UNESCO World Heritage SiteUNESCO Heritage
Obi-Rakhmat Grotto
Uzbekistan

Obi-Rakhmat Grotto

Shallow karst cave with Neanderthal fossils

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Historical Context

About

The Obi-Rakhmat Grotto, located in Uzbekistan, is a significant Middle Paleolithic archaeological site known for its Neanderthal fossils. Discovered in 1962, the cave features a rich stratigraphy with 22 distinct layers, indicating prolonged Neanderthal habitation. The lithic assemblages found at the site suggest a transitional industry between the Middle and Upper Paleolithic periods. The site's faunal remains, consisting mainly of Siberian mountain goat and red deer, indicate its use as a short-term hunting and butchery station by hominins. Notably, the discovery of a juvenile Neanderthal's cranial and dental remains offers insights into the morphology and genetic lineage of Neanderthals in Central Asia, connecting them to European populations. The site is dated to around 70,000 to 90,000 years ago, with some layers suggesting even older occupations.

Paleolithic
Mesolithic
Neolithic
Chalcolithic
Bronze Age
Iron Age
Classical Period
Post-Classical Period
Early Modern Period
Industrial Period
Contemporary Period
Visual Archive

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Temporal Epochs

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Middle Paleolithic occupation

70000 BCE to 40000 BCE

Upper Paleolithic transition

50000 BCE to 10000 BCE

Classification

Archaeological Features

Unique architectural and cultural elements found at this historical site

category

Domestic and Habitation Structures

Caves
category

Environmental and Natural Features

Modified CavesCharcoal DepositsBone Middens
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Food Production and Processing Features

Butchering Areas
Knowledge Base

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Reference

Details

Country

Uzbekistan

Coordinates

41.57° N, 70.13° E