0379981 - GLÚ 2013 RIV CZ eng M - Část monografie knihy
Cílek, Václav - Lisá, Lenka - Bárta, M.
The Holocene of the Abusir area.
Abusir and Saqqara in the year 2010.. Vol. 1. Prague: Czech Institute of Egyptology, Faculty of Arts, Charles University in Prague, 2011 - (Bárta, M.; Coppens, F.; Krejčí, J.), s. 312-326. ISBN 978-80-7308-384-7
Výzkumný záměr: CEZ:AV0Z30130516
Klíčová slova: Abusir * Lake of Abusir * cemetery entrance * geology * sedimentology
Kód oboru RIV: DB - Geologie a mineralogie

The background geomorphology of Abusir lako and other depressions under the steep slopes of the Abusir and Saqqara area were very probably formed by and older, now abandoned early-Middle Holocene river course. The change of sedimentaytion from a fluvial to an aeolian one happened some 10 cm above the horizon dated to the interval between the Third to Fift Dynasty of the Old Kingdom, which means after approx. 2460 BC.
Trvalý link: http://hdl.handle.net/11104/0210820