santorini Isl. - S. Greece Info

Background

The island group of Santorini is the most well-known and active volcanic centre of the Hellenic Volcanic Arc in the south Aegean Sea. It is a very complex stratovolcano dominated by a large, sea-flooded caldera created by several large explosive eruptions. The different products of about 2 million years of volcanic activity have accumulated around a small non-volcanic basement, that once formed a small island similar to the other cycladic islands. Most of the volcanic layers are visible in the multi-colored sequences of the impressive steep inner walls of the caldera, striking the visitor who reaches the island by boat.The last eruption took place in an phreatic eruption on Nea Kameni island in 1950.

The Minoan Eruption
Santorini's volcanic activity during the past 2-500,000 years has been dominated by very large explosive eruptions at intervals of few tens of thousands of years. The most recent of this type occurred at around 1613 BC and is known as the so-called Minoan eruption. The late Bronze Age eruption, one of the biggest known volcanic explosions in younger time,- and one of the most studied, but still most mysterious eruptions of all time-, devastated not only Santorini, but had a deep impact on the whole of the Eastern Mediterranean. Perhaps it even had serious world-wide effects and changed history.
Still today, one can see its deposits, the characteristic, tens of meters thick layer of white pumice and ash that blankets most of the surface of the island group. The eruption changed the shape of the island itself dramatically: it is now believed that before the eruption, it had the shape of an almost complete ring that enclosed an earlier, shallower caldera. Then, large sections of island collapsed into the emptied magma chamber after the eruption, literally disappearing under the sea. The ring-island was breached to the W and NW, and the caldera was significantly widened and deepened.
The Minoan eruption devastated the rich, highly developed economic center, that Santorini was at that time. Since 1969, intense archaeological excavations have brought to light an important Cycladic/Minoan town which had been buried beneath the volcanic ash for almost 4000 years. Although it appears that people had time to evacuate their island in time before the eruption, carrying most of their goods with them, the findings from Akrotiri are impressive: especially, they include well-preserved and magnificent wall paintings, ceramics and other objects. Thanks to the work of numerous archaeologists, a new light was thrown on an important prehistoric period and culture. The spectacular discovery even induced continuing speculations that relate the volcanic destruction of Santorini to the legend of the sunken Atlantis.

The historic eruptions of Santorini volcano (Palea and Nea Kameni)
Although at present dormant, Santorini has been active several times in historic time. Since its last major explosive eruption (at about 1645 BC) numerous minor and medium-sized, mainly effusive eruptions have occurred. This activity built the dark-colored islands of Nea and Palea Kameni inside the caldera. Their first appearance was witnessed and reported by Greek and Roman writers. The last eruption on Nea Kameni occurred in 1950. At present, Santorini is dormant, and volcanism manifests as fumarolic activity and hot springs around the islands.

Santorini Volcano Photos

Significant volcanic eruptions: Santorini volcano

In the past 10,000 years, Santorini has had at least 12 confirmed volcanic eruptions, out of which 11 are documented by historical records, while the others can be inferred from geological evidence.
There is one uncertain or discredited eruption in 19 AD from Santorini volcano.
The table below lists all known eruptions (date in bold face) of Santorini volcano since around 2000 BC. Updates on the most recent volcanic activity of Santorini can be found on the news page of Santorini volcano.
DateNoteVEIDeathsDamage
1950 Jan 10 - Feb 2Nea Kameni (Liatsikas dome)
Historical obs./docs.
2
1939 Aug 20 - 1941 Jul 2 ±1 d.Nea Kameni (Triton, Ktenas, Fouque domes)
Historical obs./docs.
2
1928 Jan 23 - Mar 17Nea Kameni (Naftilos dome)
Historical obs./docs.
2
1928 Jan 23
(eruption 1928 Jan 23 - Mar 17)
Historical obs./docs.
248
Info
1925 Aug 11 - 1926 MayNea Kameni (Dafni dome)
Historical obs./docs.
2
1866 Jan 26 - 1870 Oct 15Georgios, Afroessa and Reka domes
Historical obs./docs.
2
1866 Feb 20
(eruption 1866 Jan 26 - 1870 Oct 15)
Historical obs./docs.
21
Info
1707 May 23 - 1711 Sep 14Nea Kameni
Historical obs./docs.
3
1707 May
(eruption 1707 May 23 - 1711 Sep 14)
Tsunami recorded
Historical obs./docs.
3
Info
1650 AD Sep 27 - Dec 6Colombo Bank (6.5 km NE of Thera)
Historical obs./docs.
4?
1650 AD Sep 26
(eruption 1650 AD Sep 27 - Dec 6)
Kolumbo volcano 6.5 km NE of Santorini
Tsunami recorded
Historical obs./docs.
4120
light
Info
1570 AD - 1573Mikri Kameni
Historical obs./docs.
3
1050 AD
(eruptive episode 1050 AD)
Tsunami recorded
Historical obs./docs.
0
726 AD Jul 15 ±45 d.NE side of Thia Island
Historical obs./docs.
4?
46 AD Dec 31 - 47 Feb 1 ±30 d.Thia Island
Historical obs./docs.
3
46 AD
(eruption 46 AD Dec 31 - 47 Feb 1 ±30 d.)
Tsunami recorded
Historical obs./docs.
3
Info
19 AD
Discredited Eruption
-197 BC
(eruption 197 BC)
Tsunami recorded
Historical obs./docs.
3
Info
197 BCHiera Island
Historical obs./docs.
3
-1610 BC
(eruption 1610 ±14 y. BC)
Tsunami recorded
Historical obs./docs.
7100-1,000 (*)
heavy
Info
1610 ±14 y. BCPlinian "Minoan" eruption; Central and northern caldera area7?
(*) Estimated numbers
Remark:
Our list of volcanic eruptions closely follows the database of eruptions of the Smithsonian's Global Volcanism Project (GVP), the internationally most recognized data source for volcanic eruptions, but also includes significant eruptive episodes or related volcano events. "Volcanic eruptions" are usually to be understood as sequences of individual eruptive episodes that can follow each other, or even overlap (if several vents are involved), and can last many years, decades or even longer. For example, the current activity of Stromboli volcano is understood as a single eruption that has been ongoing since 1934.
Sources: NOAA National Centers for Environmental Information (NCEI), Global Significant Volcanic Eruptions Database. doi:10.7289/V5TD9V7K | Global Volcanism Project / Smithsonian Institution

Eruptions of Santorini volcano



1950 eruption
10. Jan. 1950 - 2. Feb. 1950: Small effusive activity ("Liatsikas" lavas) preceded by phreatic explosions.
More info

1939-41 eruption
20. Aug. 1939 - July 1941 -- Formation of several lava domes ("Tritona", "Ktenas", "Fouqué", "Smith-Reck" and "Niki"). Extrusive and slighly explosive activity. Lava outflow in most cases preceeded by phreatic explosions.
more info

1925-28 eruption
11. Aug. 1925- 17. March 1928 -- Moderate effusive and explosive activity. Growth of Nea Kameni. Lava flows, lava fountains and ash-falls.
- Aug. 1925 -- Rising temperature in the Red bay ("Kokkina Nera", gr. = red waters) at the eastern shore of Nea Kameni and subsidence of Nea Kameni's east shore. Vapor fountains and lava outflow. ...more info

1866-1870 eruption
4. Feb. 1866 - 15. Oct. 1870 -- Moderate effusive and minor explosive activity. Mikri and Nea Kameni unite. Lava flows, lava fountains and ash-falls. ...more info

1711 - 1866 activity
No volcanic activity occurred during 1711-1866. Mikri and Nea Kameni were 2 separated islands forming 2 natural bays (Georgios and Vulkano bay). Sulfuric fumaroles in Vulkano bay. Building of a small harbor and ca. 50 summerhouses (!) on Nea Kameni.

1707-1711 eruption: Nea Kameni appears
23. May 1707 - Sept. 1711 -- Formation of Nea Kameni (gr., = "the new burnt island"). Strong surtseyan and effusive activity. Ash-fall and gas explosions. Lowering of the coastline of Thera and Mikri Kameni. ...more info

1650 Kolumbo volcano eruption
27. Sept 1650 -- Kolumbo submarine volcano (ca. 8 km NE of Cape Kolumbo, Santorini): strong surtseyan-subplinian eruption with ash and pumice fall, toxic gasses (>50 fatalities). Generation of a strong tsunami.
more info on Kolumbo volcano

1570 eruption: Mikri Kameni Island appears
Formation of Mikri Kameni (gr., = "small burnt island"). Surtseyan activity, ash-fall and block fall-out accompany the formation of a lava dome which rises above sea level to form the new island Mikri Kameni.

1457-1458 activity
Unclear reports from Athanasius Kircher (1665) and Buondelmonte (1465/66) indicate that either a part of Palea Kameni collapsed and disappeared or a new island between Palea Kameni and Thera was built.

726 AD subplinian (?) eruption
Strong explosive probably sub-plinian eruption. Records by Nicephoros (758-823), Theophanes (752-818) and Cedremus (after 1059). Probably small effusive activity following the pumice eruption creating the black blocky lava lobe at Agios Nikolaos (the small harbor bay with the church and hot iron springs).

46 - 726 AD activity
No reports of activity are known from that period. There was either actually no eruption or it has not been recorded.

46 AD eruption - appearance of a new island
Appearance of a new island that probably grew together with Hiera and formed the basis of Palea Kameni. Descriptions by Roman historians Seneca (4 BC-65 AD), Livy (59 BC-AD 17), Pliny the Elder (23-79 AD), Dio Cassius (ca. 200 AD), Aurelius Victor (4th century AD), Philostratos (ca. 200 AD), Orosius (5th century AD), Cassiodorus. (418-562 AD), Labbreus (1670). Probably surtseyan activity with updoming of the sea-floor.

197 BC eruption: appearance of Palea Kameni
Formation of an island called Hiera (gr., = "the holy one") inside the caldera, probably a precursor of Palea Kameni. Documented by greek and Roman writers: Strabo (66BC - 24 AD), Plutarch (ca. 40-120 AD), Pausanias (ca.120 AD), Justinus (2nd century AD), Eusebius from Cesarea (270-340 AD) and Ammianus Marcellinus (ca. 330-400 AD). Probably surtseyan activity with updoming of the sea-floor (comparable with the 1707-1711 events).

1613 +- 13 BC Minoan eruption
The most recent plinian eruption on Santorini occurred in the late Bronze Age at around 1613 BC and is known as the so-called Minoan eruption. It is one the biggest known volcanic explosions in younger time,- and one of the most studied, but still most mysterious eruptions of all time-. It devastated not only Santorini, but had a deep impact on the whole of the Eastern Mediterranean. Perhaps it even had serious world-wide effects and changed history.
Size of the Minoan eruption
Dating of the Minoan eruption
Still today, one can see its deposits, the characteristic, tens of meters thick layer of white pumice and ash that blankets most of the surface of the island group. The eruption changed the shape of the island itself dramatically: it is now believed that before the eruption, it had the shape of an almost complete ring that enclosed an earlier, shallower caldera.
Large sections of island collapsed into the emptied magma chamber after the eruption, literally disappearing under the sea. The ring-island was breached to the W and NW, and the caldera was significantly widened and deepened.
The Minoan eruption devastated the rich, highly developed economic center, that Santorini was at that time. Since 1969, intense archaeological excavations have brought to light an important Cycladic/Minoan town which had been buried beneath the volcanic ash for almost 4000 years. Although it appears that people had time to evacuate their island in time before the eruption, carrying most of their goods with them, the findings from Akrotiri are impressive: especially, they include well-preserved and magnificent wall paintings, ceramics and other objects. Thanks to the work of numerous archaeologists, a new light was thrown on an important prehistoric period and culture. The spectacular discovery even induced continuing speculations that relate the volcanic destruction of Santorini to the legend of the sunken Atlantis.

Santorini Volcano FAQ

+When was the last eruption of Santorini volcano?

+How often does Santorini volcano erupt?

+How active is Santorini volcano at present?

+When was the largest eruption of Santorini volcano?

Latest satellite images

Santorini satellite image sat1Santorini satellite image sat2
Santorini Volcano Tours
Santorini Island (Greece)
Santorini Geology Tour
private tours to discover Santorini's geology with a volcanologist, 1-3 days
1-3 days - Custom (variable)
Price from 750 EUR
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Santorini Island (Greece)
Fascination Volcano
7-day geo and walking tour on Santorini, Greece
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Santorini Volcano Maps

Below is a selection of maps showing the location and surroundings of the volcano at various resolutions based on aerial-imagery / terrain maps. Feel free to use them for non-commercial purposes on your blog or website as long as you credit them with a link back to this page (click to copy it).
Satellite/aerial-type map of Santorini volcano (world scale)
Satellite/aerial-type map of Santorini volcano (world scale)
Terrain-type map of Santorini volcano (world scale)
Terrain-type map of Santorini volcano (world scale)
Satellite/aerial-type map of Santorini volcano (region scale large)
Satellite/aerial-type map of Santorini volcano (region scale large)
Terrain-type map of Santorini volcano (region scale large)
Terrain-type map of Santorini volcano (region scale large)
Satellite/aerial-type map of Santorini volcano (region scale medium)
Satellite/aerial-type map of Santorini volcano (region scale medium)
Terrain-type map of Santorini volcano (region scale medium)
Terrain-type map of Santorini volcano (region scale medium)
Satellite/aerial-type map of Santorini volcano (region scale small)
Satellite/aerial-type map of Santorini volcano (region scale small)
Terrain-type map of Santorini volcano (region scale small)
Terrain-type map of Santorini volcano (region scale small)
Satellite/aerial-type map of Santorini volcano (local scale large)
Satellite/aerial-type map of Santorini volcano (local scale large)
Terrain-type map of Santorini volcano (local scale large)
Terrain-type map of Santorini volcano (local scale large)
Satellite/aerial-type map of Santorini volcano (local scale medium)
Satellite/aerial-type map of Santorini volcano (local scale medium)
Terrain-type map of Santorini volcano (local scale medium)
Terrain-type map of Santorini volcano (local scale medium)
Satellite/aerial-type map of Santorini volcano (local scale small)
Satellite/aerial-type map of Santorini volcano (local scale small)
Terrain-type map of Santorini volcano (local scale small)
Terrain-type map of Santorini volcano (local scale small)
Satellite/aerial-type map of Santorini volcano (scale of 10s of km)
Satellite/aerial-type map of Santorini volcano (scale of 10s of km)
Terrain-type map of Santorini volcano (scale of 10s of km)
Terrain-type map of Santorini volcano (scale of 10s of km)
Satellite/aerial-type map of Santorini volcano (scale of 20-40 km)
Satellite/aerial-type map of Santorini volcano (scale of 20-40 km)
Terrain-type map of Santorini volcano (scale of 20-40 km)
Terrain-type map of Santorini volcano (scale of 20-40 km)
Satellite/aerial-type map of Santorini volcano (scale of approx. 10-20 km)
Satellite/aerial-type map of Santorini volcano (scale of approx. 10-20 km)
Terrain-type map of Santorini volcano (scale of approx. 10-20 km)
Terrain-type map of Santorini volcano (scale of approx. 10-20 km)
Satellite/aerial-type map of Santorini volcano (scale of 5-10 km)
Satellite/aerial-type map of Santorini volcano (scale of 5-10 km)
Satellite/aerial-type map of Santorini volcano (scale of few kilometers)
Satellite/aerial-type map of Santorini volcano (scale of few kilometers)

Further information / links:

Santorini Decade Volcano / www.decadevolcano.net/santorini/santorini.htm
Tom's private website about Santorini, Etna and other volcanoes. Contains a huge archive of volcano photos, information and other stuff.

Visit Santorini

Almost every postcard promoting Greece shows the typical churches with their blue domes. The village of Ia in the northwest of the main island of Thera is one of the most beautiful villages in the Mediterranean. In 1952, all of the island's villages were destroyed by a severe earthquake and were only slowly rebuilt afterwards. The burgeoning of tourism, which created work for the inhabitants of the archipelago, was helpful around 1970. Before, people could only support themselves through agriculture (wine, tomatoes and fava beans) or through emigration and shipping.

Even though tourism has become very prevalent in some places (e.g. through cruise ships), there are still original villages. Anyone who gets to know the island's beautiful hiking routes will experience a completely different Santorini than that shown on the glossy postcards.

Especially in spring you can discover rare orchids, collect herbs (e.g. oregano or thyme) and photograph beautiful flower meadows. If you venture away from the tourist centers of Thira and Kamari, you will find beautiful taverns where you can enjoy freshly prepared Greek specialties. The best time to travel to Santorini is March-June and mid-September - end of October. If you are really brave and like photography, you should also visit Santorini in winter.

Tom Pfeiffer and Tobias Schorr are experts on the island, both speak modern Greek and have been traveling to Santorini since around 1994. Since around 1996 they have been leading groups to the most beautiful and interesting places on the island. Of course, they have also made friends with some Santorinians who support them with their tour groups. One of their friends lives on the island of Palea Kameni, so close to the volcano... In small tour groups you can discover Santorini in a very special way with Tom and Tobias.
Sunset over the Nea Kameni volcano (c) Tobias Schorr
The bay with thermal water at Palea Kameni island (c) Tom Pfeiffer
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Kolumbo submarine volcano (Greece): earthquakes in the area decrease, unlikely related to volcanic activity

Earthquakes over time (past 30 days) near Kolumbo volcano
The earthquake swarm in the area half way between Santorini and Amorgos Island continues to decrease. Only occasionally, earthquakes have been reaching magnitudes higher than 3. Read all
Wed, 12 Feb 2025, 10:12

Santorini volcano (Greece): earthquake swarm continues, two more magnitude 5 events

Earthquakes in the Cyclades region over the past 24 hours as of 12 Feb 2025 morning
After a few comparably calmer days, the earthquake swarm has picked up again a bit although overall there are no significant changes. In the past 24 hours, the area between Santorini, Ios, Amorgos and Anafi islands has been shaken by 2 quakes above magnitude 5, and 29 quakes between magnitude 4 and 5, as well as hundreds of smaller quakes. Read all

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