Gufkral: farming, tools and changing homes

The mound near Tral

Gufkral lies beside Bonmir in the Tral area of southern Kashmir. Archaeological deposits survive on a raised karewa terrace, above the surrounding fields. The site is particularly important because its excavated sequence includes occupation without pottery, later Neolithic households and subsequent megalithic and historical remains. It preserves changes within a settlement, rather than a single moment called the Stone Age.

The name is commonly explained through the Kashmiri words for cave and potter. Caves in the terrace and the work of local potters form part of the place’s more recent history. Their presence does not by itself demonstrate that present families descend directly from particular excavated households, or that every visible cave was occupied in the Neolithic period.

Excavation and the three Neolithic phases

Excavations in 1981–82 by the Archaeological Survey of India, associated with K. D. Banerjee and A. K. Sharma, distinguished three Neolithic phases: IA, IB and IC. The first was aceramic, meaning pottery was absent from the excavated assemblage. Pottery appeared in the subsequent phases. These labels describe deposits and their contents, not named peoples.

The original excavation review describes pits, floors, postholes and later building remains. Such features must be interpreted together. A pit can be a shelter, a storage place or a feature reused for another purpose; finding one does not identify its function without the surrounding evidence.

Changing homes and the difficulty of matching accounts

The excavation review reports a compact floor sealing the aceramic deposits. In its account of the following phase, mud and rubble construction accompanied the disappearance of dwelling pits. Later deposits included refuse pits and repaired floors. Stone harvesters, spindle whorls and bone implements expanded the evidence for household production.

One later overview instead describes people continuing to occupy pits in phase IB and moving above ground in IC. These accounts should not be blended into a falsely precise sequence. Sharma’s first-season report independently places the disappearance of dwelling pits in IB, agreeing with the annual excavation review. This article follows that primary account while noting the later overview’s different assignment.

The first season in closer detail

Sharma records the first excavation season as 18 August to 20 October 1981. Six quadrants were opened, five reaching natural soil. That limited area matters: the excavated sequence cannot describe every part of the mound with equal confidence.

His report distinguishes two floor levels within the aceramic phase. Some pits were enlarged and reused; postholes and reed impressions in mud supported an interpretation of light superstructures. Hearths were outside the dwelling pits. Red ochre occurred on early working surfaces and on a grinding stone. The report also describes a bone needle with a damaged eye, alongside points, awls and scrapers. Such small objects extend the history beyond shelter and food to the making and repair of everyday materials.

Sharma’s crop discussion was provisional: grain identification was continuing, and he considered both collection and cultivation. Later summaries describe farming more confidently. The recovered grains and the interpretation of how they were obtained should remain distinct.

Food, animals and household tools

Archaeological syntheses associate early Gufkral with wheat, barley and lentils, together with both wild and domesticated animals. Later deposits add peas and show increased reliance on domestic stock. Stone and bone tools include equipment for cutting, piercing, grinding and processing materials. The evidence places cultivation, herding and hunting within the same changing economy.

The excavation review records sheep, goats and cattle, as well as hunted animals. Its interpretation emphasizes the growing importance of husbandry through the sequence. This does not mean that one household activity immediately replaced all others. Animal bones and plant remains are samples of what survived and was recovered, rather than a complete menu or a census of every herd.

Charcoal and the calendar

The 1982–83 archaeological review identifies pine charcoal in samples assigned to phases IA and IB, and Prunus and Indian horse chestnut in another IB sample. It records their excavation contexts and radiocarbon measurements. Wood identifications add evidence about materials brought into the settlement; they do not establish that every identified tree grew immediately beside a house.

Radiocarbon ages expressed as years before present must be distinguished from calibrated calendar dates. Later summaries place the Neolithic phases broadly within the third and early second millennia BCE. The precise-looking endpoints sometimes reproduced for these phases are not recorded founding or abandonment years. No month or day is known. The timeline therefore treats Gufkral as an archaeological period.

Later stones and disturbed evidence

A later survey of southern Kashmir describes fallen megaliths at Gufkral and objects found around the mound, including beads near trenches for water infrastructure. Its observations help document what remained visible after the original excavation. The position of a fallen stone, however, cannot automatically reconstruct the arrangement in which it first stood.

The same caution applies to objects collected on a disturbed surface. A bead found near a modern trench has lost part of the information that an undisturbed layer could provide. It may be significant, but its findspot alone cannot assign it securely to a Neolithic household or establish the date of a nearby monument.

New dating research in 2026

A study published in August 2026 by Abdul Adil Paray, Manoj Kumar and Rajveer Sharma reports twenty dated samples from Gufkral’s extension, Hariparigam and Qasim Bagh. The researchers sampled exposed deposits to limit disturbance at threatened sites and calibrated their results with IntCal20. Across all three sites, the reported dates extend from about 2890 to 516 BCE, with many falling between 2500 and 2200 BCE.

That combined range must not be presented as the occupation span of Gufkral alone. The extension also needs to be distinguished from the original excavated area. The study adds chronological evidence and a method for investigating vulnerable deposits, but its site-specific sample table is needed before assigning individual results to Gufkral’s earlier phase scheme.