OBSERVATIONS ON THE HISTORY OF EARLY HEBREW (1000 B.C.E.–200 C.E.) IN THE LIGHT OF THE DEAD SEA DOCUMENTS

1992 ◽  
pp. 349-361 ◽  
Keyword(s):  
Dead Sea ◽  
Author(s):  
Steven D. Fraade

The Damascus Document is an ancient Hebrew text that is one of the longest, oldest, and most important of the ancient scrolls found near Khirbet (ruins of) Qumran, usually referred to collectively as the Dead Sea Scrolls for the proximity of the Qumran settlement and eleven nearby caves to the Dead Sea. Its oldest parts originate in the mid- to late second century BCE. While the earliest discovery of the Dead Sea Scrolls occurred in 1947, the Qumran Damascus Document fragments were discovered in 1952 (but not published in full until 1996), mainly in what is designated as Qumran Cave Four (some ten manuscripts altogether). However, it is unique in that two manuscripts (MS A and MS B) containing parts and variations of the same text were discovered much earlier, in 1896 (and published in 1910), among the discarded texts of the Cairo Geniza, the latter being written in the tenth-eleventh centuries CE. Together, the manuscripts of the Damascus Document, both ancient and medieval, are an invaluable source for understanding many aspects of ancient Jewish (and before that Israelite) history, theology, sectarian ideology, eschatology, liturgy, law, communal leadership, canon formation, and practice. Central to the structure of the overall text, is the intersection of law, both what we would call “biblical” (or biblically derived) and “communal,” and narrative/historical admonitions, perhaps modeled after a similar division the biblical book of Deuteronomy. A suitable characterization of the Damascus Document, to which we will repeatedly return, could be “bringing the Messiah through law.” Because of the longevity of its discovery, translation, publication, and debated interpretation, there is a long history of modern scholarship devoted to this ancient text.


1888 ◽  
Vol 5 (11) ◽  
pp. 502-504
Author(s):  
Edward Hull

I Have been very much interested in reading Mr. Russell's two communications published in the Geological Magazine for August and September last. The analogy which he draws between the history of the Dead Sea valley and that of some of the lake valleys in the western part of North America is instructive as showing how similar physical features can be accounted for on similar principles of interpretation over all parts of the world. Mr. Eussell very properly draws attention to the paper by his colleague Mr. G. K. Gilbert on “The Topographical Features of Lake Shores,” in which principles of interpretation of physical phenomena are laid down applicable to lakes both of America and the Jordan-Arabah valley. With some of Mr. Russell's inferences regarding special epochs in the history of this valley I am very much disposed to agree; more particularly in reference to the mode of formation of the Salt Mountain, Jebel Usdum; or rather, of the salt-rock which forms the lower part of its mass. If this interpretation be correct, it removes the difficulty of understanding why the rock-salt is confined to one small corner of the lake, which, at the time the salt was in course of formation, was vastly more extensive than at present.


1993 ◽  
Vol 39 (1) ◽  
pp. 59-67 ◽  
Author(s):  
Y. Yechieli ◽  
M. Magaritz ◽  
Y. Levy ◽  
U. Weber ◽  
U. Kafri ◽  
...  

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.


1981 ◽  
Vol 72 (1-2) ◽  
pp. 23-41 ◽  
Author(s):  
C. Tinkler ◽  
J.-J. Wagner ◽  
M. Delaloye ◽  
H. Selçuk

1961 ◽  
Vol 7 (4) ◽  
pp. 347-360 ◽  
Author(s):  
Morton Smith

I think I should begin with an apology for my temerity in accepting your invitation to discuss the Dead Sea material as a whole. Such a discussion is certainly premature while the greater part of the material is still unpublished, and while certain basic studies of the documents have yet to be made, or, at least, made public. The question of the palaeographic dating of the manuscripts, for instance, which could have great consequences for the reconstruction of the history of the sect, must remain sub judice until we have the material fully before us.


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