Waits River Formation
The Waits River Formation is a late Silurian to early Devonian limestone containing lesser amounts of phyllite and schist.
Waits River Formation Stratigraphic range: late Silurian to early Devonian | |
---|---|
Type | sedimentary, metamorphic |
Sub-units | Standing Pond Volcanic Member |
Underlies | Bradford Schist |
Lithology | |
Primary | limestone |
Other | phyllite, schist |
Location | |
Region | New England |
Country | USA |
Extent | Vermont, Massachusetts, New Hampshire |
Type section | |
Named for | Village of Waits River (within Topsham) and stream |
Named by | C. H. Richardson, 1906[1] |
The description by the USGS is:
- Gray quartzose and micaceous crystalline limestone weathered to distinctive brown earthy crust; interbedded and intergradational with gray quartz-muscovite phyllite or schist. Where more metamorphosed the limestones contain actinolite, hornblende, zoisite, diopside, wollastonite, and garnet, and the phyllite and schist, biotite, garnet, and locally andalusite, kyanite, or sillimanite.[2]
References
- Richardson, C.H., 1906, THE AREAL AND ECONOMIC GEOLOGY OF NORTHEASTERN VERMONT. From the Fifth Report Vermont State Geologist. Argus and Patriot Press, Montpelier, Vermont.
- Waits River Formation, Mineral Resources On-Line Spatial Data
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