Landscapes and Societies 2010
DOI: 10.1007/978-90-481-9413-1_9
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Empire and Environment in the Northern Fertile Crescent

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Cited by 10 publications
(14 citation statements)
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“…Higher up these mountains, within traditional summer pasture zones ( yayla ), medieval and modern settlement is more rare, and sites of Roman and late Roman date are often easier to recognize, as at the large upland village of Karacaoluk Yaylası (AS 334; Casana ), located at nearly 1000 masl. Sites like this one, up to the highest altitude site recorded in the Amanus, AS 225 (Casana , 546), a small cluster of buildings at nearly 1800 masl, suggest the existence of highly specialized agricultural production or other activities, as they are above the altitude which can support traditional mixed cultivation of olive, grape and cereals (Wilkinson , 142).…”
Section: Regional Surveysmentioning
confidence: 90%
“…Higher up these mountains, within traditional summer pasture zones ( yayla ), medieval and modern settlement is more rare, and sites of Roman and late Roman date are often easier to recognize, as at the large upland village of Karacaoluk Yaylası (AS 334; Casana ), located at nearly 1000 masl. Sites like this one, up to the highest altitude site recorded in the Amanus, AS 225 (Casana , 546), a small cluster of buildings at nearly 1800 masl, suggest the existence of highly specialized agricultural production or other activities, as they are above the altitude which can support traditional mixed cultivation of olive, grape and cereals (Wilkinson , 142).…”
Section: Regional Surveysmentioning
confidence: 90%
“…to C.E. 1000) that we see some increases in valley floor aggradation (Wilkinson ). Unfortunately, because valley floors receive episodic delivery of sediments from the neighboring terrain and sedimentation rates vary depending upon local geomorphology and river basin conditions, it is difficult to quantify rates of erosion and sedimentation.…”
Section: Introductionmentioning
confidence: 82%
“…Here we focus on the later sedimentary sequences from the valley in the Carchemish and Kurban Höyük areas (Fig. 1) which provide compelling evidence for a later phase of colluviation (Wilkinson 2010) and which followed on from earlier alluvial fills (Miller-Rosen and Goldberg in Algaze 1995; Pournelle in Algaze et al 2001: 59). At the river basin scale, the complex alluvial fills of the Euphrates River have been interpreted as demonstrating the following chronological sequence:…”
Section: The Middle Euphratesmentioning
confidence: 99%