2 Hydrogeology
Sunday, 28 October 2007
8:00 AM - 12:00 PM
VALLEY OF KINGS, POSITIVE AND NEGATIVE YUCCA MOUNTAIN ANALOGUES
Paper number: 2-2
Program: Technical Sessions
Time: 8:15 AM – 8:30 AM
Authors
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Katarin A. ParizekThe Pennsylvania State University, Univesity Park, PA
Abstract
63 tombs are known in the Valley of Kings, Luxor, Egypt. Some date from 1550 to 1100 centuries BC. Water remains the single most destructive agent. Some have been badly damaged by flooding of unprotected entrances. All continue to be damaged by vadose water that migrates along joints, fractures, zone of fracture concentration and faults within Thebes Limestone (Eocene). Even during smaller storms, surface water accumulates within exposed fractures, contributing to episodic flow. Damage to interior decorations is cumulative and is more intense at structural intersections. Roof collapse is especially serious in KV- 13, 18, 32 and 47. Rock falls have raised ceilings by 2.4 m even where passages are only 1.5 to 2 m wide. 1.0 to 2.0 m-sized blocks have fallen in some passages closed for safety. Tunnel stability is related to structure, changes in water content, flooding, excessive stone removal, stacking of tombs and unstable substrate. The Valley of Kings could afford YMP scientists and engineers new examples of both positive (e.g. artifact preservation within the vadose zone) and negative analogues (episodic flow and tunnel stability).