The end of the Bronze Age as an example of a sudden collapse of civilization

by Florian Ulrich Jehn

Why do civilizations collapse? For some civilizational collapses in the past there is one striking event that leads to a quick end, like environmental damage for the people on the Easter Islands. For other civilizations, several causes interact with each other, as it happened for the Maya, where environmental damage, climate change and hostile neighbors sealed their fate (Diamond, 2011). But the most mysterious case I came across is the simultaneous collapse of almost all major empires in the Mediterreanen during the late Bronze Age. In only around 50 years between 1200 and 1150 BCE the Mycenaean Kingdoms and the Hittite Empire dissolved, Egypt lost its control over the Levante and broke down shortly after. Only Elam and the Assyrian Empire survived somewhat intact. To put this into perspective, there weren’t many states around in this time of human history. Depending on how you count it this means that most existing states on Earth in this time either collapsed or declined. There is less data about China and India for the late Bronze Age, but there are some indications that they also struggled at a similar time, which would make this a global crisis that involved every state that existed at that time. However, as the data from India and China is very scarce I will focus on the Mediterranean, describe my current understanding of the Bronze Age collapse and what we might be able to learn from it today.

So, what happened? This is still debated much and there are many conflicting theories, but I try to tell here the story that seems most likely to me (I am not a historian, so maybe take this with a grain of salt). I’ve seen many papers that traced the collapse back to only one or a few causes, but it made more sense to me that basically all proposed causes are responsible to some degree and I try to highlight their connections in the text and Figure 2.

We know from the archaeological record that most of the cities in the region were destroyed by force (Figure 1). The people who destroyed those cities are usually simply called “Sea People”. They have this vague name because they do not consist of a single culture. Depending on the location and year their composition varied considerably (Burlingame, 2011). Also, they do not seem to have any overarching command structure and attacks happen more or less randomly. From the movement of their attacks we can see that the general direction the sea people moved was from north to south and it seems that along the way they either destroyed the local population or integrated them into their move southwards (Carlin, 2019).

Other research links these movements to a drought that led to widespread famines (Weiss, 1982), which was likely caused by a cooling of the mediterranean sea (Drake, 2012). This decreased evaporation, which led to reduced precipitation, resulted in a drought and famine. The sea itself cooled because of a large volcanic eruption of Mount Hekla in Iceland (Yurko, 1999), that likely produced a volcanic autumn that reduced temperature globally and clouded the sky (this is also the link to the problems of the civilizations in India and China).

Figure 1: Map of the Sea People invasions in the Aegean Sea and Eastern Mediterranean at the end of the Late Bronze Age (blue arrows). Some of the major cities impacted by the raids are denoted with historical dates. Inland invasions are represented by purple arrows. (Source: Kaniewski et al., 2011)

But this climatic approach does not explain everything. The civilizations in this part of earth already survived similar events in the past. For example the destruction of the Minoan civilization on Crete (which is in the middle of the eastern Mediterranean) was caused by another major volcanic eruption (Marinatos, 1939). However, all other civilizations survived mostly unharmed. This indicates that also the societal structure comes into play. There are indications that the civilizations of that time were highly centralized, with the main cities and palaces collecting all of the output of the surrounding farms and workshops (Nakassis et al., 2011). The resources collected in this way were then used to trade and to satisfy key supporters of the ruling class. However, this system relies on the ability of the central government to collect the output of everyone else. This ability was disrupted by the changing climate. The cities in the Mediterranean usually had a higher need for food and other resources to maintain themselves than their immediate surroundings were able to deliver. Thus, they relied on the smaller cities to regularly provide them with food. With the changing climate, the smaller cities needed the food they produced for themselves and stopped their deliveries to the main cities (Knitter et al., 2019). Without those deliveries the central authority had two problems at once. Suddenly there is a shortage of daily everyday goods the citizens needed but, they also missed out on valuable trade goods. Those trade goods were quite important, as the states of that times were connected in a vast trade network reaching from Egypt to Scandinavia (Varberg et al., 2020). This trade network was essential, as all states of that time needed tin and copper to produce bronze. While copper is relatively abundant and can be mined in many places, large tin deposits are much rarer. Major deposits can be found in present day Spain, Southwest England and Afghanistan (Berger et al., 2019). Therefore, without trade you lose the access to tin, which means you cannot smelt bronze anymore. As bronze was especially important for the production of weapons and armor, a loss of it means a reduced ability to defend yourself against invaders. Another important function of the trade network was to keep in connection with the other empires. There are several indications that the empires helped each other out with food and military aid during emergencies (Burlingame, 2011). What also made defense much harder was a series of earthquakes that hit the Mediterranean at that time. They likely destroyed much of the fortifications and palaces in the region, which left the cities defenseless and in chaos (Nur and Cline, 2000). All those factors were further enhanced by the impact of diseases. There are several indications that a kind of pandemic was rampant during this time as well. However, it is unclear which diseases it was. Likely candidates include the bubonic plague and smallpox (Norrie, 2016). This destabilized society and decreased the available resources, which led to migration and finally to pressure on other cities. The final contributing factor I found is civil war. There are several cities where only the palace is burned down, while the rest of the city remained unharmed, which is an indication of a violent uprising (Carlin, 2019).

All those factors draw a very complicated picture of the Bronze Age collapse (Figure 2). There is not a single defining cause for the collapse. Every factor on its own would likely not have been enough to topple several Bronze Age empires. However, their interaction led to a quick end of the Bronze Age, which had been relatively stable for centuries or even millennia.

Figure 2: Interaction of the different factors that led to the late Bronze Age collapse (own figure).

The reason I am trying to tell this story is that it reminds me of the current situation of the world. There are many factors contributing to a complex system of which we don’t always have a deep understanding or overview of. It is really hard to pinpoint the date when it is too late for a system before it collapses. When was the point the fate of the people of the Bronze Age was sealed? When Mount Hekla erupted? When the centralized structure collapsed? When tin became unavailable? The causes that seem most likely to me is the eruption of Mount Hekla and the series of earthquakes.Those two events started a kind of chain reaction by interacting with the way the society of that time was organised. A volcanic eruption that hit a different kind of society would not have been so fatal, as was shown by the earlier eruption at Crete. However, it is almost impossible to pinpoint the main cause of or even determine if there is something like this. This highlights how difficult it is to really find the exact tipping point of a system.

There is also some research that shows that humans have difficulties finding tipping points and that we might even be lacking the right techniques to do this right (Dudney and Suding, 2020). Therefore, I think we should be more careful when it comes to tipping points in our modern world. Right now this seems most urgent for climate change. We have a lot of tipping points in our climate system like thawing permafrost or a quickly dying rainforest (Lenton et al., 2019). And even though we are getting to understand those better, there are still many unknowns. We can learn from the Bronze Age collapse that a civilization can shine its brightest shortly before its destruction (Carlin, 2019). And in many respects the civilization of that time was not that different to the one we have today, like the vast trade networks, the interdependence of states and the need to acquire certain scarce resources. However, we also have more resources and more knowledge than the people in the Bronze Age. Also, we are much more connected and better equipped to help each other out. Still, we should not be too self assured, as the people of the Bronze Age might also have thought that they had it all figured out, right before disaster struck.

Imagine a person that was born 1230 BC in Ugarit, a prosperous city of the vast Hittite Empire. Everything seems to be going well. The cisterns and granaries are full, goods and people from all over the known world regularly arrive at the city and a surprisingly large portion of the population is able to write. Now fast forward 80 years to 1150 BC. Ugarit is a blackened ruin, the Hittite Empire simply does not exist anymore, everyone she knew is dead from disease, war and famine and the sun has not shown through the grey clouds for years.

I hope we can avoid such a fate for our current civilization.

Thanks to Jan Wittenbecher, Peter Ruschhaupt, Lutz Breuer, Matteo Trevisan and Luise Wolf for proofreading this text and providing valuable comments!

If you want to learn more about the topic you can find all the resources I used below. Also, there is a somewhat similar post from earlier this year.


Berger, D., Soles, J. S., Giumlia-Mair, A. R., Brügmann, G., Galili, E., Lockhoff, N. and Pernicka, E.: Isotope systematics and chemical composition of tin ingots from Mochlos (Crete) and other Late Bronze Age sites in the eastern Mediterranean Sea: An ultimate key to tin provenance?, edited by A. Zerboni, PLoS ONE, 14(6), e0218326, doi:10.1371/​journal.pone.0218326, 2019.

Burlingame, K.: Forces of Destruction: The Collapse of the Mediterranean Bronze Age, Bachelor Thesis, Pennsylvania State University., 2011.

Carlin, D.: Chapter 3: The End of the World as They Knew It, in The end is always near: apocalyptic moments, from the Bronze Age collapse to nuclear near misses, HarperCollins Publishers, New York, NY., 2019.

Diamond, J. M.: in Collapse: how societies choose to fail or survive, Penguin Books, New York, NY., 2011.

Drake, B. L.: The influence of climatic change on the Late Bronze Age Collapse and the Greek Dark Ages, Journal of Archaeological Science, 39(6), 1862–1870, doi:10.1016/​j.jas.2012.01.029, 2012.

Dudney, J. and Suding, K. N.: The elusive search for tipping points, Nat Ecol Evol, doi:10.1038/​s41559-020-1273-8, 2020.

Kaniewski, D., Van Campo, E., Van Lerberghe, K., Boiy, T., Vansteenhuyse, K., Jans, G., Nys, K., Weiss, H., Morhange, C., Otto, T. and Bretschneider, J.: The Sea Peoples, from Cuneiform Tablets to Carbon Dating, edited by K. Hardy, PLoS ONE, 6(6), e20232, doi:10.1371/​journal.pone.0020232, 2011.

Knitter, D., Günther, G., Hamer, W. B., Keßler, T., Seguin, J., Unkel, I., Weiberg, E., Duttmann, R. and Nakoinz, O.: Land use patterns and climate change—a modeled scenario of the Late Bronze Age in Southern Greece, Environ. Res. Lett., 14(12), 125003, doi:10.1088/​1748-9326/​ab5126, 2019.

Lenton, T. M., Rockström, J., Gaffney, O., Rahmstorf, S., Richardson, K., Steffen, W. and Schellnhuber, H. J.: Climate tipping points — too risky to bet against, Nature, 575(7784), 592–595, doi:10.1038/​d41586-019-03595-0, 2019.

Marinatos, S.: The Volcanic Destruction of Minoan Crete, Antiquity, 13(52), 425–439, doi:10.1017/​S0003598X00028088, 1939.

Nakassis, D., Parkinson, W. A. and Galaty, M. L.: Redistribution in Aegean Palatial Societies Redistributive Economies from a Theoretical and Cross-Cultural Perspective, American Journal of Archaeology, 115(2), 177–184, doi:10.3764/​aja.115.2.177, 2011.

Norrie, P.: How Disease Affected the End of the Bronze Age, in A History of Disease in Ancient Times: More Lethal than War, edited by P. Norrie, pp. 61–101, Springer International Publishing, Cham., 2016.

Nur, A. and Cline, E. H.: Poseidon’s Horses: Plate Tectonics and Earthquake Storms in the Late Bronze Age Aegean and Eastern Mediterranean, Journal of Archaeological Science, 27(1), 43–63, doi:10.1006/​jasc.1999.0431, 2000.

Varberg, J., Kaul, F. and Gratuze, B.: Bronze Age Glass and Amber Evidence of Bronze Age long distance exchange, Adoranten, (2019), 5–29, 2020.

Weiss, H.: The decline of Late Bronze Age civilization as a possible response to climatic change, Climatic Change, 4(2), 173–198, 1982.

Yurko, F. J.: End of the Late Bronze Age and other crisis periods: a volcanic cause?, in Gold of praise: studies on ancient Egypt in honor of Edward F. Wente, edited by E. F. Wente, E. Teeter, and J. A. Larson, Oriental Institute of the University of Chicago, Chicago, Ill., 1999.