1914—15] Fjelduygningen mellem Sørfjorden og Samnangerf jorden. 247 



XXXIV. Strongly pressed Moberg-conglomerate. Dip 70° E. 



XXXV. Flaser-saussurite-gabbro. 



XXXVI. Conglomerate? The rock reminds onc of XXXIV 

 and XXIX and to a small degree of XXVII. Dip 55° S. E. 



XXXVII. Flaser-saussurite-gabbro. 



XXXVIII. Grev sericite-gneiss at the Trengereid station. 

 Partly eye-gneiss with numerous lenses and veins of quartz. 



Some small sharp folds are seen. Dip 60° E. S.E. 



XXXIX. Flaser-saussurite-gabbro. 

 XL. Quartz-sericite-schist. Dip 80° E. 

 XLI. "Green gneiss", see p. 224. 



X LII. Garnet- bearing gneiss rich in chlorite, with numerous 

 lenses of quartz, probably belonging to the previous zone. 



XLIIIa. White- and black-mottled marble. Dip 68'° E. S.E. 



XLIIIb. Gneissose garnet-bearing phyllites. Dip 80° E. S.E. 



XLIII c. Darker or lighter phyllites which most likely belong 

 to the previous zone. Dip 80° E. 



XLIV. Light chlorite-bearing gneiss. Dip 75° E. 



XLV. Garnet-bearing carbonaceous phyllitc of greyish colour. 

 Dip 75° E. 



XLVI. Strongly pressed Moberg-conglomerate. 



XLVII. "Green gneiss". In some places suggestive of 

 conglomerate-structure. Dip 80° E. N. E. 



XLVIII. Schistose sericite and quartz-bearing serpentine- 

 marble. 



XLIX. Garnet-bearing quartz-sericite-schist. 



L. Impure marble with layers of quartz-sericite-schist. 



LI. Garnet-bearing chloritisized quartz-sericite-schist. 



LII. Marble-quartz-sericite-schist. In the east part the rock 

 contains some serpentine. 



LIII. Garnet-bearing sericite-phyllite. 



LIV. Sericite-bearing marble-quartz-schist. 



LV. Garnet-bearing chlorite-schist rich in quartz. 



LVI. Schistose greyish and white marble. At the foot-path 

 leading up to Rødberg there has been mined in a greyish white- 

 streaked marble, the dip of which is 65° E. and the breadth 

 3—5 m. 



LVII. Polymict conglomerate. 



LVIII. Grey granite ("grev gneiss") with numerous dark 

 fragments and various granitic dykes. 



