Economic valuation of resuscitating the Dead Sea

Water Policy ◽  
2006 ◽  
Vol 8 (4) ◽  
pp. 351-370 ◽  
Author(s):  
Nir Becker ◽  
David Katz

As a result of diversion of upstream waters and intensive mineral extraction along its shores, the level of the Dead Sea is dropping at a rate of almost one meter per year, causing the sea continuously to break its own record as the lowest place on earth. The loss of the sea and the accompanying ecological and cultural damage in the basin has traditionally been regarded as an unavoidable consequence of rational economic policy. This study investigates for the first time the non-market economic value of conservation of the Dead Sea basin using both contingent valuation (stated preference) and travel cost (revealed preference) studies. Study results indicate that all three local populations, Israeli, Jordanian and Palestinian, demonstrate a substantial willingness to pay to preserve the cultural and environmental heritage of the region. Such results strengthen the case for conservation of the region, which, heretofore, has relied strictly on ethical and ecological rationales.

2006 ◽  
Vol 55 (3) ◽  
pp. 129-139 ◽  
Author(s):  
Avihu Ginzburg ◽  
Moshe Reshef ◽  
Zvi Ben-Avraham ◽  
Uri Schattner

2004 ◽  
Vol 141 (5) ◽  
pp. 565-572 ◽  
Author(s):  
YUVAL BARTOV ◽  
AMIR SAGY

A newly discovered active small-scale pull-apart (Mor structure), located in the western part of the Dead Sea Basin, shows recent basin-parallel extension and strike-slip faulting, and offers a rare view of pull-apart internal structure. The Mor structure is bounded by N–S-trending strike-slip faults, and cross-cut by low-angle, E–W-trending normal faults. The geometry of this pull-apart suggests that displacement between the two stepped N–S strike-slip faults of the Mor structure is transferred by the extension associated with the normal faults. The continuing deformation in this structure is evident by the observation of at least three deformation episodes between 50 ka and present. The calculated sinistral slip-rate is 3.5 mm/yr over the last 30 000 years. This slip rate indicates that the Mor structure overlies the currently most active strike-slip fault within the western border of the Dead Sea pull-apart. The Mor structure is an example of a small pull-apart basin developed within a larger pull-apart. This type of hierarchy in pull-apart structures is an indication for their ongoing evolution.


2019 ◽  
Vol 32 (4) ◽  
pp. 636-651 ◽  
Author(s):  
Lisa Coianiz ◽  
Uri Schattner ◽  
Guy Lang ◽  
Zvi Ben‐Avraham ◽  
Michael Lazar

Author(s):  
Yin Lu ◽  
Jasper Moernaut ◽  
Revital Bookman ◽  
Nicolas Waldmann ◽  
Nadav Wetzler ◽  
...  

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