Fio\ 2. 



EXPLANATION 



im 





'iiA 



ANDALUSITE SCHISTS ~\ Q 5 

 FELSPA THIC QUAHTZITES \ $ S 



' LIMESTONES 

 BIO Ti TESNEISSES, 

 SCHISTS & GRANULITES 

 /[with SUBORDINATE 



RORNBLENOE- 

 A SCH/STS 



I NO RITE OF 

 THE K Eft N ELS 





s s S 7 



W/7W XENOLITHS "1 



8 



MAINLY OF 



FY VIE SEH/ES 







3 



WITH XENOLITHS 



MAINLY OF 



ELLON SEHIES j 



£ NO ATTEMPT IS MADE TO IN 01 C ATE 

 BY DEPTH OF ORNAM£NT THE 

 GRADUAL PASSAGE FROM HIGHLAND 

 SCHISTS TO CONTAMINATED ROCKS £ 

 FROM THESE TO NOR/TE OF THE KERNELS 





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if 



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THE 



ARNAGE MASS 

 ABERDEENSHIRE 



H.H.READ 



Scale 



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i i i i i 



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 i/p of Fo/iation. 



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/. 



Crazg7vaZl 



V/W,/7777,mi 



Hill of Dudwick 



SUGGESTED SECT ION ACROSS THE ARNAGE MASS. 



