502 PROCEEDINGS OP THE GEOLOGICAL SOCIETY. [Jan. 19, 



Pennyweight Flat, Poverty Point, Grolden Point, White Flat, and Balaclava 

 show the course of the 



Shallow Channel of Ballaarat. 



The Mopoke G-ullies, and the Bakery -hill Lead form the 



Mopoke Mainchannel, which likewise runs into the 



Grravel-pits Mainchannel, which just below the Camp enters on its sub- 

 basaltic course, goes imder Bath's Hotel, and meets the Grolden-point Deep 

 Lead under Dana Street. Here ends the famous Gravel-pits Mainchannel 

 according to law ; for the Grolden-point Lead, having been registered 

 before the Gravel-pits, takes the precedence, and hence it is that after the 

 junction of these two leads the Golden-point Lead retained the name — and 

 so the 



Gravel-pits Mainchannel died a legal death, although not a geological one. The 

 Golden-point Lead is, we may say, a '■'■parvenu'' ; its course is W.S.W. 

 The Inkermann Gullies, A 1 Lead, and the Haphazard Lead form the 



Inkermann Channel, wliich, falling fast in a S.S.W. direction, will soon end its 

 golden career, running into the Golden-point Mainchannel. So also will 

 the Nightingale, Malakoif, and Milkmaid Leads, as also the more important 

 Miners' Right and Mount Pleasant, which two form the 



Redan Channel, and bearing N.W., run into the 



Golden-point Mainchannel. 



The Woolshed Gullies form the Woolshed Channel, the Terrible Gullies 

 form the Terrible Lead, the White Horse Gullies form the White Horse Lead, 

 and the Frenchman's Gullies and the Magpie form the Frenchman's Lead. 

 The last three leads, after their junction, form the 



Sebastopol Mainchannel, bearing W. 



Into this mainchannel, the united channels of the Raglan, Cobler's, and 

 Long Gully will eventually run. 



The Black-lead Gullies, Hiscock's Gullies, Poor-man's Gully, and Sussex 

 form respectively the Black Lead, Hiscock's Lead, Nelson's, and the Sussex 

 Lead, which, joining together, form the 



Black-lead Mainchannel, bearing W. 

 The Chalk-hiUs, the 



Shallow channel of Buninyong, is only to be found in unconnected portions. 

 Its course, however, is likely to be detected in a westerly direction. 

 The Union Jack, Scotchman's, Devonshire, Welshman's, Rider's, and Dur- 

 ham Leads will all join the 



Greenhill Mainchannel, the course of which bears southward. 



References to the Numbers and Letters on the Map. PL XY. 



20. Bakery-hill Channel. 



21. Blackhill Quartz -lodes and -A^eiiis. 



22. Manpoke Channel. 



23. Junction where the Welcome nug- 

 get was found. 



24. The lower end of Mopoke Lead. 



25. Gravel-pits Mainchannel. 



26. Junction of the last and the Golden 

 Point deep Channel. 



27. Inkermann Channel. 



28. A 1 Channel. 



29. Haphazard Channel. 



30. Township Quartz-reef: strike N. 

 11° W.! 



31. Great Western Bore ,i r. 

 the com'se oi 



1 Auriferous Gullies "[Springs Dig- 



2. „ Channel J gings. 



3. Dead-horse Channel. 



4. „ Quartz-reef. 



5. Nuggety Gully. 



6. Little Bendigo, 



7. Kangaroo Gully. 



8. Monte Christo Quartz-reef. 



9. BrownhiU GuUy. 

 10. Rotten Gully. 

 XL Hit or Miss GuUy. 



12. Cockatoo Gully. 



13. The Eureka Channel. 



14. BrownhiU Channel. 



15. Caledonian Channel. 



16. Long-looked-for Channel. 



17. Lady Berkeley Channel. 



18. Nil-desperandxmi Chaimel (where 



the N.-desp. nugget was found). 



19. Blackhill Channel. 



32. Band of Hope Bore \- Golden- 



oo TT- i • Tj point Main- 



33. Victoria Bore . . • j §iannel(26). 



34. Pennyweight Flat. 



