446 H. G. Raverty— The Mihran of Sind and its Tributaries. [Ex. No. 
north-west of Kuhram. It flows in a very deep bed.” 505 Another 
minor tributary also called the U'nbhla, will be noticed presently. 
s> 
“The Tiluhi ( a river dependent on rain, arises from the 
— 
overflow of water in the bills a little south of Nahun. Its course is 
towards the south-west, and it passes close to Sadhura on the west side; 
and a considerable distance lower down unites with the Panch Nadi, as 
the Ghag-ghar is also called after other tributaries unite with it.” 
Now, this rain-dependent river unites with the channel of the 
Markanda six miles and a half south-west of Sadhura. 
s> 
“ The next tributary westward,the Gnblila 1 )? rises in the hills 
west of Pinjor, a little to the west of the Gliag-ghar, passes west of 
Banhur, and from thence runs towards Raj-purah, about mid-way 
between Anbalah and Salirind, and passes the last-named place about 
one kuroh distant on the west side. In going to Salirind from Raj- 
purah you cross it by a brick masonry bridge, but it is now in a di¬ 
lapidated condition.” 
Where it unites with the Ghag-ghar is not said, but it seems to 
9 9 
have united with the Suweti ( ) or Ohu-hey ) a few 
M M 
miles between Sannur and Patialali ; and it now unites with a river 
called the “ Puttealawalee river ” in the maps, 606 but which, at the 
time of this Survey, does not appear to have been in existence. 
The next tributary is the Gumhtala ( ilv*). “ It conies from the 
hills south of Pinjor, and a little to the .east of where the Ghag-ghar 
rises. It takes a southerly course, and passes west of Anbalah. After 
leaving that place or the road to Salirind, after passing the kol-i-db 
[lake] outside Anbalah, one kuroh and a half north-west is that deep 
rain-dependent river, the Gumhtaila ; and you cross it by a masonry 
bridge of brick, called the Pul-i-Raj Garli, now dilapidated. Raj Garh 
itself lies half a kuroh north on a khdk-rez or artificial mound. This river 
unites with the Ghag-ghar between seven and eight kuroh farther to the 
south-west.” 
Here a vast change has occurred. The Gumhtala is no longer 
known ; and the Ghag-ghar, since the period in question, has deserted 
its former bed a little below Chhat; and instead of flowing by Banhur, 
it has entered, and flows in the old bed of the Gumhtala to within 
At the present time, its waters (or a river of the same name) unite with the 
Ghag-ghar north of Agund. It is the “ Oonbla” of the maps, 
600 This is the “ Landra,” and “ Patiala rau ” of the Gazetteers, and the 
“ Konsilla N.” of the maps, south of Patialali ; and the “ Pnttealwalle Riv.” of the 
maps, north of that place, is a mere tributary of the so-called “ Konsilla.” See 
page 449. 
