248 Carl Fred. Kolderup. [Nr. 8 



LIX. Polymict conglomerate strongly pressed and ricli in mica. 

 Dip 85° E.N.E. 



LX. Grey granite of the same kind as LVIII. 



LXI. Felspar-bearing hornblende-sehist, Dip 75° W.S.W. 



LXII. Green-schist with parts of phyllite. Dip 40° W.S.W. 



LXIII. Grey gneiss rich in biotite, very likely belonging to 

 the green-schist just mentioned. 



LXIY. Phyllite with lenses of quartz. 



LXV. Schistose garnet-bearing amphibolite. Dip 80° W.N.W. 



LXVL Calcite-bearing quartz-phyllite. 



LXVII. Fine-grained granite rich in plagioelase with some 

 light-coloured mica. Dip 80° W.N.W. 



LXVIII. Soap-stone. Ancient quarry above the railroad. 



LXIX. Phyllite with veins of quartz and some dykes of 

 granite. Strike N— S, dip about 90°. 



LXX Schistose basic hornblende-syenite. Strike N— S, dip 

 about 90°. 



LXXI. Phyllite rich in biotite with lenses of quartz. At 

 several places gneissose layers rich in garnet occur. In the east 

 half of tliis extensive zone the rock is more folcled than further 

 westwards, and the strike is also different. In the west the strike 

 is N— S., in the east N N W.— S.S.E. 



LXXII. Serpentine of somewhat varying composition. 



LXXIII. Fine-folded phyllite in part rich in quartz. 



LXXIV. Felspar-bearing hornblende-sehist. 



LXXV. Phyllite. Dip 50° W.S.W. 



LXXVI. Felspar-bearing saussuritisized hornblende-sehist. 

 Dip 50° S.S.W. 



LX XVII. Fine-grained gneiss strongly split and of a dark 

 greyish colour. Dip 60° S.W. It is cut by some dykes which 

 must be designated as saussurite-diabases. 



LXXVIII. Dark grey-coloured eye-gneiss partly rich in mica. 

 The rock is intersected in every direction by numerous cracks. Dip 

 about 50° W.S.W. 



LXXIX. Crushed chloritic gneiss with numerous small veins 

 of calcite. 



LXXX. Light-coloured phyllite with thin layers of quartz. 

 Dip 45° W.S.W. 



LXXXI. Fine-grained mottled marble of grey and white 

 colour. Dip 05° S.W. 



