94 Carl Fred. Kolderup. 



List of figures in text. 



Fig. 1. The Dalsfjord seen from Skaareijeld page 13 



„ 2. Microphoto of crushed basement conglomerate at the east 



end of Bergevand (7 X) — 16 



„ 3. Section at the lower boundary of the basement conglo- 

 merate in the south east wall of Kvamshesten. a. greyish 

 green schists, b. black schists, c. hard greenish schists 

 and d. conglomerate — 17 



„ 4. The thrust plane below the eastern part of the southern 

 precipice of Kvamshesten. The overhanging conglomerate 

 is obviously very jointed — 18 



„ 5. Kvamshesten seen from the east. The shadow falls sharp 



along the thrust plane — 19 



„ 6. Basement conglomerate above the farm Øvre Fossedal ... — 22 



„ 7. Conglomerate in the western part of the highest top of 



Hængenipen — 23 



„ 8. Geological section between Markevand and Grundevand. 



Conglomerates alternating with sandstones — 24 



„ 9. Breccia from the lower boundary of the Devonian area in 

 the gap west of Keiservand. The underlying rocks in this 

 districts are: quartzites (with quartzschists) and phyllites. 

 The fragments of the breccia consist of the same sort of 

 rocks. 72 nat. size — 26 



„ 10. Microphoto of basement conglomerate above the farm Øvre 

 Fossedal. The light fragments consist of various syenites 

 and granites and of felspars and quartz, the dark fragments 

 of rocks rich in hornblende — 28 



„ 11. Microphoto of conglomerate about 500 m. above sea level 

 on the north side of Kringlen. The fragments consist 

 mostly of syenite rich in microperthite, fine-grained granite, 

 pyroxenite, felspar and light hornblende that is partly 

 altered into chlorite, (about 9 X) — 29 



„ 12. Block of bottom conglomerate with numerous angular 

 fragments (breccia) above the farm Øvre Fossedal. The 

 irregular arrangement of the fragments can be seen di- 

 stinctly. V3 nat. size — 30 



„ 13. The same block as that on fig. 12 seen from another side — 31 



