20 ABKiv FÖR bota:::\Ie:. BA^■D 13. >":o 7. 



Sand, dark grey 0,7 6 m. 



Sand, whitish grey 0,04 » 



Clay, black, in the lower part 



strongly carbonaceous . . . . 0, :-i » 

 Clay and sand, in thin alternating 



strata 0,33 » 



Coal, poorer towards the top . .0,69 » 



Sand, yellowish 0,o8 » 



Clay, intermLxed with sand . .0,05 » 



Clay, greyish 0,3 3 » 



Coal, meagre 0,50 » 



Clay, chiefly dark grey, darker 



towards the top l.oo » 



Coal (dust) 0,40 » 



Sand, greyish, with rust-coloured 

 nodules, containing lumps of 



coal 1 , 1 7 J' 



Clay, greyish, fractured, upwards 

 more sandy and at the top with 

 alternating strata of clay and 

 sand; fragments of plants . . 0,eo t> 



Coal 0,1 6 » 



Clay, blackish, fractured, contain- 

 ing plant-remains 1,7 o » 



Sand, greyish white 1,5 9 » 



Sandstone, very soft, fine-grained, 



greyish white (" below the road) 1,97 » 



/ 12,35 m.-f- 



If this section is compared with the one given by Moberg, 

 the agreement is found to be almost complete, and it may 

 therefore be supposed to be close to the latter. The dip of 

 the strata is mostly 70' towards X.E., but varies between 

 60'' and 85°. 



The clay containing the plant-remains is blackish in 

 colour and much fractured, so that the plants mostly occur 

 as small fragments. Of some of the species, however, fairly 

 good specimens have been obtained. The material has been 

 collected by Prof. Xathor.st, Prof. Moberg, Mr. A. F. Carl- 

 son and Dr. Möller, the larger part by Prof. Moberg. 



