246 Carl Fred. Kolderup. [Nr. a 



XVII. Various schistose chloritic rocks. 

 XVIII- Grey and white marble. Some distance above the 

 railroad a small remainder of coral has been found. Dip 80° E. S. E. 



XIX. Strongly pressed Moberg-conglomerate with pebbles 

 of marble of the same type as XVIII. 



XX. A zone, 8 m. broad, the 7 westernmost metres of which 

 are constituted of quartz-sericite-schist, intersected by wavy chloritic 

 divisional planes, and alternating with thin layers of chloritic schists. 

 The easternmost portion, 1 m. of breadth, is likely to be regarded 

 as a strongly pressed conglomerate. 



XXI. A marble-zone 5 m. of breadth, which widens con- 

 siderably upwards in the mountain. In the west the marble is 

 grey, in the east variegated (white, red and grey). Dip 75° E. S.E. 



XXII. Gneiss, which is very much stretched, partly with 

 eyes of felspar, veins and lenses of pegmatite with red felspar, 

 as in V. The dip of the stretching structure is 25° S. S. W. Dip 

 of the rock is 80° E. S. E. 



XXIII. A schistose grey gneiss with chlorite and hornblende 

 on the cleavage planes. This gneiss is more fine-grained than 

 XXII from which it is separated by a thrust-plane. It contains 

 much calcite and effervesces with H Cl. 



XXIV. Variegated marble (red, green, grey and white). 

 Dip 90°. 



XXV. Strongly pressed Moberg-conglomerate, intersected by 

 numerous fissures. See fig. 19. 



XXVI. Schist:se marble rich in sericite. Dip 60° W. 



XXVII. Strongly pressed conglomerate with chloritic ce- 

 menting matrix. Dip 75° W. 



XXVIII. Very schistose and fine-grained grey marble. 



XXIX. Pressed conglomerate ? 



XXX. Flaser-saussurite-gabbro. Lenses and stripes of lighter- 

 coloured rocks in darker-coloured ones. 7 of the collected rocks 

 must be designated as hornblende-schists, with a greater or smaller 

 amount of felspar or zoisite. The others can be characterized as 

 amphibolites ore more or less saussuritisized uralite-gabbros. 



XXXI. Light grey gneiss, in which lenses of white quartz 

 occur. 



XXXII. Dark grey marble. The breadth of the zone is 

 about 10 m. at the sea, at the railroad 7 m. 



XXXIII. Various rocks rich in chlorite. 



