140 A SuRVEY oF THE: 
the rocks hurled from which, by the earthquake of 1803, ‘buried a small 
fort and village, which once stood here:—dreadful mementos are seen in, 
these mountains, of the effects of that catastrophe. Under O7ha Ghur, 
a stream falls into the Jumna, and several cataracts are seen falling:, 
among the surrounding precipices.—There are some hot springs at the 
bed of the Jumna, which is 400 feet below the hamlet. 
Latitude observed 30. Ze a7, 
Ldth Apel 1817,.—O/°ha Gini to Rand. 
Total distance 4. = —Iu paces 91,815. 
2655 paces aloug the mountain’s side, and descent to the Jumag.— 
Cross it.ona Sangha:of 2 small spars; its length 20 feet, breadth about, 
25 feet.—The river rushes with gréat violence. under the Sangha, and., 
nearly touches it.The general breadth of ithe. stream: is greater, but it. 
is here confined between two rocks, 
1200. paces, by ‘the margin:of: the rivers the rest, for the most sae: 
ascent, and in’some places very steep and. nisgon 
oBbeinl off is ‘a «small lang woh 1S ccaunel about 800 feet ‘above the: 
left vbank of the! river, on the slope of the) mountain ;—the general 
lower .line of snow on it, does net appear to be more than:1000 feet 
abovethe village. The opposite bank of the river-is composed of yellow | 
granite precipices, rising murally from the stream.to the height of about. 
2500) feet, or more.—The’ courses of -the. rock: ‘are: disposed almost 
horizontally, as. high’as.1000. feet. above: the -river3; but, towards the , 
