ee a ee a 
Miscedlaneous Localities of Minerals. 58 
perhaps three to four thousand dozen, which are disposed 
of in New-England, New-York and Philadelphia—75 cents 
a dozen are obtained for them 
30. Slate, —— Faces: one mile N. W. from 
Woes Vil 
. ‘Ste Basal, Reed in two dikes or walls c crossing the 
Bean } ip ee the 
Blackstone, at the Branch Factory, a few 
running about N. E. and S. W. consisting of columns of 
various sizes and figures in mica-slate. 
$2 and 33. S vente overlying argillite, in immense 
ledges near the Blackstone, in Cumberland and Smit 
some eras it is Eaawed = perpendicular veins of white 
a pe “Argillite, on the banks and near the Blackstone un 
pe the sandstone. Cumberland and Smithfield. 
3. Granit ite, Cumberland, a ridge running N. and 8. be- 
Pe ont Cumberland Hill and Diamond Hill. ‘ 
36. N. W. from Diamond Hill and E. of the granite. 
37 and 33. Quartz, fair specimens of the formnaton of 
“Diamond Hill.’ 
39. Anthracite, Cumberland. 
40. Anthracite, North Providence. 
41 and 42. pels: do. at Valley Falls. 
43. Limestone, and 
44. The “Argillite, which accompanies it North Prov- 
“sag 
5, 46, 47, and 48. A suit of the Gray Wacke slate 
of Patch Falls and village. 
d 50. Magnetic Iron stone. This singular stone is 
very = a Sg in rounded masses, scattered over the sur- 
face about Cumberland Hill, Providence, and in Foster. 
I intended to have added to the foregoing specimens 
more detailed and correct sketch of the Geology fic. of 
this state, which for want of leisure and better health, I 
must postpone 
Providence, July 31, 1824, 
