Hi Everyone… very little information is provided about the questionable sample above. Photos unfortunately don’t give us viewers any idea about the weightiness of the sample. This factor alone would clearly help us to eliminate melted aluminum from consideration. Aluminum is as light as a feather so to speak. Nor does a photo permit us to do a quick
streak test on a bit of unglazed porcelain from around the house such as the unfinished bottom of beige / white coffee cups or soup bowls. This test would eliminate all brittle white / silvery sulfides from contention, because these sulfides do not produce a metallic silvery streak, but rather they produce darker non-metallic streaks.
The sample above does not look natural to me, but even silver that has been melted will look unnatural. So our first question is if the silvery material is embedded in a rock matrix. If so, that too would certainly eliminate melted aluminum from contention.
What is responsible for producing the widespread creamy / slightly yellowish discoloration on the sample? Does it result from using artificial lighting for the photos? If we had the sample in our hands, we would immediately know the answer to that question. It looks similar to commonplace
lead oxide, the same stuff we see on lead bullets that have been in the ground for decades. That could indicate possible galena smelting / lead melting at some time in the past.
A simple
specific gravity determination in conjunction with a
streak test on your sample would go a long way towards identifying it. But I think it would be a better idea to simply have a quick XRF or some other type of analysis completed to be sure.
Gunsil’s comments above are correct. Most silver does not occur in the form of nuggets or native silver embedded in rock specimens. In actual fact, most of it is smelted primarily from sources of
acanthite and to a lesser extent from other non-native silver ores. Acanthite is a brittle, dark silver sulfide (Ag2S) with 87% silver composition. It is not field detectable unless it contains detectable native silver, obviously we recover acanthite incidental to digging native silver signals.
Galena, a brittle lead sulfide ore that produces a very dark streak test result, is a primary source of silver because it often contains a considerable amount of acanthite as an impurity. Acanthite does not influence galena to be more easily detectable, in fact if the acanthite concentrations were typically much higher than we normally see, the opposite would be true. Galena, depending on its structure and configuration, is normally easily detectable with a prospecting-capable / sensitive VLF detector. It does not react to either of my ground-balancing PI detectors, even utilizing the most sensitive settings and small mono coils, and with the ground balance feature turned OFF for use in a sensitive bench test.
Native silver occurrences in North America are well-documented in mineralogical and applicable mining literature. In the silverfields of northeastern Ontario it occurs in the form of hardrock veins, and as hardrock and nugget float material similar to the examples depicted below. There are a number of documented (photographed) examples of our silver float found exposed on the surface at the turn of the previous century that weighed several hundreds of pounds. Modern day electronic prospectors have found countless fine examples of native silver float over the past 40 years or so…………………….Jim.