CATALOGUE. 



39 



160. BlJEEAGOGABH .. 



161. Gcjpt Gudaoli 



162. Manikpue 



163. Kandela 



164. Huema 



165. Gandttaei 



166. SlEGTTJA 



Lat. 24° 00' ; Long. 80° 41' ; Elev. ; Temp. 



A warm spring is said to exist about quarter of a mile 

 east of the town.— Official Records. 

 Lat. 25° 05'; Long. 80° 50'; Elev. ; Temp. 



It is 2 or 5 miles south of Puldeo. In the Atlas of India 

 it is marked as a village, but it is merely a spring, 

 near which there may be a few huts for Brahmins, as it is 

 a place of pilgrimage. It issues from a cave, which can be 

 entered crouching, and is warm. — J. P. Stralton in epist. 

 Lat. 25° 04'; Long. 81° 08'; Elev. ; Temp. 



Close to Manikpur, about half a mile in a jungle called 

 Chururgar : water, though hot at first, soon cools down. — 

 Official Returns. 

 Lat. 25° 05' ; Long. 81° 16' ; Elev. ; Temp. 



About 10 miles east and north from Manikpur, on the 

 Eewah frontier, 7 miles south-west of the village of Kotha 

 Kandela. — Official Returns. 

 . Lat. 24° 31'; Long. 82° 33'; Elev. abt.700; Temp. 



This spring is opposite to Hurma, a village on the north 

 bank of the Sone, and between the villages of Chucki and 

 Gangi, about 3 miles east of Khyra and 10 east of 

 Burdhi. Water clear, has no taste, and leaves no deposit. 

 The spring is on the south bank of the river near the 

 stream, near the village of Gangur. — F. R. Mallei, Geol. 

 Surv., India. 

 Lat. 23° 36' ; Lang. 83° 18' : Elev. abt. 1,800 ; Temp. 

 About 4 miles due east of Seersa hill, close to the road 

 from Pertabpur to the north ; much frequented by wild 

 animals on account of the lick. — V. Ball, G. S. I. 

 , Lat. 23° 41'; Long. 83° 42'; Elev. 1,460; Temp. 186°. 



In Sirguja, commonly called Tattapani (hot water), springs 

 rise over a large space which is always covered with the 

 vapour from the hot water. — Breton, Med. Top. of Ceded 

 Provinces, 1826, page 4. These springs constitute by 

 their number and copious outpourings a very remarkable 

 and, in this part of India at least, a unique, display. They 

 are all arranged, with one exception, on or in the imme- 

 diate vicinity of a strong ridge of pseudomorphic quartz 

 and breccia, which evidently marks a line of fracture. It 

 is not easy to say how many distinct active springs there 

 are .at Tattapani ; but these were seen by me certainly 



( 137 ) 



