884 
TasLe VII.—Analyses of foreign coals, 
AUSTRALIAN, 
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SISSIES LEE 8 Feel ata al! me e 
1 | 225 | 2.47 |82.15 (58.20 | 7.17 |_---.-------- 05 2210.66 10/245 eee to ak 7,330 | 35.6 | 1.810 
2| 1082 | 2.0 |82.6 |56.6 | 8,8 | White --__- 150°, |. cp | ae 7,559 17,255 | 36.6 | 1.737 
ate 09 eet Ee IN OG ek oo ee ise I 6, 687 |6,895 | 87, | 1.704 
4 | 3118 | 2.81 [88.05 [62.92 |11.22 | Gray______- (Dp) fe Sea PER pe on __----|6, 865 | 38.2 | 1,604 
5 | 1209 | 2.77 |36.11 52.66 | 8,46 |-__-- 0 cc gee es 6,910 | 40.6 | 1.460 
6 | 4216 | 2.49 36,53 53.02 | 7.96 Yellowish ene Gives 6,975 | 40.8 | 1.450 
brown. 
7 | 1209 | 2.94 /36.57 [51.87 | 9.12 | Reddish ___| 0.88 |_.-__|----- 6,770 | 41.6 | 1.421 
8 | 8265 | 2.74 |38.68 |58.65 | 4.98 | Brown_-_--|------ OM aA 7,100 | 41.9 | 1.390 
JAPANESE 
SeiRakia aetna 0.14 |1.07 |0, 42 7,970 | 27.6 | 2.630 
BeoGies 221264 ds See 7,140 | 39.4 | 1.538 
See 0.21 {0.82 [0.88 |__.._|------'6, 880 | 42.2 | 1.375 
agi Se ete 0724 |e. 7,015 | 42.8 | 1.335 
Reddish ___| 0.69 |----- Cities sit: _-----|6, 660 | 42.8 | 1.885 
Brown. ____| 0.56 |0.03 |0.45 6,880 | 43.1 | 1,323 
Se HH SP ELD 0.88 |.----!_-..-| 1.70 6,820 | 43,3 | 1.813 
ae SLE (rig (i eaten 6,530 | 43.3 | 1.309 
Gray.c..- < 0. 28 |0.02 |0, 21 6,710 | 43.7 | 1.290 
TR SEE RS Rat TD HAE AS (tees 6,855 | 43.7 | 1.288 
Grarisaks OTe {wakes ees -<--~- |------|6, 660 | 43.8 | 1, 286 
tate (hae 6,853 | 44.0 | 1.276 
iciirnes caren. ee Reema ede 6,875 | 44,7 | 1,241 
Red dish:| 0,40: fisc wl uac| ee 6,513 | 44.7 | 1.239 
gray. : s 
Gray..----- BRS es oie sami 6,274 | 44.8 | 1.280 
Toke Bit een eels 6,436 | 45.1 | 1.221 
brown 
Scders Ree 2.90 |_..--|..---|------|6, 652 |6, 165 | 45.3 | 1.206 
eer a SE 0,96] o25ef anton se 16; 800 | 45.6 12.188 
Tid eh tee Reale 6,350 46.3 | 1.160 
brown x 
erent eee s Forsint Peas See 5,565 | 50.4 | 0.983 
CARY Ye eee PAR ae Wt FD ge as 5,245 | 52.8 | 0.892 
« INDIAN. 
be 3546 2.04 5.16 ‘2.00 10.80 | Light gray-| 0,62 }-----]_----|.-----|_..... 6,795 | 40.3 | 1.480 
The upper beds of Philippine coal which have thus far been discovered, 
and which outcrop at certain places, should for the greater part be classed 
under the name sub-bituminous, which has recently been adopted by the 
