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Sunday 28 July 2013

SCRUBBY GULLY, TORRINGTON NSW


Scrubby Gully is located on the western side of The Torrington Pendant, where the Mole Granite intrudes the overlying sedimentary rocks. In many places the boundary is notable for the presence of silexite, essentially a topaz-quartz rock. See especially my earlier blog entry “Torrington – Essential Reading” as well as the various references mentioned in the blogs on downloading from DIGS and the ALF site.Scrubby Gully may be reached by following the Butler Mine road and then the Mystery Face road, which branch to the left several kilometres north of Torrington from the Silent Grove road. At the Mystery Face car park, the fence directly ahead marks the boundary between the Conservation Area and private property. Follow the fence to the left for 15-20 minutes until it descends into Scrubby Gully. The alluvial areas are marked by hatching on the adjoining map. (The Scrubby Gully Mine shown is a bismuth/tungsten/lead deposit.)

To the right (upstream) are the Scrubby Gully alluvial workings, dating from the 1870’s and 80’s. Large quantities of “tin” (cassiterite) were extracted from here and from the gully below (downstream of the boundary fence). From the 1960’s until now fossickers have visited this area in search of topaz, especially the sky blue variety, for which the locality is well known.

For details of the geology of the diggings, see TWE David’s 1887 memoir on the Vegetable Creek Tin Mining Field (pages 71 and 164 especially. This can be downloaded from DIGS. The Minerama books on Topaz and Beryl also contain useful information.

The topaz comes in two forms – very waterworn (like the tin) and scarcely worn at all, reflecting the two likely sources - the ancient alluvial deposits and vughs in the silexite and adjacent granite. Only a very small proportion is the desirable sky blue variety. Along with the topaz is black tourmaline (schorl) and the occasional sapphire and zircon (both very worn). Pale green beryl is also found as unabraided crystals, no doubt also derived from the same vughs and veins as the topaz crystals and the tourmaline.

Any place where sediment is accumulating in holes and cracks is worth investigating for these gems. Remember that beryl is not a dense mineral and does not concentrate in the sieve centres as the other minerals mentioned do.

Typical topaz producing crack

A good trap








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The writer digging for topaz at Scrubby Gully 1998
A few good finds
Some choice Scrubby Gully topaz

Beryl crystal from Scrubby Gully

Wednesday 24 July 2013

THE GLORY HOLE YARROW CREEK NEAR GLEN INNES NSW

LIST OF ALL BLOG ENTRIES TO DATE

The original Glory Hole January 2003
This spot always proved popular with those who came on our Baptist Church Fossicking Group trips and during Minerama (the annual Glen Innes gem and mineral show). 

Although I had visited this part of the creek several times before 2003 and had even taken groups there, nearly everyone was not at all keen about venturing into the waterholes which characterise the place. In January 2003 the water level was about as low as it ever gets because of a dry summer and so, with our newly formed fossicking group, we decided to give it a go.
 
A series of joints in the granite has produced some ideal traps for gemstones. The largest of these is blocked with large rocks at one end (all submerged) and full of sand at the other. The problem with the sand is that there isn’t any place to put it when you dig it out where it won’t wash back in again next time the creek floods. The best I could do was to throw it up into the shallow end and hope to reach the bottom at 
The first good find January 2003
the deep end.

This worked out fine, as it turned out, because I was able to get in under the rocks and extract some rich gravel. We took no photos of the finds, unfortunately (predigital camera time for us). All the gem photos are of stones found in other cracks nearby on later visits.

There were cutters in every sieve – sapphire, zircon, garnet, black spinel and quartz – and it’s no wonder we called it the Glory Hole. 

The name is now used for all that section of the creek. This was the first bonanza we had found in Yarrow Creek and one of the biggest. The gems were embedded in white clay and I have no doubt that there are still good finds to be made in the original location. Just get rid of the sand!
January 2003

Working on a productive crack January 2013

All the other cracks located here have also produced quality gems and I’m convinced that there are both new cracks and extensions of the original ones yet to be explored.

Good wash January 2013










See my video on gem hunting at the Glory Hole here .

My other fossicking videos from around Glen Innes are to be found here along with others dealing with mining and general geology.
I also have playlists on Glen Innes, the Blue Mountains and New Zealand.
All New England and other Geology blogs and videos
A good pyrope garnet January 2013
Zircons and garnets March 2009
Sapphires March 2009

Monday 22 July 2013

DOWNLOADING REPORTS FROM THE AUSTRALIAN MUSEUM, SYDNEY NSW

The Australian Museum in College St, Sydney NSW, is one of Australia’s most prestigious scientific institutions.
To quote the Museum’s website (here) We have published the results of scientific work on the Australian natural and cultural environment for more than 150 years. The Australian Museum houses some of the world's most important collections of Australian animal, fossil and geological specimens and cultural artefacts. Research on these millions of objects yields insights into how our world changes through time and how its diversity can be classified and interpreted.”

The Museum’s collections had a considerable influence on me in my High School days, especially the mineral displays, and I have drooled over them many times since. However, it is their printed reports which concern us here. While their geological and mineralogical content is nowhere near as extensive as those to be found in DIGS, nevertheless to use an old expression, they are “a mine of information”.

 To access an important part of this resource, go to this site: By selecting appropriate keywords, I was able to come up with these interesting articles. You should do the same, as well as exploring what other resources the Museum has to offer online.






Brian England: “Ben Lomond Zeolites” 










Sutherland et al “The Tumbarumba Basaltic Gem Field” 









Hollis, J. D.; Sutherland, F. L., 1985. “Occurrences and origins of gem zircons in eastern Australia” 





If you locate other useful records, please add them to this entry as a comment and I will transfer them to the main text if appropriate.

Why not check out my You Tube channel here where you can view gem hunting, mining and general geology videos. I also have Glen Innes, Blue Mountains and New Zealand playlists. New subscribers are always welcome.

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Friday 19 July 2013

KINGSGATE QUARTZ

The Kingsgate mines (near Glen Innes, NSW) have been a major source of bismuth and molybdenum since the 1870’s and recent exploration has revealed that economic amounts of these resources still exist.


Much facettable quartz has been found in the dumps right up to recent years and would be still if access were permitted
Because of mining exploration in recent years, the public has been refused access to the area except under strict supervision on a few rare occasions such as during Minerama, the annual Glen Innes gem and mineral show.

As a result of Kingsgate's long mining history, there are numerous reports available about the area, all of which make reference to the presence of quartz crystals.

Here is a list of easily accessible downloadable references:

Previous references in my Blog:
June 4 2013 DOWNLOADING PDF DOCUMENTS FROM "DIGS",
June 7 2013 The Molybdenum Industry in NSW (Mineral Resources 24, 1916, by EC Andrews) and Molybdenum in NSW (Mineral Resources 43, 1978, by CR Weber, IBL Paterson and DJ Townsend).
July 4 2013 MINERAMA BOOK DOWNLOADS FROM ALF Molybdenite
July 5 2013 MORE USEFUL BOOK DOWNLOADS FROM ALF Kingsgate Mines.

Other references downloadable from DIGS:

Crystal Report 14 (1944) (GS1943/013)

Notes on the Occurrence of Piezoelectric Quartz in Australia with Special Reference to the Kingsgate Field (1944) (GS2009/0915)


 

Why not check out my You Tube channel here where you can view gem hunting,mining and general geology videos. I also have Glen Innes, Blue Mountains and New Zealand playlists. New subscribers are always welcome.

All New England and other Geology blogs and videos


Wednesday 17 July 2013

ENSTATITE FROM YARROW CREEK NEAR GLEN INNES NSW

In my first years of gem hunting in Yarrow Creek I occasionally came up with pieces of a mineral which looked like black spinel but differed in that they showed a green to orange-brown colour when held up to the sun. The best specimens were transparent and gemmy.




As I had done before with specimens of pink sapphire, I sent a few samples to Hylda Bracewell, the highly regarded gemmologist then living in Torrington NSW. Hylda concluded that they were enstatite with some examples approaching hypersthene in their properties.

These minerals are members of the pyroxene family, which are commonly found in basic to ultrabasic igneous rocks and some metamorphic rocks. Their chemical formula can be summarised as (AB)Si0, where A and B are metals. In the family of which enstatite and hypersthene are part, the metals are magnesium (Mg) and iron (Fe). Pure enstatite contains no iron, only magnesium, hypersthene contains both iron and magnesium.

 An important question to be answered is this: where does this mineral come from? Not from the local granites, which appear to contain no pyroxene minerals. Not from the same volcanic source as corundum, zircon and spinel, since it is not found with them in most local creeks. Perhaps from the gabbro dyke which outcrops just upstream from Garnet Corner, some other dyke yet to be identified, or from xenoliths in the granite.

These minerals are not especially hard or dense, but hard and dense enough to end up in the sieve centre along with the sapphire, zircon, garnet and spinel which make up the bulk of the concentrate. Enstatite has a hardness of 5.5 on Mohs’ Scale and a specific gravity of 3.2 – 3.3. They can be cut as gems but need to be protected from undue wear. The colours are not particularly attractive and difficult to see in a set stone.
Despite its shortcoming as a gemstone, a piece of rich green enstatite is a good find and many amateur cutters would like to work on a Yarrow Creek stone if they could find one.

Why not check out my You Tube channel here  where you can view gem hunting, mining and general geology videos. I also have Glen Innes, Blue Mountains and New Zealand playlists. New subscribers are always welcome.

All New England and other Geology blogs and videos
Facetted enstatite 1.5 carats