[vOL. XIII. 
180 
2md seam 
1st seam 
Records of the Geological Siirvey of India. 
Brought forward 
. 138' 
3" 
Dark sandstone ...... 
. 4' 
11" 
Sandstone. 
. 11' 
10" 
Stony coal. 
. 2' 
3" 
Sandstone ...... 
. 10' 
9' 
Stony coal .... . . 
6" 
Sandstone. 
. ir 
1" 
Shale (fossiliferous) .... 
10" 
'Coal . 
. 1' 
10" 
Carbonaceous shale ..... 
2" 
Coal . . . 
. 1' 
1" 
Burnt Coal . 
. 4' 
Trap. 
1" 
Charred Coal . 
. 1' 
1" 
Sandstone. 
11" 
Carbonaceous shale ..... 
. 2' 
7" 
Sandstone. 
10" 
Shale ....... 
4" 
Bottom seam, stony and burnt 
. 3' 
(Seam not cut through) 
Total . . . 202' 4" 
The fossils at this locality were more various, and are preserved partly in a 
dark fine, grained shale, and partly in a more sandy rock. They are— 
Schizoneura ? (probably ? gondwanensis) —two specimens, rather badly preserved, but 
showing apparently an arrangement of leaflets like in Schizoneura, with dissolved 
sheaths. 
JHquisetaceotis stalks. These are very numerous, and all of the same kind, i.e., very 
broadly ribbed, ribs and furrows in juxta-position. They are presumably the stalks 
and stems of the same plant, to which the above-mentioned leaved specimens 
belong, probably Schizoneura. 
Vertehraria indica, Eoyle.—Several specimens of the real Damuda form ; also branched 
specimens. 
Gangamopteris ogclopferoides, Fstm.—The common form, 
Glossoptens communis, Pstm.—Several specimens. 
Olossopteris sp.—A more oval leaf, with comparatively a very long stalk. 
Noggerathiopsis Idslopi, Pstm.—Several specimens, both in the dark shale and in 
the more sandy variety. 
Seeds. —Small, slightly winged, belonging perhaps to Noggerathiopsis. 
Taking now these fossils and those from No. 24 into close consideration, wo 
find that although the second seam is separated from the bottom seam by a 
coTn]iaratively thin band only, yet the flora has a slightly different character. 
1 ertebraria becomes more numerous, and Olossopteris, although representing only 
