err 
Geolooy, Yc. of the Connecticut. 223 
icate poppy red, much resembling some varieties of the ru- 
oy 
“Tt scratches crystallized quartz,” says Professor 
Dewey, “and melts, rather hardly, into a dark . 
Found in digging 4 a well. 
2. Colophonite. At Conway ? 
0. Magnesian Garnet. At Haddam. wen Cleaveland’s 
Min Vol. * p- 777 
41. Epidote. At Milford Hills, in nie. greenstone. 
(Stdliman.). Also at Litchfield and Washington, in graphic 
granite and an: segeeeliaee (Brace.) Also at Had- 
dam, crystallized. ‘Also ite Nand. (Webster.) Also at 
Athol, Worcester county, ‘Mas in prismatic bladed crys- 
tals, associated with black aunad schorl and hornblende. 
Also in Shutesbury, in smal] crystals in gneiss. It occurs 
also ina great many other places, mat oncnpciigs in various 
rocks, and not very interesting. 
. Zoisite. At Haddam. (Webster.) Also at Wardsbo- 
Be Vermont, in much compressed, greenish grey, pris- 
matic crystals; sometimes a foot long and ae or two inch- 
es wide. (Dewey.) Discovered by Dr. Allen. Also 
at eyes Brattleborough and Woteoinek ( Hall.) 
. Arenaceous Epidote.. At Haddam. (Webster.) Also 
at ees Leyden, Shelburne, Buckland, Whate ely, 
Belchertown, ee ‘and a great number of Placery in 
hornblende and greenstone slate. 
42. Prehnite. Near New- Haven, in secondary green- 
stone, in radiated masses, or in veins. Also at Woodbury, 
in the same sort of rock, in mammillary, botryoidal and al- 
most globular masses. (Silliman.) Also Retpeen Simsbury 
an -Wintonbary, in mammillary masses in greenstone. 
(Hayden.) Also in Deerfield, candied; and, indeed, in 
algae every part of the secondary greenstone ranges from 
New-Haven to Gill; in all the forms mentioned above. In 
Deerfield the radiated masses sometimes contain pyritous 
Copper. They occur there, also, on pseudomorphous quartz, 
having evidently been peed since the decomposition of 
the crystals originally occupying the cavities. In the same 
