Kvamshestens devonfelt. 95 



Fig. 14. The first red sandstone layers in basement conglomerate 

 about 700 m. above sea level in the mountain south west 

 of Selsvand page 33 



„ 15. The alternating layers of green and red sandstones in the 

 northern part of Kvamshesten seen from the mountain west 

 of Selsvand. The dipping to the north is steepest near the 

 basement conglomerate that can be seen farthest to the right — 34 



» 16. Sketch showing the layers from Mariefjeld (east of Kvan- 

 dalsvand) to Bleien. Taken from the hill south of Kvan- 

 dalsvand. Red and green sandstones overlying basement 

 conglomerate — 35 



„ 17. View from a hill south east of Kvandalsvand towards the 

 south west spur of Bleien (also called Blaafjeld). Under- 

 most we see the basement conglomerate and over this the 

 alternating layers of red and green sandstones — 35 



„ 18. View from the south west end of the lake in Tjønnebotn 

 towards the layers of red and green sandstones between 

 the two narrow gaps at the inner end of the botn. To the 

 right conglomerate — 36 



„ 19. The series of red and green sandstones in the rock wall 

 that goes in north western direction from the gap at the 

 right side on fig. 18 — 37 



„ 20. View from the west side of Krokevand and eastwards. The 

 three mountain tops are: Kringlen to the right with bot- 

 tom conglomerate, Eidsfjeld to the left with red and green 

 sandstones in the lower part and younger conglomerate at 

 the top, and in the background Bleien with the series of 

 green sandstones — 38 



„ 21. The turning of the layers of red and green sandstones north 

 of the north western end of Krokevand, seen from the op- 

 posite side of the lake — 43 



„ 22. View from a height west of the Leknes summer farm to- 

 wards Bleien, whose top is partly covered with mist. A 

 syncline of red and green sandstones. To the left base- 

 ment conglomerate with some layers of sandstone — 43 



„ 23. View from the west side of Bjørndalsvand towards its 

 south eastern corner. Almost vertical layers of red and 

 green sandstones. To the left the right side of the syn- 

 cline on fig. 22 — 44 



„ 24. View from the west side of Bjørndalsvand towards its 



north eastern corner. The left part of the same syncline — 45 



„ 25. Stauren seen from the west. The layers of sandstone are 



turning northwards, to the left on the photo — 46 



„ 26. Sketch map of the region north of Blaavand. Displace- 

 ment of different layers of red and green sandstones — 47 



„ 27. The northern part of the Devonian area seen from the 

 Førdefjord. In the foregrund the peninsula north of Helle- 



