Azokh Cave and the Transcaucasian Corridor

Please use this identifier to cite or link to this item: 192.168.6.56/handle/123456789/13936

Full metadata record

DC Field	Value	Language
dc.contributor.editor	Yolanda, Fernández-Jalvo	-
dc.contributor.editor	Tania, King	-
dc.contributor.editor	Levon Yepiskoposyan	-
dc.contributor.editor	Levon Yepiskoposyan	-
dc.date.accessioned	2018-10-24T06:49:25Z	-
dc.date.available	2018-10-24T06:49:25Z	-
dc.date.issued	2016	-
dc.identifier.isbn	978-3-319-24924-7	-
dc.identifier.uri	http://10.6.20.12:80/handle/123456789/13936	-
dc.description	Azokh Cave (also known as Azikh or Azykh) contains Pleistocene and Holocene stratified sediment infill. The site was discovered by M. Huseinov (also named Guseinov by other authors) who led the previous phase of excavations. The geographic location of the site is at an important migratory route between Africa and Eurasia. The site has yielded Middle Pleistocene hominin remains (a mandible fragment) recovered in the 1960s during a previous phase of excavation work, together with Acheulean (Mode 2) stone tools and contemporaneous fauna. An important characteristic of the Azokh 1 cave site is a continuous sedimentary record along a 7 m section, ranging in age from Middle Pleistocene (MIS 9-8) to Late Pleistocene (Mousterian industry/Mode 3, MIS 5), and to Holocene periods at the top of the series	-
dc.language	en	en_US
dc.language.iso	en	en_US
dc.publisher	Springer	en_US
dc.subject	Azokh Cave and the Transcaucasian Corridor	en_US
dc.title	Azokh Cave and the Transcaucasian Corridor	en_US
dc.type	Book	en_US
Appears in Collections:	Archeology and Heritage Management

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