A. Wing's Discoveries in Vermont Geology. 



Q, quartzyte. Adjoining the Red Sand rock on tbe w 

 I of the section on page 343, a "dolomitic sandstone.' 



-ection from the Bed Sand-rock west of New Haven to the Quartzyte 

 at Bristol village. 

 In the excursion with Mr. Wing we passed along by the west- 

 era foot of the Hogl,:u-U range, north of the village of Bristol. 

 At one point the limestone stratum was seen to form the lower 

 part of the quartzyte bluff, and to dip beneath rh, .pi.-irt/w.- at 

 i\y. as if actually an underlym- stratum. Mr. \Vi n ^ 

 spoke of this limestone at the time as part of the Primordial or 

 Red Sand-rock series. 



A section of Hogback in the Vermont Geologi 

 taken along a line south of the rei 



between Bristol and Lincoln, makes r 



domical Keport. 



•d by Mr. Wing, 



the west base 



represented in the figure; but tbe Report says (p. 346) : "in the 

 " New Haven Kiver, passing up to 

 limestone occasionally seen, inter- 

 stratified with the quartz"rock, nearly as far as Starksboro village ; 



; of Rutland, I found that the 

 nearest outcrops of the two v 

 t they were conformable. They \ 



j eastward ; but 



> remote to make it -ure 

 nformable according to 



mterstratified with, and replaced by, hy 



