110 
River Murray into the mallee lands of N.W. Victoria. The 
‘quality of the water has not altogether been unsuspected, and it 
is clear from the position of Mulgundawa that the water is im- 
oun and in consequence has acquired an accession of 
mineral ingredients ; ; but it is not improbable that, in course of 
‘time, some sensible diminution in the percentage value of its 
salts will result. 
BoRE-SECTION AT MULGUNDAWA. 
3. 40. Fine yellow sand, with fragments of oyster; pectens and 
spines of Ci idaris. 
43. Greyish- a fine-grained calciferous Me with calciferous 
stone pellets. Jsis sp. a olyzoa. 
:60-69. Similar W 43. Terebratulina alttiina. Isis sp. 
Scutellina patella, Fibularia Lon Polyzoa 
75. Sameas 43. Shell ee very r 
.84-93. Same as 60-69. Fossil-debris rare. Scutellina patella 
= other dee: Graphularia, Dimya 
ssimilis. 
“97-98. Grey, ee caleiferous sand, and slightly argillace- 
us. 
100-107. Same as 60-69. Terebratulina catinuliformis. 
160-164. Greenish-grey, very fine- Re caleiferous sand. 
erebratulina catinuliform 
175. Yellowish-grey, calciferous, are 
180-186. Bluish- grey, clayey sand, very fine, and slightly eal- 
No fossils. 
188-200. Grey kloifoiðui sand and sandrock. No fossils. 
202-206. Mottled grey-brown sandy clay. Chief source of the 
fossils, 
207-208. Very stiff brown-black clay. 
209. Brown clayey sand. 
216-226. (From seven hien D Very stiff brown-black clay. 
230-232. Brown clayey sa 
238. Light brown v m 
246-250. Stiff black clay. 
‘254-260. Black and rey clays. 
264. Brown clayey s 
.265. Brown sharp ibd, with much comminuted shell-debris ; 
E eoe corroded and eroded ; small splinters of 
wood, freely diffi used. 
285. Grey ee ee sand, with wre 
292. Greyish-white sand, very fine-grained ; the coarser pene 
of translucent sub-angular ees z grains up 
5 mm. diameter; fossiliferous, and splinters ot 
carbonised wood 
