230 Miascellancous Localities of Minerals. 
, if properly managed. Many specimens ns He been 
sent 14 to be cut and polished by Davis & Babbitt, lap- 
idaries, and to be set by Col. Baker, for es bles ear- 
in considerable quantities, is found at the locality of yenite, 
3 epidote, &c. in Cumberland. We occasionally 
‘meet with specimens of soiree ne quartz, contaaaee 
within them small crystals of yen 
Amethyst is found on the bodice of the Blackstone River, 
in Cumberland. We have not had an opportunity as yet 
of examining this locality, sufficiently to decide whether it 
will probably provetobeasimportantasthatatBristel. 
Very large crystals “$i sane of the common bean 
per! ect terminatior ness Hill. 
ve ? ibe dee BY THE EDITOR. 
Prof. wey, at p. 50 of our last ae eo ae 
ed the Aish pie oF applying the na icu r- 
of tale ibed 2, Xi 
3, in vindication of the 
but we conceive it Bessy to oablich his remnant at 
large, because his reasons are sufficiently explained i in coe 
original Spa oad already alluded to. 
n confirmation of Mr. Webb’s observations as to the eu- 
us effec bok heat, we would add, that specimens brought 
‘us, two or three years ago, from the same locality, by 
J D.S. 8. a H. Smith, of Sutton, exhibited under the 
ypipe the same hy ead which are so soohentely 
described by ion ad ebb. 
3. By Dr. Samven Rosrnson. 
Prosiguiok R. I, March 25, 1924. 
aan, Gounskeaias Prase sandtaled with actynolite 1 ga . 
east of . Eee raw Beraaeda which is about 1 ci 
N Prividenis : 
ies 
: ive 
* Mowe ar Tal, or either itses oF then; will excange 
ip of other States. 
