FREE BOOKS

Author's List




PREV.   NEXT  
|<   169   170   171   172   173   174   175   176   177   178   179   180   181   182   183   184   185   186   187   188   189   190   191   192   193  
194   195   196   197   198   199   200   201   202   203   204   205   206   207   208   209   210   211   212   213   214   215   216   217   218   >>   >|  
, the name Kundashpi with that of Vindaspa by Gutschmid, and, later on, Ball has added to these a long list of names in Egyptian and Assyrian inscriptions which he looks upon as Iranian. Kundashpi recalls at first sight Gundobunas, a name of the Sassanid epoch, if this latter form be authentic. Tiele adopts the identification of Kushtashpi with Vistaspa, and Justi has nothing to say against it, nor against the identification of Kundashpi with Vindaspa. The main body, finding its expansion southwards checked by Urartu, diverged in a south-easterly direction, and sweeping before it all the non-Aryan or Turanian tribes who were too weak to stem its progress, gradually occupied the western edge of the great plateau, where it soon became mainly represented by the two compact groups, the Persians to the south on the farthest confines of Elam, and the Medes between the Greater Zab, the Turnat, and the Caspian. It is probable that the kingdom founded by Deiokes originally included what was afterwards termed _Media Magna_ by the Graeco-Roman geographers. This sovereignty was formed by the amalgamation under a single monarch of six important tribes--the Buzo, Paraatakeni, Struchatas, Arizanti, Budii, and Magi. It extended north-westwards as far as the Kiziluzon, which formed the frontier between the Persians and the Mannai on this side. Northwards, it reached as far as Demavend; the salt desert that rendered Central Iran a barren region, furnished a natural boundary on the east; on both the south and west, the Assyrian border-lands of Ellipi, Kharkhar, and Arrapkha prevented it from extending to the chief ranges of the Zagros and Cordioan mountains. The soil, though less fertile than that of Chaldaea or of Egypt, was by no means deficient in resources. The mountains contained copper, iron, lead, some gold and silver,* several kinds of white or coloured marble,** and precious stones, such as topaz, garnets, emeralds, sapphires, cornelian, and lapis-lazuli, the latter being a substance held in the highest esteem by Eastern jewellers from time immemorial; Mount Bikni was specially celebrated for the fine specimens of this stone which were obtained there.*** Its mountains were in those days clothed with dense forests, in which the pine, the oak, and the poplar grew side by side with the eastern plane tree, the cedar, lime, elm, ash, hazel, and terebinth.**** * Rawlinson has collected t
PREV.   NEXT  
|<   169   170   171   172   173   174   175   176   177   178   179   180   181   182   183   184   185   186   187   188   189   190   191   192   193  
194   195   196   197   198   199   200   201   202   203   204   205   206   207   208   209   210   211   212   213   214   215   216   217   218   >>   >|  



Top keywords:
mountains
 

Kundashpi

 

identification

 
Persians
 
tribes
 
Vindaspa
 

Assyrian

 

formed

 

Chaldaea

 

Mannai


frontier
 
Northwards
 

fertile

 

reached

 

copper

 

contained

 

Demavend

 

Kiziluzon

 

deficient

 

resources


Cordioan
 

silver

 

Ellipi

 
region
 

Kharkhar

 
border
 
natural
 

boundary

 

Arrapkha

 

barren


rendered

 

Zagros

 
desert
 
furnished
 

Central

 
ranges
 

prevented

 

extending

 

cornelian

 

clothed


forests

 

specimens

 
obtained
 

poplar

 
terebinth
 
Rawlinson
 

collected

 

eastern

 
garnets
 

emeralds