I have serious doubts that any pictures of that ore will ever see the light of day. In fact, I would be willing to bet money on it. Nice try though.

Take care,
Joe
Larry and all. I believe Wasp posted at least twice why he shared the report, and what the reports involvement with the thread is. Re-read his posts if you missed it.Ozarker wrote:we appear to be on our own in trying to figure out what it means and how it relates to the thread.
Larry
Paul Crismon was running an old fashion assay shop in which they did basic assays and the business was in decline. (My initial image was one of a spotless laboratory with the latest technologies and technicians buzzing about.) [Kind of like where Cubfan works?]Salt Lake City Desert News, Saturday May 13, 1972
Assaying: A Proud Profession Is Fading
By ARNOLD IRVINE
Associate Business Editor
Measuring a small quantity of brownish powder into a finely balanced chemist’s scale, Paul Crismon seems pretty calm about the imminent uprooting of his assay office.
He dumps the powder into a flask, adds liquid and sets the flask boiling over a Bunsen burner. The acrid fumes disappear up the chemical-encrusted chimney.
“I do the wet assaying. My helper does the fire assaying.” He explained as he wrote some markings on a beaker.
There used to be six assay offices on West Temple. Now Crismon and Nichols is the only one left. The Salt Lake Redevelopment Agency is going to move us out soon,” he drawled as he worked in the jungle of flasks, beakers, glass tubing and other chemist’s paraphernalia that crowd the laboratory. It’s hardly the spotless work area of the research scientist. The counters and walls are encrusted and stained with the remains of thousands of tests.
The agency is acquiring the assay office along with other property in the area near the Salt Palace. The old buildings will be demolished and the land sold to developers who will put it to new uses in keeping with the new West Temple image.
“It’s costing the Redevelopment Agency $27,000 to move us. They have to do it at no expense to us. The furnaces will all have to be rebuilt.” Crismon said, looking at a battery of firebrick furnaces especially constructed for the assay tests. “They cost a lot of money.”
The new location is 440 S. 4th West. Now known as Crismon and Nichols Assayers and Chemists, the firm started as Crismon Brothers in 1900. It has been at its present location, 229 S. West Temple for 67 years.
The building that houses the laboratory was built in 1905 by Crismon’s grandmother who owned the property. Crismon’s father and uncle were the founders of the assay business.
“There’s only one other old-time company assay company left in town,” Crismon said. “The Union Assay Office Inc. had to move from West Temple when the Salt Palace was built. They’re at 269 Brooklyn Ave.”
“We just do straight chemical and fire assaying. We have to use these processes because the smelters and shippers use them,” Crismon explained.
He noted that there are new assay companies in the area that employ the more recently developed spectrographic and instrumental processes.
The old assay offices have been diminishing for several years because “the small miner has been disappearing.” Crismon explained.
“In the depression days, the state had dozens of small miners. Now they’re all gone and the big companies that are left have their own laboratories,” he said.
Another cause of the decline is assaying has been the closure of the smelters at Murray, Midvale and Tooele. When Kennecott Copper Corp. took over the Garfield Smelter, the custom work was eliminated there.
Custom mill closures in Midvale, Tooele and Stockton also have cut down the assay business.
Custom smelting and milling creates umpire business for the assayers because of the disputes between the ore shippers and the processors over the content of the ore. Whenever such a disagreement arises, samples are sent to the independent assayer for tests.
“At one time or another, we’ve done umpire work from all over the world – places as far away as Saudi Arabia and Alaska,” Crismon said.
A salesman from a supply house dropped by and Crismon began looking through his chemical-laden cupboards.
“I’ll need some potassium bisulfate,“ he said.
“Business is as bad now as it was during the depression. We’re making more money but with rising costs, we’re no better off,” he mused.
Last year, he grossed about $35,000 which wasn’t as well as he had done in the year before that. This year, with more mills and smelters closed, he expects income to drop further.
Has he, because of his position as an assayer, been able to get in on the ground floor of some rich bonanzas?
We never know if an ore sample is a good deal or not. A lot of people fool themselves. They bring in the best sample they can find for assay but when they go to mine the ore body, it doesn’t have the value the assay showed,” Crismon said.
Prospectors and miners are traditionally close-mouthed about their finds and aren’t likely to tell the assayer all about them.
Come to think of it, maybe assayers are close-mouthed, too, about what they’ve acquired.
At any rate Crisomn at 64, plans to keep on assaying. “I can’t afford to retire.”
He used to put in some long hours, particularly during the prospecting booms.
“During the tungsten boom, I started working one day at 8 a.m., worked through the day, all night, through the next day and until midnight the next night,” he recalled.
“I don’t do that sort of thing anymore although I do sometimes stay here until none at night or even later. I generally start work at eight a.m. and quit at six p.m.,” he said.
As a young man, he had hoped to become a lawyer. The depression cut his law training short and he became a purser on cruise ships sailing from the East Coast.
When his father’s partner, Frank Nichols, was forced to retire from the assay business due to illness, Crismon returned to Salt Lake City, to become an assayer.
Incidentally, if you have found the “mother lode” or some such valuable vein and are wondering about the cost of an assay, the prices range from $2 for zinc copper to as much as $8 for coal and uranium.
1. The USGS has a number of published "models" on different types of ore deposits from across the U.S. Each of these models has a Model Number associated with it. These models were developed by the USGS when there were multiple analysis done on different ore deposits over a period of years that had a high commonality or a very large ore body which was of interest. These models were thus formulated off earlier analysis done on actual ore deposits - ie, these models were just a codification of what had already been found. This is what leads to a lot of the +/- symbols in the models and the multiple listings of minerals/metals/etc that can be found with a particular model. Each actual ore analysis looked at for the model development probably did not match the model exactly. There appears to be a large number of these models from what little surffing I did on the USGS site. Fore instance, here are three other models on epithermal gold deposits:
Model 25b
pubs.usgs.gov/bul/b1693/html/bull7a0j.htm
Model 25d
http://pubs.usgs.gov/bul/b1693/html/bull7khf.htm
Model 25c
pubs.usgs.gov/bul/b1693/html/bull5nqr.htm
Note that the USGS reference Garry included is for Model 25e and at the bottom of that reference it references a mine and ore analysis done in 1909!
I would conclude from this that the ore report posted by Wasp was more likely "plagiarized" by the USGS - and not the other way around.
2. Larry made the follow comment:
"And a final technical comment for now, the USGS Ep-Q Alunite Au mineral deposit model specifically states that these types of deposits are always located in vuggy veins, a characteristic that Joe Poterie made clear was not associated with Waltz’s gold. Yet, those words were deleted from the Wasp report and replaced with “quartz veins”, leading to some further speculation on my part about what this report really represents."
The actual wording out of Model 25e is:
"Texture/Structure Veins, breccia pipes, pods, dikes; replacement veins often porous, and vuggy,
with comb structure, and crustified banding."
Note that there is a semicolon after the word dikes. The second part of this sentence does not apply to the first - the first part describes structured quartz veins l. The second part speaks to replacement veins that are vuggy. Key difference between two different types of deposits.
3. One is making a very thin guess to predict what the wording is under the taped out area in the Mineralogy section - it may well be something different! Especially based on Item 2 above.
It’s difficult to say what the remainder of the Wasp report contains. Another USGS model is mentioned in the title line of Wasp’s report (Au-Ag-Te, which corresponds to Model 22b in USGS Bulletin 1693). If I had to venture a guess, I’d say one of the comparison ore samples that Wasp mentioned is supposedly from this type of deposit, but this is highly speculative. Garry (novice) has touched on this subject in a previous post.4. I suspect Wasp only posted Page 1 of the report for a reason. The info on this page is very typical of a epithermal quartz alunite gold deposit but with one key element that might expose more than desired. Not much "secret" info is exposed here, but one can see the parallel to Dutchman ore in it.