Lead Mines, &¢. of Hampshire County, Muss. 268 
that the granite veins as well as the hornblende veins, fre- 
quently connect beds of their respective roc together, an 
sometimes seem to connect together different vein 
The best place for viewing granite veins in granite, is two 
miles south of the meeting-house in Williamsburgh, on t 
road to Shepard’s manufactory, on the land of Mr. William 
Pomeroy. This locality is in full view as we pass along the 
road, and ean scarcely fail to attract the attention of the ge- 
ologist. 
Fi e mm 
granite vein, three feet wide, 
SS e vein, mm, to the other 
side, and then running padallet oy sgsih. 
Fig. 2. Here H HE H CH represent mica slate lying next 
to granite aaaaa, with a granite vem, eight inches er 
in it, running parallel with the strata. This v 
two branches d d, across the strata of mica slate, which lie in 
¥ into granite lying next the mica slate : 
these branches have a focus at m, with another granite vein 
ten inches wide, but in granite. 
