STEIKE AND DIP. 



429 



Wallingfonl, southwest part, 

 Clarendon, north part, 

 Clarendon, north part, 

 Clarendon, southwest part, 

 Clarendon, west part, 

 Clarendon, west part, 



Clarendon, west of Colviu's marble quarry, 

 Clarendon, west line, 

 Clarendon, north line, 

 Ira, north part, 

 Ira, north part, 

 Ira, Bird Mountain, 

 Ira, south of Bird Mountain, 

 Ira, east of Bird Mountain, 

 Ira, east part, 

 Ira, east part, 

 Ira, southerly part, 

 Ira, southerly part, 

 Ira, west part, 

 Ira, Herrick Mountain, 

 Ira, east base of Herrick Mountain, 

 Ira, southwest part, 

 Ira, west part of the gorge, 

 Ira, east part of the gorge, 

 Castleton, east of center, 

 Castleton, southeast part, 

 Castleton, southeast part, 

 - Fairhaven, west part, 

 Fairhaven, west part, 

 Rutland, southwest corner, 

 Rutland, southwest part, 

 Rutland, west part, 

 Rutland, west part, 

 West Rutland, east range of schist, 

 West Rutland, east of the quarries, 

 Rutland, northwest part, 

 West Rutland, east of quarries, 

 Pittsford, southwest part, 

 Pittsford, southwest part, 

 Pittsford, southwest part, 

 Pittsford, west part, 

 Pittsford, west part, 

 Pittsford, east of do., 

 Pittsford, northwest part, 



Two features of the stratigrapliical position of the talcoid schists are presented by this table. First, the 

 great body of the formation dips to the east. All of the formation south of Mount Anthony, and all 

 that lies west of a line running from the west base of Mount Eolus, the west base of Equinox Mountain, 

 to the foot of Mount Anthony, also dips eastwardly. The small ranges in Rutland County, as well as the 

 spur in West Rutland, also dip eastwardly. 



Secondly, the talcoid schists resting upon the thick Eolian limestones of Mount Eolus, Equinox Moun- 

 tain, Bald Peak, Spruce Peak, Mount Anthony, and all the range connecting these summits, have a 

 westerly dip. Supposing that these rocks exhibit their original relations to one another, we should have 



