20 
(/t) From 11,000-12,000 feet are sandstones, shales, and chert, 
with plant impressions. Here occurred No. 13 (at about 
11,125 feet), No. 14 (at about 11,560 feet), No. 15 (at 
about 11,925 feet) (llha copter is) . 
(/) From 12,000-13,000 feet there is, at first, a bed of porphyry; 
then, again, sandstones, conglomerates, and shales, with 
plant impressions. In these series were taken Nos. 16, 
1 7, 18, 19 (at 12,350-12,480 feet) and Nos. 20 and 21 
(at about 12,880 feet), with Phacopteris , Knorria , Lcpi- 
doclenclron. 
{m) Between 13,000-14,000 there are sandstones and shales. 
No. 22 is from there, at about 14,000 feet. 
(n) From 14,000-15,000 feet are conglomerates, sandstones, 
with shales; in the latter plant impressions. Nos. 23 
and 24 are from there, at about 14,825 feet. 
{<>) From 15,000-16,000 feet are quartzose rocks, shales, and 
sandstone. 
(p) From 16,000-18,000 feet arc sandstones, conglomerates, 
are quartzose rocks. No. 25 was taken fromt his bed, 
which contains Knorria, Catamites, &c. ; also Comilaria, 
Fenestella, Product us, &c. No. 26 is also from there, 
at about 17,125 feet. 
(q) From 18,000-20,900 feet is a scries of sandstones, con- 
glomerates, porphyry, &c., without fossils. 
(End of section East.) 
(30.) 1874. Smyth (R. Brough) Report of Progress, Geological Survey of Victoria, No. 1. 
Pot/. Svo. Melbourne, 1871. (Government Printer). 
At page 24 of this Report. Mr. It. B. Smyth states that lie found, 
in Tasmania, Glossopteris Browniana associated together with Pecopteris 
(. AlctJiopteris ) australis, one of the characteristic forms of the Jurassic coal- 
beds of Australia. 
(31.) 1876. Smyth (It. Brough) Geological Sketch-map of Australia. 2nd Edition. De- 
partment of Mines. Melbourne, 187G. 
(32.) 1876. Smyth (R. Brough) Report of Progress, Geological Survey of Victoria, No. 
III. Poy. 8 vo. Melbourne, 1S7G. ( Government Printer.) 
In this Report there are, with the discussion of the Geological Sketch- 
map of Australia, given also various remarks of general interest on the 
Mesozoic (so called) coal strata. 
