Cii.vr. XXXVI] 
NACJrUR : GUGrLDOHO. 
947 
more difficult than usual to work by open-cast methods. Thus, in 
many ])laces it will not bo possible to make deep trenches across the 
deposit in order to show its true width and character, owing to the 
fact that the north end of the trench would have to be cut out of 
solid quartzites. Still the slope of the hill is usually not too steep for 
the necessary dead- work to be done to allow the deposit to be 
scientifically worked, for it must not be overlooked that being on a hill 
side it will be possible to work it to a much greater depth, as far as 
drainage troubles are concerned, than a deposit situated in alluvial 
fields. 
The figures of output from this deposit from 
Output. ^^^^ ^^^^ shown below:— 
Year. Long tons. 
1904 5,57G 
1905 8,227 
190fi ]r),.525 
1907 11,270 
24. Guguldoho 
(Jessop & Co.) 
The situation of this deposit is shown in figure 71 on page 943, from 
which it will be seen that this is probably only a continuation of the 
Manegaon ore-band, which, as explained on page 943, either dies out 
temporarily or dives below the quartzite hill separating these two de- 
posits. The Guguldoho portion of the band was traced for another 
mile and a half to the east to the boundary between the Nagpur and 
Bhandara districts and then on the other side of the boundary for some 
300 to 400 yards. 
The total length of the portion of the Manegaon-Guguldoho band 
lying in the Nagpur district is thus about 3 miles. The Asalpani deposit, 
lying some 13 miles east by north from this point on the Nagpur- 
Bhandara boundary, may possibly be a continuation of this band, 
especially as ore is reported as having been found recently in the 
interevning ground. 
The strike of the ore-band averages east to west at the west end and 
curls round to east by south at the east end. The dip is usually very 
steep, often vertical, and invariably, as far as seen, to the south side 
of the strike. 
IV z 
