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China

Kizil Caves

Buddhist rock-cut cave complex in China

Time Periods

Paleolithic

Paleolithic

Mesolithic

Mesolithic

Neolithic

Neolithic

Chalcolithic

Chalcolithic

Bronze Age

Bronze Age

Iron Age

Iron Age

Classical Period

Classical Period

Post-Classical Period

Post-Classical Period

Early Modern Period

Early Modern Period

Industrial Period

Industrial Period

Contemporary Period

Contemporary Period

Location

About

The Kizil Caves, also known as the 'Thousand Red Houses,' form a significant Buddhist rock-cut cave complex in Xinjiang, China. Situated along the ancient Silk Road, these caves represent the earliest major Buddhist cave complex in China, with development spanning from the 3rd to the 8th centuries CE. The site includes 236 caves, with 135 remaining relatively intact. The caves exhibit a variety of architectural styles, including the Dharmagupta-influenced simpler square caves and the Sarvastivadin-associated central pillar caves. The murals in Kizil, spanning multiple stylistic periods, display influences ranging from Indian Gandhara to Iranian and Sogdian art, underscoring the cultural exchanges along the Silk Road. The caves highlight the transmission of Buddhism and its artistic traditions into China and are recognized for their archaeological and historical significance.

Gallery

Explore photographs of ancient structures, artifacts, and archaeological excavations at Kizil Caves

File2nd-century_CE_Sanskrit_Kizil_China_Spitzer_Manuscript_folio_383_fragment_verso.jpg
FileAjatasatru_Cave_Cave_219_Kizil.jpg
FileArmed_attendants_to_King_Anandavarman_Maya_Cave_205_Kizil_Caves.jpg

Archaeological Features

Explore the unique architectural and cultural elements found at this historical site

Religious and Ritual Structures

Temples

Artistic and Decorative Features

MuralsCave PaintingsInscriptions

Domestic and Habitation Structures

Caves

Historical Timeline

Journey through time and discover key events in this site's archaeological history

Plan Your Visit

Details

Country
China
Source
Wikipedia