"To the drying up of the Hakra, or Gliaggar, many centuries ago, in conjunction with moral evils, is ascribed the existing desolation. According to tradition, this stream took a westerly direction, by Phidra, where it is yet to be traced, and fell into the Indus below Uchh. The couplet recording its absorption by the sands of Ner has already been given, in the time of Rao Hamir, prince of Dhat. If the next European traveller who may pass through the Indian desert will seek out the representative of the ancient Sodha princes at Chor, near Umarkot, he may learn from their bard (if they retain such an appendage) the date of this prince, and that of so important an event in the physical and political history of their regions. The vestiges of large towns, now buried in the sands, confirm the truth of this tradition, and several of them claim a high antiquity ; such as the Rangmahall, already mentioned, west of Bhatner, having subterranean apartments still ill good preservation. An aged native of Daudusar (twenty- five miles south of Bhatner) replied, to my inquiry as to the recollections attached to this place, that “ it belonged to a Panwar prince who ruled once all these regions, when Sikandar Riimi attacked them.”"