The Seven Stages in Tumble Polishing Stones: The Selected 40 Stones

The first Post in this series described Stage One, Stone Collection. To illustrate the next six stages in the tumble polishing of stones, I decided to select 40 of the stones I had collected at Riverton in early November. I chose a range of sizes, colour and quality. The following are photos of all 40 stones, first of all how they appear dry and then how they appear wet. This demonstrates how wetness brings out colours and patterns much better.

Stones 1 to 5:

1st 4 dry1st 4 wet

It will be interesting to see how much of each stone is worn away throughout the tumbling process. Stone 1 (far left) is about 8 cms long and about 5 cms wide at its widest point (using the graph paper it is lying on in the “dry” pic above).  Stone 3 is about 6 cms long and 4.5 cms wide, while Stone 5 (far right) is just over 7 cms long and is 3 cms wide. I think that Stone 1 is of volcanic origin, as it has small specks in it that would have originally be gaseous pockets, and will turn out to be similar to another Riverton stone I polished recently (below). 

DSC07257

Stone 2 is also probably volcanic in origin, having similar specks. Stone 4 looks like a conglomerate (which simply means it consists of small rounded stones cemented together in a fine-grained matrix). [As its surface became clearer after some tumbling, I decided Stone 4 is in fact a breccia, composed of angular fragments.] Stones 1, 2, 4 and 5 would be too big for a 3lb barrel.

Stones 6 to 10:

2nd 4 dry2nd 4 wet

These are progressively smaller, with Stone 6 (far left) being about 6 cms long and 4 cms wide. Stone 7 could be argillite (a kind of mudstone subjected to heat and pressure) or epidote (green coloured rock), Stone 9 is a breccia (which simply means it consists of broken fragments of very small stones) and Stone 10 is another conglomerate. 

Stones 11 to 15:

3rd 4 dry3rd 4 wet

The progression to smaller continues. Stone 14 (second from right) is a pink granite that is just over 5 cms long and is just under 4 cms wide at the top. Stone 12, a quartzite, demonstrates how wetness brings out the nature of a stone. Dry, it appears a bland white. Wet, patterns of colour in a strand-like formation become visible with a subtle depth being present. Stone 15, which could be argillite, has an interesting wavy band of white silica.  

Stones 16 to 20:

4th 4 dry4th 4 wet

Stones 18 and 19, both about 4 cms long, are potentially quite spectacular. Stone 18 has a number of different coloured bands. Stone 19 contains contrasting black and white sections, and it will be interesting to see if these erode or polish differently.

Stones 21 to 25:

5th 4 dry5th 4 wet

Stone 25 (far right) has some interesting bands that will be brought out by the tumble polishing, but Stone 22 (second from left) may turn out to be even more interesting. The white on the surface of Stone 23 (middle) may be worn away in the process it goes through, but there may be interesting patterns underneath.

Stones 26 to 30:

6th 4 dry6th 4 wet

Stone 26 (far left) is 3.5 cms long and just over 2.5 cms wide. Its two-toned character attracted my eye on the beach. White is a colour that always stands out on the beach too, Stone 27 being a white quartz with a couple of dark intrusions.

Stones 31 to 35:

7th 4 dry7th 4 wet

Stone 31 (left) may be part-jasper, and Stones 32 and 34 are probably varieties of jasper. Stone 33 has interesting reddish protuberance that caught my eye on the beach. Stone 35, white quartz, is 3 cms long and just under 2 cms wide. 

Stones 36 to 40:

8th 4 dry8th 4 wet

The smallest stone, Stone 40 (far right), jasper, is 2 cms by 1.5 cms. Up to 20% of a stone may be worn away by the tumbling process so not much may be left of this at the end. However, small stones are good in a tumbling barrel as they “carry” the grit and polish to the larger stones.   

I weighed the 40 stones on a set of scales I have in my stone tumbling shed. First placing the empty container on the scales, I moved the setting back to zero so that only the weight of the stones would be indicated = 1605 grams (3.5lbs).

a - weigh in

I will weigh the stones after each stage of tumbling to see how much of them is worn away. 

The next Post in this series describes Stage Two of tumble polishing, the 100 grit tumble.

How Much of a Stone is Worn Away During Tumble-Polishing?

How much of a stone is worn away during any stage of the tumbling process is of course dependent on a number of factors. The three major ones are the hardness of the stone, the size of the grit/abrasive used, and the length of tumbling time.

Most of the books on stone tumbling don’t comment on this issue, though Del Fairfield in “Lapidary” (a “Teach Yourself Book” published by St Paul’s House, London, in 1973) mentions that seven days tumbling in grade 80 grit leads to “about a 5 per cent reduction” in weight (page 15). 

I recently decided to pay some attention to this question so I purchased a small set of digital scales. I have done the calculations for two batches of stones so far.

For a batch of Riverton Back Beach stones that went into a 4lb barrel and were tumbled for 6 3/4 days with 7 tablespoons of 100 grit: Starting weight of stones = 1620 grams; End weight of stones = 1424 grams. This means that 196 grams of the stones were worn away from them, which is just over 12% of their weight.

For a batch of Birdlings Flat stones that went into a 3lb barrel and were tumbled for 5 1/2 days (there was a loss of electricity which shortened the normal one week’s tumbling time) with 4 tablespoons of 220 grit: Starting weight of stones = 862 grams; End weight of stones = 820 grams. This means that 42 grams of the stones were worn away from them, which is just under 5% of their weight.   

Orepuki Stones after Stage One of Tumbling

Orepuki is a small town near a beach right at the bottom of the South Island. It is often mentioned as a good place to find interesting stones. I visited there in February and April this year and brought home some stones for polishing. These photos are of  my first batch of Orepuki stones just out of a 4lb barrel where they had been tumbled for a week in 100 mesh silicon carbide grit. I am just about to inspect each one to decide what should be done with it next.

 

Polishing Agates from Birdlings Flat: Stage One

I found a small number of agates at Birdlings Flat and was given a number more by people I met on the beach. I have now tumbled these for one week in 100-mesh silicon carbide grit (see the bottom of this Post for an explanation of what agate is). The interesting results are as follows: 

The Gitche Gumee Museum is a rock and mineral museum in in Michigan. Its website has the following explanation about agate and its formation:

“Agate is a form of chalcedony, which is silicon dioxide in the form of microscopic fibrous quartz crystals. Agates naturally develop when an empty pocket inside a host rock, usually volcanic lava,  fills in molecule-by-molecule, layer-by-layer, as these microcrystals form concentric bands or other patterns. The colors and arrangement of the microcrystals are influenced by changes in pressure, temperature, and mineral content that occur during the formation process. The empty cavities and seams filled with fluids rich in dissolved and suspended quartz molecules (silica), as well as other mineral impurities. When the silica concentration became supersaturated, it developed a gelatin-like consistency either throughout the pocket or in a layer that served as the active crystallization front. Over time, the silica molecules began to form miniature fibrous microcrystals that attached to the sides of the cavity or seam. During the filling-in process other mineral impurities collected at the inside of the chalcedony silica band, forming intervening and often contrasting bands.” 

Wikipedia puts it like this:

“Most agates occur as nodules in volcanic rocks or ancient lavas, in former cavities produced by volatiles in the original molten mass, which were then filled, wholly or partially, by siliceous matter deposited in regular layers upon the walls. Agate has also been known to fill veins or cracks in volcanic or altered rock underlain by granitic intrusive masses. Such agates, when cut transversely, exhibit a succession of parallel lines…giving a banded appearance to the section. In the formation of an ordinary agate, it is probable that waters containing silica in solution – derived, perhaps, from the decomposition of some of the silicates in the lava itself – percolated through the rock and deposited a siliceous coating on the interior of the vesicles. Variations in the character of the solution or in the conditions of deposition may cause a corresponding variation in the successive layers, so that bands of chalcedony often alternate with layers of crystalline quartz.” 

Birdlings Flat Stones After First Stage of Polishing

These stones have spent one week in a tumbling barrel with 100-mesh silicon carbide grit. This first stage of the tumble-polish process removes the weathered outer layer of the stone and brings out its colours more clearly. Many of these stones will be quartzites.

 

Stones in the Process of Tumbling

These stones have undergone the first stage of tumbling with 100 grade silicon carbide grit. Most of them are from Riverton beaches, in Southland, but a couple are from the West Coast of the South Island (New Zealand). Some will need more tumbling in this coarse grit because they still have small pits or scratches not yet smoothed away.

Pre- and Post-100 Grit

When collected from a Riverton beach, stones are already rounded and smooth from hundreds of years of natural tumbling. When wet, the stones reveal their polishing potential – polishing brings out the colours more intensely and fixes their shine. 

Below are photos of Riverton stones before going into the barrel with 100 size silicon carbide grit, the first stage of tumbling, and after four days in the of tumbling (they then go back for another three or four days to complete the first stage of the smoothing process):