TY - JOUR
T1 - Late Quaternary deposition and erosion processes along the margins of the Yamin Plain, northeast Negev, Israel
AU - Dody, Avraham
AU - Nahlieli, Ariel
AU - Avni, Yoav
AU - Cohen, Hai
AU - Weiner, David
AU - Porat, Naomi
PY - 2008/12/1
Y1 - 2008/12/1
N2 - This study presents rates of accumulation and transport of sands as well as rates of incision along the margins of the Yamin Plain, northeastern Negev, and evaluates the stability of the present landscape. Geomorphological mapping, OSL and 14C dating, and sedimentological analyses suggest that rates of erosion range between ~45 mm/year in the eastern side of the study area and 0.05 mm/y on the western side. The calculated erosion rates show that, until recently, geomorphic processes in the eastern part of the plain were dominated by accumulation of sands derived from the Hazeva Group. However, accelerated erosion is observed near the contact between the sand units and the carbonate bedrock of the Judea Group. It appears that the area west of the plain has been stable during the last glacial (circa 73-18 ka). We suggest that the exclusion of domestic grazing from the Yamin Plain in the 1950s changed the balance between erosion and sedimentation and caused accelerated erosion mainly in the eastern part of the Yamin Plain by decreasing infiltration and increasing runoff.
AB - This study presents rates of accumulation and transport of sands as well as rates of incision along the margins of the Yamin Plain, northeastern Negev, and evaluates the stability of the present landscape. Geomorphological mapping, OSL and 14C dating, and sedimentological analyses suggest that rates of erosion range between ~45 mm/year in the eastern side of the study area and 0.05 mm/y on the western side. The calculated erosion rates show that, until recently, geomorphic processes in the eastern part of the plain were dominated by accumulation of sands derived from the Hazeva Group. However, accelerated erosion is observed near the contact between the sand units and the carbonate bedrock of the Judea Group. It appears that the area west of the plain has been stable during the last glacial (circa 73-18 ka). We suggest that the exclusion of domestic grazing from the Yamin Plain in the 1950s changed the balance between erosion and sedimentation and caused accelerated erosion mainly in the eastern part of the Yamin Plain by decreasing infiltration and increasing runoff.
UR - http://www.scopus.com/inward/record.url?scp=69549116843&partnerID=8YFLogxK
U2 - 10.1560/ijes.57.3-4.199
DO - 10.1560/ijes.57.3-4.199
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AN - SCOPUS:69549116843
SN - 0021-2164
VL - 57
SP - 199
EP - 211
JO - Israel Journal of Earth Sciences
JF - Israel Journal of Earth Sciences
IS - 3-4
ER -