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Sunday, 7 September 2014

WEBB’S SILVER MINE NEAR EMMAVILLE, NSW AUSTRALIA

WEBB’S SILVER MINE NEAR EMMAVILLE 
NSW AUSTRALIA
Please take note: Practically all localities mentioned in these Blogs are on private property, under a mining lease or both. No-one should enter without permission from the landowner or lessee as appropriate.
The mine is marked "Silver" 7 (upper left)
I became aware of the existence of Webb’s Silver Mine (also known as Collison’s (NOT Collisions)) while I was still at school as a result of numerous visits to the late and much lamented Geological and Mining Museum in Sydney. This would have been in the mid 1950’s. The photos and specimens really piqued my interest in geology and mineralogy in particular.
It wasn’t until October 1988 that I made my one and only visit to the site when I rode my pushbike out there. The mine is reached by traveling 9-10 km after leaving The Gulf road, not far out of Emmaville, and then following a track to the right for a further 2.5 km. The mine site is usually described as being on Little Plant Creek, which runs into the Beardy River not far to the north. The map illustrated is the Grafton 1:250000 geological sheet.

My notes made that day mention a steel poppet head over a well-preserved shaft, numerous derelict sheds and ruins, 2X5 head stamper batteries, one in reasonable condition, piles of drill cores and specimens of galena, sphalerite and arsenopyrite on the dumps.
Photo by Wwoofa, Australian Lapidary Forum
Photo  by Wwoofa
Since then, several fossicking trips have be organised to Webb’s during the Emmaville Gemfest. The area is held under lease by Silver Mines Ltd; you can read their summary of the future prospects of the site here (now missing). I quote from this source: “Highest grade undeveloped silver project in Australia”, “a JORC compliant resource of over 12Moz of silver”, “From 1884 to1901 approximately 55,000t were mined at an average grade of at least 23oz/t”, “The current resources at a 70ppm Ag cut-off are approximately 1.49Mt @ 245ppm Ag, 0.27% Cu, 0.71% Pb and 1.56% Zn”.
The silver price is somewhat depressed at the moment (September 2014) which no doubt is quite depressing for the company, which is sitting on a great resource waiting for the right time to begin extracting it profitably.
Taken from Mole Tableland map DIGS R00041396
The classic reference to the geology of the Emmaville and Torrington areas is TWE David’s “Geology of the Vegetable Creek Tin-Mining Field”, 1887. (DIGS reference R00031676, if you wish to download a copy.) The relevant pages are 156/9. David tells us that the vein was discovered by Mr L Webb, that it can be traced for several miles, that the metalliferous part of the vein is nowhere more than 3 feet wide and that the ore minerals present are galena, copper pyrites, mispickel and “a variety of grey copper containing silver and a trace of gold (silver fahlerz)”. We know copper pyrites as chalcopyrite, mispickel as arsenopyrite and fahlerz as “fahlore”, a complex mineral of the tennantite-tetrahedrite family, containing at least 5 metals (iron, copper, zinc, silver and antimony) as well as arsenic and sulfur.

Another reference, written around the time when mining was at its peak, is “The Mineral Resources of NSW” (DIGS reference R00051137) compiled by EF Pittman in 1901. If you want to read what mining was like at that time, start at page 111. The photo of the mine is taken from this source. This is definitely a book that readers of this Blog should download.
From Pittman circa 1901
The comprehensive reference “The Mineral Deposits of NSW (Markham and Basden, 1975, DIGS Reference R00037944) has a lot of information on the mine, commencing on page 379 in the section dealing with the Mole Granite. We learn that the main shaft is 203m deep, with 7 major levels, that 3 separate ore shoots were mined, the main one yielding over 40 000t of ore containing 760-920 g/t of silver as well as significant quantities of the other metals.
The various documents available from the Web which have been uploaded by Silver Mines Ltd will give you a summary of their prospecting and that of their predecessors, which has been quite extensive since mining was active. Here are several:
From DIGS: Review of Environmental Factors (Exploration Activities at Webb’s Silver Mine) 2012 (R00070524). This is a report prepared by Geolink Pty Ltd for Silver Mines Ltd.
Report for Silver Mines Ltd 2010. Here. This is a good summary of the geology and potential of the mineral deposit.

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Thursday, 5 June 2014

JONES’ SWAMP CREEK – GUYRA TO INVERELL ROAD

JONES’ SWAMP CREEK – GUYRA  TO INVERELL ROAD

Over the years we’ve followed up suggestions, leads, hints – whatever you like to call them – about places where sapphires might be found. Jones’ Swamp (Creek or Gully) 3km north of Wandsworth on the Guyra to Inverell road was one of these. We only went once, because it was obvious that we had far better places to fossick than this. Nevertheless, it wasn’t a total failure and it would appear that there are still possibilities there.
The site is one of the original declared fossicking areas of the 1970’s, No. 39 to be exact. The place is on the left as you travel from Guyra and it is (surprise, surprise) basically a swamp. In 2003 that bothered me more than in later years; our experiences at
Rainy Swamp and Pretty Valley proved that sapphires are sometimes found in swamps.
Brett Brown visited the spot and we went out with him the following week. (Brett and Jenny used to run the Cathedral Gallery at White Cliffs).  Brett had found some typical sapphires and zircons, some of reasonable size, so it seemed promising.
As it turned out, the combination of swamp, winter and a shortage of water where it counted somewhat limited our fossicking, but I can confirm that there are gemstones there. We found no cutters, but that
Sue and Evelyn - and a nice fire for the day
doesn’t mean you won’t.
Here are some more pieces of information. According to Wwoofa (Australian Lapidary Forum thread on fossicking localities) the GPS co-ordinates are 6675680N 56356174E. There used to be a photograph there, but it’s been deleted to make more forum space. I don’t think it showed more than the bridge. Turn left at the bridge along a track. This is a broad travelling stock reserve, mostly barren granite country with swampy alluvium along the watercourse.

Two related reports concerning an Authority to Enter issued to Amsil Sapphires Pty Ltd in 1974 can be found in DIGS. The reference numbers are DIGS MR06260 and  MR06259 . Basically, the reports indicate that the creek does have good potential (see the extract) but you need to remember that this report is on another part of the creek. Furthermore, there might have been actual mining on that spot in the years after 1974.
Extract from Amsil Sapphires report
The map portion (from a map issued in 1972 with the Records of the Geological Survey of NSW, 14 part 1 – DIGS reference Records 14(1)), shows that basalt is widespread in the district (normal for sapphire deposits) with the country rock being granodiorite. It also reveals that both Moredun Creek (north) and Georges Creek (south) are sapphire bearing. You could try checking these localities in DIGS. Maps might also reveal other public access places along these three creeks worth investigating.

Sunday, 18 May 2014

THE RED ROCK SAPPHIRE DEPOSIT NEAR WELLINGROVE, NEW ENGLAND DISTRICT NSW AUSTRALIA

THE RED ROCK SAPPHIRE DEPOSIT NEAR WELLINGROVE, NEW ENGLAND DISTRICT NSW AUSTRALIA
This is an unofficial name for a place that lies on a stock route north west of Glen Innes. It is accessed by a gate on the right hand side of the Bonshaw road (also known as Strathbogie and Wellingrove road) about 15km from Glen Innes. It is a km or 2 after the Reddestone Creek bridge, just before the road begins to descend to Back Plain Creek. There may or may not be a sign (reading Red Rock West) on the gate. Once through the gate, the location may be found by taking left hand branch tracks back towards the road. Total distance from the gate would be around 500 metres.
The gate, courtesy of Google Earth
Access is difficult when there is enough water to use for sieving (this is boggy country) and when access is easy the gully will probably be dry. This spot is at the head of a gully draining down to Back Plain Creek at the bottom of the hill. The country rock is basalt, often deeply weathered to a reddish soil loaded with ironstone nodules.

In the soil, scattered among the ironstone nodules, (which are the result of the weathering of the basalt) are small amounts of spinel, sapphire and zircon. How did they get here? This is not a normal alluvial deposit, of the sort we are familiar with in Yarrow Creek. It has some resemblance to 
Wellingrove Fossicking Area - "wash" at the bottom
the so-called “wash” at the Wellingrove Fossicking Area, which is 2-3 km away, as the crow flies. There, the overlying basalt ends at the point where the entry track leaves the sealed road. The underlying rock in the reserve is granite, which intrudes the Emmaville Volcanics on the northern edge. The “wash” may be thought of as a reworked volcanic ash layer, erupted before or along with the neighbouring basalt flow. There has been some concentration of the dense minerals, possibly by rain water at the time of the eruption, but there are few of the normal alluvial indicators such as pebbles of quartz which might have been expected to have been derived from the granite.

At Red Rock there may have been ash layers associated with the basalt, either below or between flows, which could be the source of the gems, or they may be derived from the basalt itself where they formed xenocrysts in the lava. See my blog on Dog’s Tooth Sapphires at Pretty Valley (here) for links to articles which throw some light on this subject.

Extract from the Grafton Metallogenic Map
The extract from the Grafton Metallogenic Map show the geology of the immediate area. The numbers refer to mineral localities. 1835 is the Wellingrove Fossicking Area, 1836 Pablo’s Sapphire Mine, 1837 an alluvial sapphire mine on Back Plain Creek, 1839 the Wellingrove limonite deposit and 1840 Hamel’s Gully, an alluvial deposit, probably on a former course of Reddestone Creek. Tb indicates “Tertiary basalt"). Note also the cross hatching, representing “alluvial” sapphire deposits. I’m only guessing, because I haven’t explored the area, that the prospect at Pablo’s Mine and the areas near it showing cross hatching (south of the Wellingrove Fossicking Area) are similar to Red Rock and that gems will be found near the edge of the basalt in other places in the area. None are likely to be productive enough to mine.
Minerama ran a field trip to Red Rock in 2003. Most people found a few colours but the lack of water was the real issue. I believe some cutters were found, however. Our fossicking group went there several times, with the same result – a few sapphires and zircons and a lot of mud and ironstone, enough to make it interesting even if we found no cutters.

Saturday, 12 April 2014

THE CASCADES, YARROW CREEK NEAR GLEN INNES NSW AUSTRALIA

THE CASCADES, YARROW CREEK 
NEAR GLEN INNES NSW AUSTRALIA
The Crossing is in the centre, the long pool is on the left
This section of Yarrow Creek lies between Garnet Corner and The Crossing (click to go to the Blog List page for information on these locations). In dry weather, it is possible to park in the centre of the area, otherwise walking upstream from the crossing is the best option.
It can be divided into three parts. The uppermost is the cascade area itself. Immediately below Garnet Corner, the stream descends steeply through a drop of about 10 metres to a blockup of large granite boulders. There are numerous small pools and cracks on the way down. Some good gemstones have been extracted here using yabby
The beginning of the pool
pumps. However, a lot of sand has washed down from the Garnet Corner diggings as fossickers have dug and sieved over the years. This may have been washed further downstream by floods since the beginning of 2012.
Boulder blockup and the pool
No doubt there will be good finds made amongst the boulders one day, but it will take a lot of work to shift all but the smallest of them.
The middle section is a long
pool, commencing immediately below the boulders. Within 2 or 3 metres of the rocks, the water will be over your head. Good for swimming (brr) and perhaps ideal for a wetsuit and snorkel equipped fossicker. The 13 carat sapphire in the picture came from the edge of the deeper water. There are some large boulders in the pool immediately after the deepest part and then sand takes over. Some nice cutters have been found among the boulders.
Finds including the 13 carat stone
The final section leads to the rock barrier which crosses the creek another 100 metres or so further downstream. Wash is scarce along here but some good stones have come from the pool just above the barrier and by digging under the left bank (facing downstream).
There is an extensive alluvial flat on this bank which probably conceals former channels of the creek. Naturally, no-one knows where they are and they are probably loaded with gems.
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My finds at Minerama in 2007

Thursday, 6 March 2014

KELLY’S HUT CREEK NEAR GLEN INNES NSW AUSTRALIA

KELLY’S HUT CREEK NEAR 
GLEN INNES NSW AUSTRALIA

Kelly's Hut Creek

It’s surprising how few tributaries Yarrow Creek has upstream of the bridge at Pinkett. A search on Google Earth will allow you to follow the creek upstream from the bridge quite easily. On the left bank (facing upstream) there are a few minor tributaries, of which Rainy Swamp Spring Creek is the most interesting. See the blog on Rainy Swamp for information here. Further up there are Mt Slow Creek and Log Paddock Creek near the Mt Slow road bridge. Upstream from there Frenchies Swamp Creek is practically the only one. (See here for information.) These creeks all carry gemstones.
There are one or two right bank tributaries, but the only sizable one is Kelly’s Hut Creek which rises in the 
distant hills towards Guyra as does Yarrow Creek itself. This creek is crossed on the Mt Slow road about 2km before the Yarrow Creek bridge. There is no signpost, however.
The point where Kelly’s Hut Creek meets the Yarrow is not easy to locate. It is a very rocky place and it so happens that the tributary runs under a lot of boulders and is easily missed. For those who are familiar with Dwyer’s property (for a long time a popular fee-paying fossicking area), you take the tracks leading upstream as far as you can go, park near the dingo fence, go through the big hole in it and walk upstream. Kelly’s Hut Creek is on the right about 400 metres further on.
If you actually do this, you will be trespassing on the neighbouring property. All of Yarrow Creek and Kelly’s Hut Creek past the dingo fence are not on Dwyer’s property. Please note that on the various Minerama and Baptist Church Fossicking Group trips, we did have permission from the landowner but as the access track is not passable when the country is wet such outings were rare. In fact, the last of these would have been in 2004.
For about 2km above the junction there are many rocky areas. The gemstones are identical to those in Yarrow Creek, including pyrope garnets. The creek then turns at right angles and runs parallel to Yarrow Creek, though at a distance of about 2km from it. From this bend on, no more gemstones have been found. Searches of the literature through DIGS were fruitless; in fact the one reference I was able to locate stated categorically that, apart from quartz, at no point were any gemstones located. Nevertheless, the various maps showing the location of sapphire deposits in New England always include Kelly’s Hut Creek, showing the very part that I am claiming is barren to be productive and the part that we know is productive to be barren.

If you ever get a chance to fossick here I know you will enjoy it. You will also be able to verify what I have written about the place. As a guess, I think that the lower part of Kelly’s Hut Creek is probably a former course of the Yarrow, though just how this came about I can’t work out. The presence of garnet in the alluvium (found only in the Yarrow and some of its tributaries) implies that at some point in time a source of garnet must have been somewhere upstream. The geology of the catchment area of Kelly’s Hut Creek today suggests that this is unlikely. If someone unravels this mystery one day I will be glad to correct any errors in what I have written here.


Friday, 31 January 2014

FRENCHIES SWAMP CREEK NEAR GLEN INNES NSW AUSTRALIA

FRENCHIES SWAMP CREEK 
NEAR GLEN INNES NSW AUSTRALIA

The Yarrow Creek junction 2013
Frenchies Swamp Creek is one of only two tributaries of Yarrow Creek over the entire length of the two properties we have regularly fossicked. The other one is a mere trickle and hardly noticeable. Just who Frenchie was I have no idea, but the swamp bearing his name covers a swathe of country between Yarrow Creek and the Mt Slow road near the Henry River bridge.

You might think that swamps are unlikely places to find gemstones, but it has been the swampiest ground at Pretty Valley that has been the most productive, so it doesn’t pay to jump to conclusions. In the case of Frenchies Swamp, the creek flows through some rocky areas along its course and gemstones have been found in all these places. I have followed the main creek up to the limit of the last swamp (about 4km from Yarrow Creek)
3 carat zircon
and gemstones are to be found in the gullies running into the swamp there. There are more small tributaries running into the swamp around its margin but I never had the opportunity to check these out.

The junction with Yarrow Creek is not obvious except when water levels are high. It can be followed up to the first swamp (about 400m) through rocky ground with quite a bit of typical quartz gravel in places. How this got there through kilometres of swamp is one of those little mysteries. The junction is at “Sue’s Favourite Spot”, just below the "Glory Hole" section.
                                                                                 The gemstones are identical to those in Yarrow, with perhaps a lower 
Corundum fragment 1998
garnet percentage. The fact that there is any garnet at all is significant, because it implies that the source of the mineral must be in the catchments of both creeks. There is another possibility, that the swampy ground represents a former course of the Yarrow and that there are in fact large gemstone deposits present under the swampy areas.

It’s been quite a while since I checked out anything but the lowest part of the creek. In fact, it’s been 12 years since I went much further than that. Access is complicated by the fact that we never had a 4 wheel drive vehicle and relied on others on the few times we went there. Walking from The Crossing is the best bet, allowing 20 minutes to the point where the track crosses the creek.

I’m looking forward to hearing of good finds there one day. The landowner certainly believes that Frenchies Swamp Creek has more potential than Yarrow Creek. I hope he proves to be correct.
Check out the videos and blogs of Sue's Favourite Spot and the Glory Hole for more information and ideas. 
Photographs are unfortunately rather few. Sorry about that. The only one of a day's best finds was done on a scanner. Be assured that there were many good finds made over the years.
Best finds from an outing in 2006

Monday, 6 January 2014

“DOWN THE HILL” YARROW CREEK, NEAR GLEN INNES NSW AUSTRALIA

LIST OF ALL BLOG ENTRIES TO DATE

10.2 and 4.9 carat sapphires
Thanks to Google Earth. "Down the Hill" is in the centre
Many visitors to Glen Innes have enjoyed a day’s fossicking at “Down the Hill”, both on our Wednesday Baptist Church trips and during Minerama. I’ve written about the place in two previous blog entries (Quartz at Down the Hill and The Big Sapphire). Several videos have also covered the area (one, two and three). Click on the links to go there. 
                      “Down the Hill” lies downstream of “Through the Fence” and upstream of “Underground River”.

Down the Hill is an area with many rocky outcrops and, most notably, an abandoned channel through which the creek only flows in flood. At one time this was the most productive area, but the old diggings have mostly filled with sand and no-one seems too keen to spend the day removing it when they could search among the rocks. At the lower end of the channel the wash was at least two metres below the overlying sand. The last we saw of it, there was lots of black jack and    
Cliff O'Brien digging in the old channel 1998
presumably gems, but we were beaten by inflowing water and finally by a flood which filled up the hole with sand. Maybe one day, during a drought, fossickers will get another chance to experience the thrill of working this spot.
At some time, probably in the 1960’s, a small mining operation operated at Down the Hill. There was the remains of a shed or hut when I first visited the place in 1988 but hardly any sign of actual mining. This was on the flat immediately below where we parked. The only other sign of previous visitation was a Tamworth 1 pint milk bottle I found in the creek just below old hut site.
4.3 carat sapphire, 11.6 carat zircon (July 2008)
One day's small finds - December 2009
The gemstones are the usual ones for Yarrow Creek – sapphire, zircon, pyrope garnet, the occasional topaz and enstatite and, of course, quartz. My one and only cuttable ruby came from here, as well as my largest sapphire, best dog’s tooth crystal and biggest quartz 
0.3 carat ruby
Snowing July 2008
crystal. This is more a    reflection of the sheer quantity of wash we found than its superior  quality.
Snowing: July 2008 - the same day as the gemstone group above was found! July 2008