Key dates
- 1314Moisture reconstructions identify the beginning of an exceptionally wet interval in parts of northern Europe.1
- 1315Harvest failure and high prices produce a widespread food crisis; English testimony describes grain struggling to ripen.34
- 1316Another poor season deepens shortages; research on England and Wales identifies an especially severe grain crisis.4
- 1317The conventional three-year core of the Great Famine ends, although regional economic difficulties continue.104
- 1319–1320A cattle epidemic in England and Wales destroys herds, worsening problems in dairying and farm recovery.8
- to about 1325Research tracing the epizootic finds it persisting in Ireland into the 1320s.9
The geography and chronology of the Great Famine
The name Great Famine brings together overlapping events rather than describing an identical catastrophe across an entire continent. It is especially associated with Europe north of the Alps, including the British Isles and the Low Countries. Regional research exposes differences even between neighbouring areas. In Wales, a relative lack of detailed contemporary narrative does not demonstrate that farming escaped the crisis. Estate accounts and other evidence must be considered alongside prices and conditions documented in neighbouring England.
The years 1315–1317 conventionally identify the central harvest-failure episode. A broader account also follows later seasons and the 1320s, particularly where livestock losses compounded grain shortages. The final date in the title therefore does not mark the restoration of food security for every household. Distinguishing the wet interval, the acute food emergency and the rebuilding of productive resources is essential. They were connected processes, but their beginnings and endings did not coincide everywhere.410
How persistent rain threatened harvests
Tree-ring research offers evidence independent of narrative accounts of exceptionally wet years. The Old World Drought Atlas reconstructs a widespread interval of high moisture beginning in 1314. This is a reconstruction of moisture conditions, not rainfall recorded by medieval weather stations. Its value includes the spatial pattern: the wet north contrasted with parts of southern Europe that experienced different conditions. A continental label must therefore be used with care when describing the particular agricultural hazards faced by local communities.
For farmers, the timing and persistence of rain mattered as much as the presence of water itself. Saturated ground obstructed field work, while grain needed suitable conditions for ripening, harvesting and drying. A crop standing in a field was not yet a secure food reserve. Johannes de Trokelowe described problems with ripening and drying grain in 1315. These successive obstacles help explain how wet conditions could affect not only the quantity harvested but also its quality and the moment when usable grain reached stores or markets.123
Food, seed and fodder competed for limited reserves
Grain served several purposes that became increasingly difficult to reconcile during a shortage. Households required it for immediate consumption, retained some for sowing, and needed feed to maintain animals. Drawing down reserves could bridge the next week while weakening the capacity to begin another production cycle. This helps explain why repeated harvest failure was especially dangerous: a family entered the second poor year with fewer resources and less room to adjust than it had possessed before the first.
Trokelowe connects expensive fodder with difficulties in feeding pigs and obtaining animal products. His account also records a brief autumn improvement followed by renewed scarcity. The sequence illuminates seasonality: the arrival of some fresh grain did not guarantee sufficient food until the next harvest. A farm was a connected set of resources, rather than simply an acreage under cultivation. Human consumption, the next sowing and animal maintenance could all place demands on the same dwindling stock, making immediate survival and future production increasingly hard to balance.3410
Prices, purchasing power and imperfect markets
Famine cannot be explained solely by the physical absence of food from a particular locality. Grain might remain in a store or appear for sale while being beyond a household’s means. Small producers could also be food buyers if their own harvest failed to last the year. Rising prices then placed pressure on wages, savings and other resources. For such a household, the decisive issue was how much food it could actually obtain, rather than the total amount of grain produced somewhere within the surrounding region.
In his study of England and Wales, Philip Slavin identifies market problems that intensified the ecological shock, including hoarding, preferential access to exchange and weakened supervision. Trade did not operate as a seamless network carrying every available surplus immediately to the people who needed it. This does not mean that exchange inevitably worsened famine: it could move supplies out of less affected areas. The critical questions concern who could buy, under what conditions, and with what prospect of securing a delivery before household resources ran out.6510
Warfare compounded environmental damage
In parts of the British Isles, the food crisis overlapped with the long Anglo-Scottish wars. Research covering the conflict of 1296–1328 demonstrates how warfare and environmental difficulties compounded damage. War did not explain the entire European geographical reach of the famine, but it was a significant source of local vulnerability. A community already affected by failed harvests had less capacity to absorb further losses of supplies, livestock or the resources required to continue production.
The overlap changes how recovery should be understood. Better weather alone could not erase the consequences of conflict or ensure secure agricultural work. The harvest calendar therefore needs to be considered together with the geography of warfare. Two communities experiencing similar rain could have very different capacities to maintain output or obtain supplies. Research on Flanders raises a related point, connecting adverse weather with warfare and the distribution of property rights rather than treating rainfall as a complete explanation of social outcomes.75
Cattle disease was a separate, overlapping shock
The cattle epidemic should not be assigned the same dates as the main grain crisis without explanation. Timothy Newfield traces the disease westwards from central Europe around 1315 and finds its effects persisting in Ireland until about 1325. In England and Wales, the particularly destructive outbreak occurred in 1319–1320. Historical descriptions support the reconstruction of an epizootic, but they do not justify unconditionally identifying it with a single disease recognised by modern veterinary medicine.
Losing cattle meant more than losing a potential source of meat. Milk production, draught power, manure and the capacity to rebuild herds through breeding were also affected. Consequences depended on the organisation of a particular farm and were not distributed evenly between estate owners and peasant households. A replacement animal could only be purchased if one was available and the buyer had the means. Herd recovery therefore followed its own biological and economic timescale, distinct from the improvement possible in a single season’s grain harvest.98
Why some households were more vulnerable than others
Shared weather did not produce identical exposure to hunger. A household holding a food reserve, a farm with more land and a family dependent mainly on wages occupied different positions. Sam Geens’s work on Flanders highlights the importance of property relations and local power in shaping household vulnerability. Access to income and resources could alter the consequences of the same harvest failure. Neither a rainfall map nor a regional estimate of grain output is sufficient on its own to explain the social distribution of suffering.
These distinctions make it possible to examine rural experiences without treating all villagers as one undifferentiated group. A family with reserves could delay disposing of assets; a household without a buffer had less time to respond. Accepting an obligation or depleting productive resources could improve immediate consumption while weakening future independence. This describes a mechanism of vulnerability, not a claim that every family followed precisely the same path. Regional evidence is needed to establish how such pressures operated within particular local societies.5610
Recovery and the famine’s agricultural significance
An improved harvest did not automatically reverse accumulated losses. Production still required seed, animals and the means to support a household until the next crop matured. This is why research sometimes uses a longer crisis chronology than 1315–1317 alone. In England and Wales, subsequent grain difficulties and the cattle epidemic affected already depleted resources. Yet a sequence established for one region should not be extended mechanically across the continent, nor should the entire 1320s be portrayed as an uninterrupted famine of uniform intensity.
The Great Famine preceded the Black Death and constitutes a separate historical subject. It must also be distinguished from the nineteenth-century Irish potato famine. Its agricultural importance lies in the connections it reveals between cultivation, animal husbandry, exchange and social relations. Weather delivered a powerful shock, but access to resources shaped the ability to withstand it. Regional studies of timing, mechanisms and recovery provide a sounder picture than a single supposed mortality percentage applied indiscriminately to the whole European population.4810
Questions and answers
Did the Great Famine affect all of Europe?
Not in the same way. It is most closely associated with northern Europe, and moisture reconstructions show substantial differences between the north and parts of the south. The severity and duration of shortages varied regionally.110
Sources
- Edward R. Cook et al. (2015). Old World megadroughts and pluvials during the Common Era
- Seung Hun Baek et al. / Columbia Climate School (2020). Europe’s “Great Famine” Years Were Some of the Soggiest in Centuries
- Johannes de Trokelowe; translation Brian Tierney / Fordham University (1315; edition 1866). The Famine of 1315: chronicle extract, Internet Medieval Sourcebook
- Phillipp R. Schofield (2018). Wales and the Great Famine of the early fourteenth century
- Sam Geens (2018). The Great Famine in the county of Flanders (1315–17): the complex interaction between weather, warfare, and property rights
- Philip Slavin (2014). Market Failure during The Great Famine in England and Wales (1315–1317)
- Philip Slavin (2014). Warfare and Ecological Destruction in Early Fourteenth-century British Isles
- Philip Slavin (2012). The Great Bovine Pestilence and its economic and environmental consequences in England and Wales, 1318–50
- Timothy P. Newfield (2009). A Cattle Panzootic in Early Fourteenth-Century Europe
- Fredrik Charpentier Ljungqvist et al. (2024). Famines in medieval and early modern Europe—Connecting climate and society
Approximate dates (c.) describe the nature of the evidence: archaeology dates settlements, layers and remains, not single moments of invention.