The declining but non-rejuvenating base level—The Lisan lake, the Dead Sea area, Israel

1988 ◽  
Vol 13 (3) ◽  
pp. 239-249 ◽  
Author(s):  
D. Bowman
Keyword(s):  
Dead Sea ◽  
Base Level ◽  
The Dead ◽  
Sea Area

On the Origin of the Ink of the Thanksgiving Scroll (1QHodayota)

2009 ◽  
Vol 16 (1) ◽  
pp. 97-106 ◽  
Author(s):  
Oliver Hahn ◽  
Gisela Weinberg ◽  
Ira Rabin ◽  
Timo Wolff ◽  
Admir Masic
Keyword(s):  
Trace Elements ◽  
Quantitative Analysis ◽  
Spectroscopic Investigation ◽  
Dead Sea ◽  
General Validity ◽  
Production Area ◽  
The Dead ◽  
Sea Area ◽  
Non Destructive

AbstractIn this study we demonstrate the possibility to identify the production area of the scrolls, coupling non-destructive quantitative analysis of trace elements to spectroscopic investigation of the inks. This approach, that allowed us to determine the Dead Sea area as origin of 1QHodayota, is of general validity.

Sinkhole Hazard Assesment in the Dead Sea Area – Two Geophysical Aspects of the Problem

2005 ◽  
Author(s):  
M. Ezersky ◽  
A. Al-Zoubi ◽  
C. Camerlynck ◽  
S. Keydar ◽  
A. Legchenko ◽  
...  
Keyword(s):  
Dead Sea ◽  
The Dead ◽  
Sea Area ◽  
Sinkhole Hazard

Stream channel convexity induced by continuous base level lowering, the Dead Sea, Israel

Geomorphology ◽  
2007 ◽  
Vol 92 (1-2) ◽  
pp. 60-75 ◽  
Author(s):  
Dan Bowman ◽  
Yonit Shachnovich-Firtel ◽  
Shlomo Devora
Keyword(s):  
Dead Sea ◽  
Stream Channel ◽  
Base Level ◽  
The Dead ◽  
Level Lowering

Late Quaternary Geological History of the Dead Sea Area, Israel

1993 ◽  
Vol 39 (1) ◽  
pp. 59-67 ◽  
Author(s):  
Y. Yechieli ◽  
M. Magaritz ◽  
Y. Levy ◽  
U. Weber ◽  
U. Kafri ◽  
...  
Keyword(s):  
Late Quaternary ◽  
Thick Layer ◽  
Time Frame ◽  
Dead Sea ◽  
Polar Regions ◽  
Geological History ◽  
The Holocene ◽  
History Of ◽  
The Dead ◽  
Sea Area

AbstractA 34.5 m borehole, which was drilled near the Dead Sea coast (altitude -394 m) in the southern part of the fan delta of Wadi Zeelim, reveals the geological history of that area from the latest Pleistocene to present. The depositional time frame is based on six 14C dates and two U-Th dates. An erosional (or nondepositional) period is implied by the hiatus between 21,100 yr B.P. (U-Th age, depth 33 m) and 11,315 yr B.P. (14C age, depth 32 m). A subsequent arid phase is recorded by a 6.5-m-thick layer of halite; based on 14C dates this phase relates to the abrupt Younger Dryas cold period reported in temperate to polar regions. The fragility of the environment in this region is indicated by the fact that the region experienced such a severe, short aridification phase (less than 1000 yr), evidence of which is found widely in the desert fringes of the Middle East and North Africa. The aragonite found in most of the Holocene section indicates that the well site was covered by the lake for most of the Holocene. Exceptions are the intervals at 0-3 and 10-14 m depths which represent low stands of the lake.

Pterygoneurum crossidioides (Pottiaceae, Musci), a new species to the desert flora of the Dead Sea area

Nova Hedwigia ◽  
1990 ◽  
Vol 50 (1-2) ◽  
pp. 239-244 ◽  
Author(s):  
Wolfgang Frey ◽  
Ilana Herrnstadt ◽  
Harald Kürschner
Keyword(s):  
New Species ◽  
Dead Sea ◽  
The Dead ◽  
Desert Flora ◽  
Sea Area ◽  
A New Species

The genesis of the asphalt in the Dead Sea area

1979 ◽  
Vol 11 (3) ◽  
pp. 211-225 ◽  
Author(s):  
Ora Amit ◽  
Amos Bein
Keyword(s):  
Dead Sea ◽  
The Dead ◽  
Sea Area

Parameterization of a Composite Attenuation Relation for the Dead Sea Area Based on 3-D Modeling of Elastic Wave Propagation

2007 ◽  
Vol 164 (1) ◽  
pp. 23-37 ◽  
Author(s):  
Adrien Oth ◽  
Friedemann Wenzel ◽  
Hillel Wust-Bloch ◽  
Ellen Gottschämmer ◽  
Zvi Ben-Avraham
Keyword(s):  
Wave Propagation ◽  
Elastic Wave ◽  
Dead Sea ◽  
Elastic Wave Propagation ◽  
Attenuation Relation ◽  
The Dead ◽  
Sea Area
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