La crise d'aridité climatique de la fin du 3ème millénaire av. J.-C., à la lumière des contextes géomorphologique de 3 sites d'Iran Oriental (Bam, Tepe Damghani, Jiroft)

The climatic aridity in the late third millennium is a fact attested by the paleo-climate reconstructions for the Near and Middle East as well in Central Asia. The question is what are the consequences of climate aridity for human societies and how they have adapted. The geomorphological study of Sa...

وصف كامل

محفوظ في:
التفاصيل البيبلوغرافية
المؤلف الرئيسي: Fouache, Eric (author)
مؤلفون آخرون: Francfort, Henri-Paul (author), Cosandey, Claude (author), Adle, Chahryar (author)
منشور في: 2015
الموضوعات:
الوصول للمادة أونلاين:http://hdl.handle.net/20.500.12458/7
https://www.scopus.com/inward/record.uri?eid=2-s2.0-84957641865&partnerID=40&md5=72b71a46fa8f797b4e5be04ebc56ce4a
الوسوم: إضافة وسم
لا توجد وسوم, كن أول من يضع وسما على هذه التسجيلة!
_version_ 1857415062759669760
author Fouache, Eric
author2 Francfort, Henri-Paul
Cosandey, Claude
Adle, Chahryar
author2_role author
author
author
author_facet Fouache, Eric
Francfort, Henri-Paul
Cosandey, Claude
Adle, Chahryar
author_role author
dc.creator.none.fl_str_mv Fouache, Eric
Francfort, Henri-Paul
Cosandey, Claude
Adle, Chahryar
dc.date.none.fl_str_mv 2015
2018-10-07T10:38:53Z
2018-10-07T10:38:53Z
dc.identifier.none.fl_str_mv http://hdl.handle.net/20.500.12458/7
10.1515/9783110331707.27
https://www.scopus.com/inward/record.uri?eid=2-s2.0-84957641865&partnerID=40&md5=72b71a46fa8f797b4e5be04ebc56ce4a
dc.language.none.fl_str_mv fr
dc.publisher.none.fl_str_mv Walter de Gruyter GmbH
dc.relation.none.fl_str_mv Greater Khorasan : History, Geography, Archaeology and Material Culture
29
27
37
9783110331707
dc.subject.none.fl_str_mv Géomorphologie
Paléoclimat
Plateau Iranien
Eau
Aridité
dc.title.none.fl_str_mv La crise d'aridité climatique de la fin du 3ème millénaire av. J.-C., à la lumière des contextes géomorphologique de 3 sites d'Iran Oriental (Bam, Tepe Damghani, Jiroft)
dc.type.none.fl_str_mv Controlled Vocabulary for Resource Type Genres::text::book::book part
description The climatic aridity in the late third millennium is a fact attested by the paleo-climate reconstructions for the Near and Middle East as well in Central Asia. The question is what are the consequences of climate aridity for human societies and how they have adapted. The geomorphological study of Sabzevar in northeastern Iranian Plateau, Bam and Jiroft in southeastern of the same Plateau, shows that between the Chalcolithic and Iron Age water resources diminish but,thanks to favourable trapping groundwater tectonic settings, human societies adapt to changing location and adopting new irrigation techniques, in this case the qanats.
id sorbonner_cfd087c35272b60fc6fa6971d64ee237
identifier_str_mv 10.1515/9783110331707.27
language_invalid_str_mv fr
network_acronym_str sorbonner
network_name_str Sorbonne University Abu Dhabi repository
oai_identifier_str oai:depot.sorbonne.ae:20.500.12458/7
publishDate 2015
publisher.none.fl_str_mv Walter de Gruyter GmbH
repository.mail.fl_str_mv
repository.name.fl_str_mv
repository_id_str
spelling La crise d'aridité climatique de la fin du 3ème millénaire av. J.-C., à la lumière des contextes géomorphologique de 3 sites d'Iran Oriental (Bam, Tepe Damghani, Jiroft)Fouache, EricFrancfort, Henri-PaulCosandey, ClaudeAdle, ChahryarGéomorphologiePaléoclimatPlateau IranienEauAriditéThe climatic aridity in the late third millennium is a fact attested by the paleo-climate reconstructions for the Near and Middle East as well in Central Asia. The question is what are the consequences of climate aridity for human societies and how they have adapted. The geomorphological study of Sabzevar in northeastern Iranian Plateau, Bam and Jiroft in southeastern of the same Plateau, shows that between the Chalcolithic and Iron Age water resources diminish but,thanks to favourable trapping groundwater tectonic settings, human societies adapt to changing location and adopting new irrigation techniques, in this case the qanats.Walter de Gruyter GmbH2018-10-07T10:38:53Z2018-10-07T10:38:53Z2015Controlled Vocabulary for Resource Type Genres::text::book::book parthttp://hdl.handle.net/20.500.12458/710.1515/9783110331707.27https://www.scopus.com/inward/record.uri?eid=2-s2.0-84957641865&partnerID=40&md5=72b71a46fa8f797b4e5be04ebc56ce4afrGreater Khorasan : History, Geography, Archaeology and Material Culture2927379783110331707oai:depot.sorbonne.ae:20.500.12458/72024-02-05T06:29:45Z
spellingShingle La crise d'aridité climatique de la fin du 3ème millénaire av. J.-C., à la lumière des contextes géomorphologique de 3 sites d'Iran Oriental (Bam, Tepe Damghani, Jiroft)
Fouache, Eric
Géomorphologie
Paléoclimat
Plateau Iranien
Eau
Aridité
title La crise d'aridité climatique de la fin du 3ème millénaire av. J.-C., à la lumière des contextes géomorphologique de 3 sites d'Iran Oriental (Bam, Tepe Damghani, Jiroft)
title_full La crise d'aridité climatique de la fin du 3ème millénaire av. J.-C., à la lumière des contextes géomorphologique de 3 sites d'Iran Oriental (Bam, Tepe Damghani, Jiroft)
title_fullStr La crise d'aridité climatique de la fin du 3ème millénaire av. J.-C., à la lumière des contextes géomorphologique de 3 sites d'Iran Oriental (Bam, Tepe Damghani, Jiroft)
title_full_unstemmed La crise d'aridité climatique de la fin du 3ème millénaire av. J.-C., à la lumière des contextes géomorphologique de 3 sites d'Iran Oriental (Bam, Tepe Damghani, Jiroft)
title_short La crise d'aridité climatique de la fin du 3ème millénaire av. J.-C., à la lumière des contextes géomorphologique de 3 sites d'Iran Oriental (Bam, Tepe Damghani, Jiroft)
title_sort La crise d'aridité climatique de la fin du 3ème millénaire av. J.-C., à la lumière des contextes géomorphologique de 3 sites d'Iran Oriental (Bam, Tepe Damghani, Jiroft)
topic Géomorphologie
Paléoclimat
Plateau Iranien
Eau
Aridité
url http://hdl.handle.net/20.500.12458/7
https://www.scopus.com/inward/record.uri?eid=2-s2.0-84957641865&partnerID=40&md5=72b71a46fa8f797b4e5be04ebc56ce4a