Santorini’s powerful Minoan-era eruption

Around 1600 BCE, a catastrophic volcanic event reshaped the island of Santorini, buried the Minoan settlement of Akrotiri, and had far-reaching consequences across the Mediterranean. When I first visited Santorini in 1989, I read that the eruption caused Minoan civilization to collapse. But researchers have continued to investigate the eruption’s impact on the region and to refine the ages of the eruptive phases. Their results suggest that the eruption destabilized the civilization but that it did not fully decline until several centuries later.

My last post summarized the 1.6-million-year history of volcanic eruptions and includes maps and island photos: https://landscapes-revealed.net/the-astonishing-volcanic-island-of-santorini/. This post focuses on the Minoan eruption and its impact on Santorini and the surrounding region.

This southward view of the Santorini caldera shows Mesa Voumo (mountain on left side of photo), the thin southern strip of the island at Akrotiri (extends to the right of Mesa Voumo), and the currently active volcano of Nea Kaimeni that has built up in the center of the caldera since the Minoan eruption. Note that Santorini is another name for Thera—the Greek name for the largest of the islands surrounding the caldera.

Basics of Minoan civilization

Minoan civilization flourished on Crete from about 3000–1100 BCE, during the Bronze Age. The name derives from Minos, either a dynastic title or the name of a mythical ruler. Minoan civilization was remarkable for its great cities and palaces, its extended trade within the Mediterranean, and its use of writing. Its sophisticated art included elaborate seals, pottery and above all, the vibrant frescoes found on buildings’ interior walls (see photos below). 

The main center of Minoan culture was Knossos, located on the northern shore of Crete, near present-day Heraklion, Crete’s largest city. Archeologists have recreated the main palace in Knossos, although there is uncertainly about the accuracy of the reconstruction. In the limited time we had in Heraklion, we chose to visit the Heraklion Archeological Museum with its incredible collection of objects removed from Knossos (see photos below).

Minoan civilization spread throughout the Aegean region, reaching its peak around 1600 BCE, at the time of Thera’s powerful eruption, which certainly contributed to the decline of this flourishing Aegean culture.. As described below, items found in the excavated city of Akrotiri show the strong influence of Minoan culture in Santorini.

Sequence of the eruption

The Minoan eruption was the latest eruption of the Thera volcano. It had distinct phases: (1) Pre-eruption: earthquakes and minor tephra falls months before the main event likely prompted residents to evacuate; Phase 1: intense magmatic activity deposited up to 7 m (23 ft) of pumice and ash; Phase 2: Pyroclastic surges and lava fountaining destroyed remaining structures; Phase 3: caldera collapse began, possibly generating tsunamis; Phase 4: continued eruptions completed the caldera collapse and produced mega tsunamis.

The eruption is dated to 1627-1600 BCE, based on radiocarbon dating. An investigation about 20 years ago uncovered two olive trees buried alive in the pumice of the Minoan eruption on Santorini. Radiocarbon dating of the trees yielded a date of 1613±13 BCE. Ash from the eruption is found throughout the eastern Mediterranean region. Because the eruption was an instantaneous event, the ash forms an important geochronological marker.

This southward view shows layers of volcanic rock on the caldera wall. These layers are within the stratovolcano of Thera, which erupted in four distinct periods, starting about 360,000 years ago and culminating with the famous Minoan eruption. Three older calderas formed during earlier eruptions of Thera, but the current configuration is the result of the Minoan eruption. The white layer at the top of the caldera is the ash and pumice that buried the island and that is now used as building material—note the quarry in this top layer in the middle of the photo.
Close-up view of the caldera wall as we returned to Athinios Port on a boat tour to Nea Kaimeni volcanic island, located in the center of the caldera. A ferry boat is docked at the port. The zig-zag road is used by buses and taxis to transport passengers from the port to the island’s surface. The thick white layer at the top of the caldera wall is the Minoan tuff—the combined deposit of ash flows and ash falls that buried the island during the Minoan eruption.
The Minoan tuff is visible at the top of the caldera wall throughout the island. As you can imagine, all life and structures were destroyed by this thick deposit.

The ruins of Akrotiri town

Akrotiri, located on the southern end of Santorini, was damaged during a large earthquake in the early 17th century BCE. The city was subsequently rebuilt and enjoyed prosperity as one of the largest ports in the Aegean until its abandonment at the time of the Minoan eruption. The city maintained strong ties with the center of Minoan civilization located on the north shore of Crete, just 120 km (72 miles) away.

The city of Akrotiri was completely buried by ash during the Minoan eruption. Much of the area has been exposed by ongoing archeological excavations. Although this city was buried by ash, much like Pompeii, in this case the residents had enough warning to leave the island before the major phase of the eruption. No bodies have ever been found.

Preserved wall frescoes

When the city was rebuilt after the 17th century BCE earthquake, the most important rooms in houses were decorated with wall paintings of a high artistic level, indicating the inhabitant’s strong connection with Minoan culture. These works demonstrate the prosperity of Thera during the 17th century BCE and they provide much information about the people and their environment. The frescos were preserved beneath the ash. They have now been removed, via a tedious process, and are displayed in the Archeological Museum of Thera in Fira, the main town on Santorini today.

The wall paintings of Thera are executed in a mixed technique of painting on wet stucco, comparable to the wall paintings uncovered in Crete. The color palette consists of natural pigments: white from the stucco, black from carbon, red and yellow from iron-bearing minerals of hematite and ochre clay, and blue from a synthetic Egyptian pigment and/or the mineral glaucophane. They created other shades by combining pigments or mixing them with lime water.

This image is part of a longer fresco that provides a glimpse into city life. People are standing within buildings looking out to sea where boats are transporting people. A common theme of Minoan frescoes is nature. Notice the deer and other animals and plants found on land (left side of fresco) and dolphins found in the sea (right side of photo).

Other examples of Minoan art

I took these photos in the Heraklion Archeological Museum that has many spectacular objects excavated from the Knossos archeological site. Their similarity to objects found in Akrotiri demonstrate the close relationship between Crete and Thera.

Numerous ceramic figures of bulls were found in both Knossos and Akrotiri. This fresco shows bull-leaping, a ritual that seems to have had a religious or magical basis.
Some perfectly crafted bowls made from distinctive rocks.
This copper ingot from Cyprus was not surprising to see, given that Cyprus was the main source of copper used to make bronze at that time. The Minoans apparently traveled to Cyprus to buy copper, then returned it to Crete to craft into usable products.
This fresco of dolphins is from the main palace in Knossos.

Effects of the eruption on Minoan civilization

The ~1600 BCE eruption was certainly disastrous for the late Minoan civilization on Santorini—it caused people to evacuate the island and the thick deposit of ash prevented them from returning. Nevertheless, Minoan culture survived on Crete and elsewhere, although it was likely weakened by the combination of earthquakes, floating pumice, ash fall and tsunamis.

The last phase of the Thera eruption caused caldera collapse and generated a mega tsunami that devastated coastal areas of adjacent islands. Deposits from the tsunami are found all over the eastern Mediterranean, including in deep-sea cores, western Turkey, and as far away as Israel. At the Palikastro archeological site on the northeast tip of Crete, investigators found a fascinating tsunami layer with Santorini ash, broken up building stones, marine fossil shells including those of beach and open ocean organisms, pieces of ceramics and even bones. The distribution of this layer suggests the maximum wave height was 35 m (115 ft)!

The destruction of Minoan ports and ships by volcanic tephra and by tsunamis must have had severe effects on the trade network for some time. While these effects did not lead to immediate collapse of Minoan culture, they probably precipitated the culture’s decline in both economic power and aesthetic achievement.

Atmospheric effects were also probably severe. Volcanoes throw up sulphur dioxide, and large amounts of this gas, together with ash particles in the atmosphere, can alter the climate. Scientists have calculated that the eruption on Thera could have lowered annual average temperatures by several degrees across Europe, Asia and North America. Summer temperatures would have dropped even more, bringing years of cold, wet summers and ruined harvests. Some authors have attributed misfortunes documented in the Bible and in various myths and legends to the Santorini eruption. It’s even been called “the lost city of Atlantis”.

Farewell to Santorini

I took this photo from the air as we left Santorini. This view shows the natural slope of the Thera volcano and the caldera that formed in the middle of the volcano after the eruption of so much material caused the edifice to collapse.
We two geologists certainly enjoyed our time on this fascinating island. We took this “selfie” in Oia, with a view back to the caldera wall near Fira town.

We returned home on May 15, but I’ve finally managed to complete these posts. That’s because I returned to quickly leave again on a two-week hiking trip in the Owyhee Canyonlands in SW Idaho and easternmost Oregon. That trip will be the focus of my next post.

References for more information about the Minoan eruption

The Minoan Eruption of Santorini around 1613 B.C. and its consequences, 2013, by Walter L. Friedrich: https://geo.au.dk/fileadmin/www.geo.au.dk/02_Forskning/Publikationer/friedrich_satz.pdf.

The Minoan Santorini eruption and tsunami deposits in Palaikastro (Crete): dating by geology, archaeology, 14C, and Egyptian chronology’s 2016, by Hendrik J Bruins, Johannes van der Plicht, and J Alexander MacGillivray: https://www.cambridge.org/core/services/aop-cambridge-core/content/view/34D626713047C22C0AFFB5016D37CD0F/S003382220005579Xa.pdf/the-minoan-santorini-eruption-and-tsunami-deposits-in-palaikastro-crete-dating-by-geology-archaeology-14c-and-egyptian-chronology.pdf.

The Minoan Eruption of Santorini: A Cataclysmic Event That Shaped History, 2024, by Elena Skye: https://santorini.wiki/minoan-eruption-of-santorini/.

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10 Comments

  1. Jen Blank on June 23, 2025 at 9:15 pm

    Lovely read, Karen, with the mix of geology, archeology, and history. I went to Santorini/Thera as a girl and remember the long zig-zag route to the town at the top of the harbor. We also went to the central island, Nea Kameni, and walked among active fumaroles. Tried to imagine the tsunamis and ash from a much earlier eruption affecting Crete. I remember, too, swimming among small jellies and being kind of grossed out though they didn’t sting. Most impressive to me, though, were Knossos on Crete and the Heraklion Archaeological Museum. I loved the dolphin frescos. In the palace, our guide told us that while Abraham was making his way across the fertile crescent, the king of the Minoans had hot and cold running water and flush toilets. That factoid has stayed with me all these years. My parents and kids spent a few weeks on several of the Greek Isles back then, reading many (any) of the Mary Renault books we could find – and especially enjoyed “The Bull from the Sea” and “The King Must Die”. And I’d wanted to visit Crete since reading “The Moon-Spinners” by Mary Stewart….

    • Landscapes Revealed on June 23, 2025 at 10:24 pm

      Thanks Jen! So good to hear from you and share your memories. The history in this part of the world is fascinating, and wrapped up in so many myths and legends. I’ve not read any of the books you mention, but maybe I should!

  2. Sarah Kemp on June 24, 2025 at 2:46 pm

    Wonderful post. It so made me want to revisit. In 1981, so much of this has just been discovered.

    • Landscapes Revealed on June 24, 2025 at 10:27 pm

      Thanks Sarah! You would truly be amazed at the differences since 1981.

  3. Keeley Kirkendall on June 25, 2025 at 7:13 am

    I shared your post with several friends I volunteer with who just returned from Crete and they really appreciated the information. Thanks for sharing.

    • Landscapes Revealed on June 25, 2025 at 1:40 pm

      Thanks for reading Keeley, and for sharing with your friends!

  4. Mark on June 25, 2025 at 11:27 am

    A combination of archeology and geology to tell a fascinating story. Your posts are amazing with all the photos and detail! Thanks!

    • Landscapes Revealed on June 25, 2025 at 1:41 pm

      Thanks for reading Mark—it makes the effort worthwhile!

  5. Brian Boru Quinn on June 25, 2025 at 12:08 pm

    Fantastic and detailed review. So much more coherent than in 1989, as some things truly get better over time!

    • Landscapes Revealed on June 25, 2025 at 1:44 pm

      It was good to see more of the island this time. We did go to Perissa—was glad to see that it still had a more relaxed vibe than elsewhere. Still more developed though, and no campground in the middle of town!

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