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Its water is at times wholly consumed in the cultivation of the plain; but the natural course may be traced, running in a southerly and south-westerly direction, until it debouches from the hills in the vicinity of Tersheez. The Miyanabad stream is believed to be a tributary of the Gurghan.

Hyrcania was, as already observed, the western and north-western portion of that broad mountain region which has been described as intervening between the eastern shores of the Caspian and the river Arius, or Heri-rud. It consisted mainly of the two rich valleys of the Gurghan and Ettrek, with the mountain chains inclosing or dividing them.

It rises from several sources in the transverse range joining the Alatagh to the Jaghetai, the streams from which all flow westward in narrow valleys, uniting about long. 57° 35'. The course of the river from this point to Piperne has not been traced, but it is believed to run in a general westerly direction along the southern base of the Alatagh, and to form a junction with the Gurghan a little below the ruins of the same name.

The evidence goes, on the whole, to show that, while Hyrcania lay towards the west and north, the Parthian country was that towards the south and east, the valleys of the Ettrek and Gurghan constituting the main portions of the former, while the tracts east and south of those valleys, as far as the sixty-first degree of E. longitude, constituted the latter.

The central and southern ranges are connected by a more decided, mountain line, a transverse ridge which runs nearly north and south, dividing between the waters that flow westward into the Gurghan, and those which form the river of Nishapur.