Details zur Publikation

Kategorie Textpublikation
Referenztyp Zeitschriften
DOI 10.1002/gea.21517
Volltext Shareable Link
Titel (primär) Long-term sediment export estimates from northern Jordan using Roman cisterns as sediment traps
Autor Kraushaar, S.; Ollesch, G.; Siebert, C. ORCID logo ; Vogel, H.-J.; Fuchs, M.
Quelle Geoarchaeology
Erscheinungsjahr 2015
Department BOPHY; CATHYD
Band/Volume 30
Heft 4
Seite von 369
Seite bis 378
Sprache englisch
Supplements https://onlinelibrary.wiley.com/action/downloadSupplement?doi=10.1002%2Fgea.21517&file=gea21517-sup-0001-supMat.docx
UFZ Querschnittsthemen RU1
Abstract Roman cisterns served as rainwater storage devices for centuries and are densely distributed in parts of northern Jordan. A major earthquake hit the region ca. A.D. 750 and in a short time many settlements were abandoned. As a consequence, most cisterns were not maintained, and they filled with sediments that today provide a postabandonment depositional record. In two field surveys, we mapped the locations of more than 100 cisterns in the Wadi Al-Arab basin and selected two for detailed stratigraphic analysis that included 14C and optically stimulated luminescence dating. Catchment basin area for each cistern was determined by differential GPS. Both cisterns filled with sediments after the great earthquake and consequent abandonment of the region. Calculated sediment volumes are translated to long-term average sediment export rates of 2.6–6.6 t ha−1a−1, which are comparable to erosion and sediment yield rates from other studies within the Mediterranean region. Our pilot study suggests that this approach can be applied elsewhere to calculate long-term sediment export rates on hill slopes containing relict cisterns.
dauerhafte UFZ-Verlinkung https://www.ufz.de/index.php?en=20939&ufzPublicationIdentifier=16336
Kraushaar, S., Ollesch, G., Siebert, C., Vogel, H.-J., Fuchs, M. (2015):
Long-term sediment export estimates from northern Jordan using Roman cisterns as sediment traps
Geoarchaeology 30 (4), 369 - 378 10.1002/gea.21517