[ 208 ] 
tation the patient had now and then felt during his 
laft: illnefs. It weighed only about a grain. 
No parts could have a founder appearance than 
both the ureters and kidneys. The firft were not 
dilated ; nor did the laft contain any ftone, mucus, or 
gravel : the pelvis in each was of a natural fize. 
The reft of the abdominal vi/cera were in the fame 
healthful ftate, except the gall-bladder, which was 
full of ftones. The largeft was about the fize of a 
fmall chefnut, but rounder. The furface was fmooth, 
particularly at one part, where it feemed to have 
rubbed upon a lefler calculus , of the fhape of one of 
the 'certebrce of a fmall animal, without the proceftes. 
This laft had a hollow on each fide correfponding to 
the convexity of the large ftone ; and thefe cavities 
being finely polifhed, it feemed as if fometimes one 
fide, fometimes the other, of the fmall ftone had been 
turned to the great one, and had been fhaped in that 
manner by the attrition. The largeft calculus weighed 
one drachm two fcruples and two grains ; the fmall 
one but nine grains : they both funk in water ; and 
felt fpecifically heavier than any ftones I have ever feen 
taken out of the gall-bladder. Befides thefe two, there 
were feveral very fmall calculi of irregular fhapes, and 
of rough furfaces, which all together did not weigh 
above five grains. Mr. Graham, who had attended 
his Lordfhip for about 40 years, aflured me, that he 
never had any fymptom that indicated a ftoppage of 
the bile, or the pafiage of a ftone from the gall-bladder 
into the inteftines. 
Neither the head nor breaft were opened. 
Thefe are all the materials, I can furnilh you with, 
.relating to this cafe. If you defire to be more parti- 
cularly 
