

&$$ 



V 



;/ x -t^\- ; "/X^ 



i$ii 





u 





\ s \\"' * M 'C 1 7 N /V '-/ \ ri.\T\ 



i Tria55icsedimen^s and lavas. 

 <\ Paleozoic intrusive granihe-gneisses. 



rjU Paleozoic sediments. 



ill Pre-Paleozoic complex gneisses. 



A-A Depth reached by later cycles of erosion. 



0. Scale in mJJes, horizontal and verhcal. tO. 



STRUCTURE SECTIONS of CENTRAL CONNECTICUT 



