Taconian ultramafic tectonic "sliver" located along a major regional thrust fault at the top of the Rowe formation, separating it from the Moretown formation. [Note: This site is a small botanical preserve, due to the calciophilic species found growing on the talc-serpentine ledges. Collecting is not allowed. The same minerals - plus others - are found at the nearby Massachusetts talc mine; so there is no need to disturb the plant community on the ledges.]
Mineral List
5 entries listed. 4 valid minerals.
The above list contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please
register so you can add to our database. This locality information is for reference purposes only. You should never attempt to
visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders
for access and that you are aware of all safety precautions necessary.
Mineral and Locality Search
