کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
6538931 | 158706 | 2013 | 10 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
Holocene geomorphology, tectonics, and archaeology in Barrancas, arid Central Andes piedmont (33°S)
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کلمات کلیدی
موضوعات مرتبط
علوم زیستی و بیوفناوری
علوم کشاورزی و بیولوژیک
جنگلداری
پیش نمایش صفحه اول مقاله
![عکس صفحه اول مقاله: Holocene geomorphology, tectonics, and archaeology in Barrancas, arid Central Andes piedmont (33°S) Holocene geomorphology, tectonics, and archaeology in Barrancas, arid Central Andes piedmont (33°S)](/preview/png/6538931.png)
چکیده انگلیسی
Archaeology and geomorphology are closely linked in Barrancas, Argentina, where both disciplines are necessary to understand human-environment interactions during the Holocene. The geomorphology suggests that the area was located in a distal alluvial environment of the Zonda paleo-river that drained to the east. Active tectonics during the Pliocene-Early Pleistocene caused the gradual uplift of the Lunlunta Sierras to the southwest, which led to the bifurcation of the paleo-river. For most of the Holocene, the area was seasonally flooded, suggesting a lacustrine microenvironment. A long record of human occupation beginning in the Early Holocene suggests an extended period of intimate human-environment interactions. Recently, the environment has shifted dramatically. Erosion has created a badlands and significantly impacted the archaeological record. Understanding geomorphological processes is central for archaeological research in general, and especially in Barrancas. This research is an integral part of the ongoing community archaeology program in the area, and for the planned creation of an archaeological reserve.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Applied Geography - Volume 42, August 2013, Pages 217-226
Journal: Applied Geography - Volume 42, August 2013, Pages 217-226
نویسندگان
Stella Moreiras, Erik Marsh, Hugo Nami, Diego Estrella, VÃctor Durán,