io6 



STRATIGRAPHICAL GEOLOGY. 



Location — Bet 111 die at . 

 Top of Peaked hill, 

 East side of West Peaked hill, 

 Top of the same, . 

 Near C. C. Clarke's, 

 West of Baptist church, on hillside 

 Top of same hill, . 

 East of T. Twombly's, . 

 E. B. Phillips's, west corner of tow 

 C. Pe trie's, .... 

 P. G. Russel's, north line, 

 Franconia road, west part of tow 



Littleton. 

 East side of Eustis hill, 

 Near Scythe Factory Village, 

 S. M. near Lisbon line, 



Whitefield. 

 North of M. Bowles's, . 

 East of G. W. Rowland's, 

 Westof J. W. Walker's, 

 Kimball hill, top and south side, 

 East of J. Lindsey's, 

 Town-farm to N. E. Hutchins's, 



Franconia. 

 G. W. Smith's, north corner, 

 R. Wallace's, 

 W. Wallace's, 

 J. McDonald's, 



Carroll. 

 Hill north of Twin Mountain house, 



Dip. 



75° N. 32° W. 

 75° N. 62° W. 

 67° N. 42° W. 

 80° N. 32° W. 

 75° N. 10" W\ 

 80° N. 20° W. 

 70° N. 27° W. 

 55° N. it W. 

 80° N. 40° W. 

 80° N. 48° E. 

 70° N. 27° W. 



75° north-westerly. 



Vertical, strike N. 58° E. 



. Northerly about 30°. 



75° N. 62° W. 



20° West. 



West. 



65° N. 67° W. 



55° N. 8° E. 

 20° easterly. 



80° N. 27° W. 



5o°-6o° S. 10° W. 



Strike N. 53° E. 



. 80° N. it W. 



60° south. 



An inspection of these positions shows a general inclination to the 

 west of north. In the north corner of Franconia there is a local anti- 

 clinal. At the Twin Mountain house the rock dips southerly ; and there 

 is a distinct antichnal in Whitefield. The best interpretation of the 

 structure seems to be that of an inverted synclinal in Bethlehem (see 

 PL VI, Fig. 7), and an anticlinal in the spur extending northerly. The 

 north-east part of Bethlehem and large parts of Carroll and Whitefield 

 are so much covered by drift that we cannot make out the structure of 

 this formation in a very important locality. It is easier to regard the 

 porphyritic gneiss of Franconia and the Wing Road region as connected 



