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15 · Infrastructure · Seasonal forest

Drinking at Tikal

Reservoirs for a city without a river

Tikal stored rainwater to supply its population during the dry months.

Museum documentation · free public access, no account required.

DECLARED VISUAL RECONSTRUCTION · EXISTING EDITORIAL RESOURCE · TRACEKEEPERS

Generated reconstruction · Declared visual hypothesis

Declared visual reconstruction for museographic context; it is not a photograph of the original nor documentary evidence.

Specific historical recreation of Reservoirs for a city without a river, Tikal, Petén, Guatemala, Main development c. 250–850 CE
DECLARED VISUAL RECONSTRUCTION · EXISTING EDITORIAL RESOURCE · TRACEKEEPERS

Generated reconstruction · Declared visual hypothesis

Declared visual reconstruction for museographic context; it is not a photograph of the original nor documentary evidence.

History and context

Tikal grew on limestone terrain without a major permanent river near the centre. Quarries converted into reservoirs, inclined surfaces and watering holes collected rain from the wet season to get through the dry months.

Managing water was a technical and political task: cleaning, channelling and deciding access connected neighbourhoods, palaces and plazas. Reservoirs did not guarantee eternal security; droughts, pollution and conflict could strain the system at different times.

On a limestone plateau without a permanent river, Tikal captured rain from plazas and sealed surfaces towards reservoirs and watering holes. Some quarries changed function and were integrated into an infrastructure requiring continuous cleaning.

Controlling water could reinforce institutions and inequalities of access, but reservoirs alone do not explain the ninth century. Drought, pollution, war and local decisions form a multicausal problem.

Evidence and interpretation

Documented fact: UNESCO documents historical reservoirs within an urban zone of at least 1,200 hectares and irrigation structures in Tikal. Interpretation and caution: their exact relationship with ninth-century crises is the subject of multicausal research; no single demonstrated cause exists for urban decline.

Catalogue facts

Narrative date
Main development c. 250–850 CE
Location
Tikal, Petén, Guatemala
Material
Limestone · stucco · sediments · rainwater
Context
Urban infrastructure, seasonality and power
Curatorial reading
The documented fact and its interpretation appear separately in the evidence block.
Date
Main development c. 250–850 CE
Location
Tikal, Petén, Guatemala
Support
Limestone · stucco · sediments · rainwater
Documentary coverage
3 museum, heritage, primary corpus or research sources for this stop.

A closer look

About 1 min to read · 1 section. Further reading and sources · free access. Editorial review recorded: .

A mineral barrier for water

A study published in 2020 identified quartz and zeolite in the sediments of the Corriental reservoir at Tikal. These minerals, brought from outside the city, support the interpretation of a filtration system: zeolite possesses a structure capable of retaining various substances and the ensemble would function as a barrier before storage. The identification was supported by mineralogical analysis, not solely by the form of the deposit. Corriental thus offers a specific technical solution within the hydraulic network. Its existence does not demonstrate that all of Tikal's reservoirs used the same filter nor that all urban water was equally safe.

Location and territory

Physical world map with routes of human evolutionPresent-day world coastline from Natural Earth in an equirectangular projection. The overlaid markers let you explore each milestone.Map base: Natural Earth 1:110m · public domain · present-day reference coastline

LOCATED SITE

Tikal · GuatemalaMarker of the Maya city.

Sources and references

Expand this information and consult its sources

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