•-51-1 



tu 



w 



ft 



o 



p 



1 fH • 





to 



-O • CIS ^^ 



X 



•H 



(U 4-> O CQ 



+-> 



O 



CQ O 1 to ■— ' 



<u 



■H 



, -1 <U 1 



•H 



to 



Mh G, e ctJ 4-) O 



o 



X 



O -H Oh 



o 



x: 



<U -P h .-H P< 



CO 



ft 



(DO Oft 





o 



T3 C 0) > f-H 



• •» 



<u 



3 cd X O OJ < 



^^\ 



u 



4-> 4J +J O 



o 





•H (0 +-> C CM 



•-I -H c o c3 ->«. 



vO 



c 



cn 



o 



ft Q -H i-H +J ^ 



>— 1 



•H 



§1 ft to 



'— ' 



■p 



< tU -O -H 4J 





c« 



S 0) (u 13 nJ 



> 



u 



<U -H to O IX 



tu 



o 



X H 3 C 0) +J 



Q 



1— 1 



+-> CIS S 



t-H 



ft 



<U T3 +-> -H <U 



§ 





tp X C (0 +J 4J 

 O 4-> 3 -H Ctf 



13 nS o 



s 





to S X 1 -H 



o 





C O +-» O 13 • 



u 





O fn -H S 4-> C M-l 



tw 





Meidev (1960) Suggested the Determinati 

 rock Topography (AZ) by the Use of AT F 

 AT is treated as a time- intercept quant 

 intercept formula. Sketch shows the ti 

 (A) and the relationship of a pinnacle 

 Empirical results for this study area i 

 vides better estimates of bedrock relie 



24 



