GEOLOGl' OF THE POUGHKEEPSIE QUADRANGLE 79 



iaalf mile to the northeast the dip is gently away from the gneiss 

 and the strike cuts across it at a small angle. This general relation 

 holds to the Oielsea rtiad. 



The topography southeast of Fishkill Village is very flat. There 

 are few outcrops north of the Fishkill-Glenham road, between it 

 and the woods, until the farm of Albert Haight is reached and none 

 to the south of it until Glenham is reached. Low ledges of lime- 

 stone appear north of Fishkill Village. Between the Chelsea and 

 Wappinger Falls roads and north of that road and the Cold Spring 

 turnpike they are abundant. 



Just north of the village on the west side of the road, to the 

 south of the cemetery, the strike is n. 55° e. and the dip 35° s.e. 

 (lettered B in section figure 23). Farther north on the roadside 

 near the gneiss the strike is n. 15° e. and the dip 49° n.w. (lettered 

 A). At the railroad crossing on the Cold Spring road the strike is 

 n. 80° e. and the dip 46° n.w. (lettered C). Southeast of Fishkill 

 creek and northeast of the Cold Spring road, from a point a short 

 distance from the road as far as Milton Hustis's farm, the strike 

 varies from 25" to 40° east of north and the dip is toward the 

 mountain and according to readings taken varies from about 50° to 

 62° s. e. (lettered D). Along the road from Fishkill Village to 

 Brinckerhoff, about one-half mile from Main street in Fishkill 

 Village, the strike and dip are about the Same as at the railroad 

 crossing. Along the northwestern margin of the limestone to the 

 northeast of the Wappinger Falls road the strike and dip are not eas- 

 ily followed. Along a section in a northwest-southeast direction from 

 the Glenham belt through Fishkill Village to the northwestern base 

 of the Honness spur, as shown on the map and the accompanying 





Fig. 23 Section across the Fishkill limestone along a northwest-southeast line through Fishkill 

 VillagsE rom the G'enham gneiss to the Mount Honness spur, to show the character of the folds 

 Distance 2 miles 



section (fif. 23), the limestone is in a series of northwest-south- 

 west folds which have suffered great erosion and, at places, much 

 disturbance. The latter is shown along the highway and in the rail- 

 road cuts southwest of Brinckerhoff, where the strike is only at a 

 small angle to the east of north and at one place n. 50° w. with east- 

 erly dip. Northeast of Brinckerhoff the strike and dip return to the 

 former general direction. In the railroad cut just north of the Johns- 



