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Lambert Road serpentinite, Orange, New Haven Co., Connecticut, USA

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During road realignment and construction of a commercial building in the fall of 1984 through summer of 1985, a small serpentinite body and surrounding metamorphic rock was blasted. The serpentinite is one of several similar lenses mapped by Fritts (1965) as "Odl" (Ordovician Derby Hill Schist, limestone member) and paralleling the south side of Route 1 from the Baldwin Quarry in Milford NE to the Maltby Lakes in New Haven. The geology and mineralogy is essentially identical to that found at the Baldwin Quarry. No outcrops remain at the construction site, but about 150 meters NE along the strike there are exposures near some retail shops.

Mineral List



16 entries listed. 13 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.

References

- Fritts, Crawford E. (1965): Bedrock Geologic Map of the Ansonia Quadrangle, Fairfield and New Haven Counties, Connecticut. USGS Map GQ-426.
- Weber, Marcelle H. and Earle C. Sullivan. (1995): CONNECTICUT MINERAL LOCALITY INDEX. Rocks & Minerals (Connecticut Issue), Volume 70, No. 6, p. 403.

Mineral and/or Locality  
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