249 
Part 3.] Foote: Re^yresentalives of the Oomlwana Series^ 
21. Gritty sandstones, and shales, grey, alternating. 
20. Ditto, buff and drab, false bedded. 
19. Ditto, grey and whitish grey, flaggy. 
18. Shales, gritty, grey, drab. 
17. Gritty sandstones, coarse, ferruginous. 
16. Ditto, buff, false bedded. 
15. Ditto, grey, drab. 
14. Shales, sandy, drab. 
13. Ditto, white, grey, huffy. 
12. Gritty sandstones, brown, flaggy, with a few pebbles. 
11. Ditto, false bedded. 
10. Conglomerates and sandstone (local), with red clay in galls and lenticular 
patches. 
9. Pebble and boulder bed (local). 
8. Sandstone, gritty, buff, brown. 
7. Ditto, ferruginous. 
Small fault. 
6. Grit, shaley, drab. 
5. Conglomerate, gritty, ferruginous, enclosing gneiss pebbles. 
4. Grit, fine light-colored, enclosing boulders. 
3. Ditto, coarse, fcn-uginous. 
2. Ditto, fine bedded, shaley, brown, buff, pinkish. 
1. Boulder bed. 
Gneiss, 
The direction of this section is, roughly speaking, from west-south-weat'to east- 
north-east, and the length about one-third of a mile. The dip is easterly, but shifts 
several points northward and southward with the rolling of the beds. The 
average dip is from 12® to 15,® but varies a good deal in parts. The plant 
remains were mostly obtained from beds Nos. 13 and 14, but a few also from a 
thin bed of clayey red sandstone, a little distance south of the section locally 
underlying No. 11. 
The fossils obtained at the Terany end of this patch of i^lant beds were found 
in the materials excavated in sinking two new hoturies in the paddy flat im¬ 
mediately east of the villages. As the beds are nearly horizontal, their base is 
obscured by the water in the wells; but they are probably low down in the series, 
as they lie close to the gneiss boundary. 
The fossiliferous rock is a fine shaley micaceous sandstone of deep buff coloui’, 
and unfortunately rather friable, so that the impressions of the plants are very 
easily effaced. They will be enumerated further on. 
III.— The (Katjeat) Kaei Patch, 
A good section of the western end of this patch is formed by a nullah which 
-drains into the tank north-east of Terany. 
Section No. 4. 
16. Grit, purple (overlaps on to the gneiss). 
15. Shales, drab and buff and grey, mottled. 
14, Ditto, s.andy, buff, with large concretions. 
