96 Carl Fred. Kolderup. 



vang, lowest in the background the foot of crystalline schists 



that is overlaid by the Devonian rock in steep walls page 48 



Fig. 28. The north side of Helleberget seen from Fængestad. gr.-gr. 

 means the boundary between the Devonian area and the 

 underlying crystalline schists — 49 



„ 29. View of the west side of Bjørndalsvand towards Bleie- 



stauren and Bleien — 51 



„ 30. The syncline in the western part of Lillehesten seen from 



the mountain west of Selsvand — 54 



„ 31. Alternating layers of red conglomerate and red sandstone 

 (the dark stripes) at Grundevand in the western part of 

 Lillehesten — 54 



„ 32. The eastern summit of Lillehesten seen from the south. The 

 lower part forms a foot of crystalline schists, separated from 

 the Devonian area by a thrust plane. The capping is com- 

 posed of crushed crystalline rocks from wich fig. 33, 34 

 and 35 show microphotos — 60 



„ 33. Microphoto of a breccia 100 m. east north east of the cairn 



on Lillehesten — 62 



„ 34. Microphoto of the breccia 30 m. east of the cairn on Lille- 

 hesten — 63 



„ 35. Microphoto of the breccia 30 m. east of the lake between 



the two summits of Lillehesten — 64 



„ 36. Microphoto of green sandstone from the cairn on Bleien. 

 The light minerals are microperthite, plagioclase and 

 quartz, the dark chlorite, epidote and iron ore — 68 



„ 37. The lower boundary of the Devonian area of Kvamshesten 



Along the north side, Along the south side — 75 



„ 38. Geological cross-section through the area of Kvamshesten 

 The rocks are: green shists, quartzshists, basement conglo- 

 merate, red and green sandstones, green sandstones — 77 



„ 39. Geological map of the district between Nordfjord and Sogne- 

 fjord in Western Norway — 84 





