A Review of the University of Auckland’s “Geology: Rocks and Minerals” Website

Index to “StoneSpeak” Reviews and Articles Series

A Review of “Mindat.org”

A Review of the “GeoTrips” Website

A Review of Peter Ballance’s (2017) “New Zealand Geology: An Illustrated Guide”

 

Online Access to “Gemstones” by Jocelyn Thornton (1985)

This valuable booklet, now hard to find in secondhand bookstores, used to be available online on Peter Thornton’s website [www.peterthornton.com/files/nzgemstones.pdf]. I briefly reviewed it in TumbleStone Blog back in 2016 (see here) and have often referred to it, for example, in Posts on Gemstone Beach and Slope Point. However, I noticed a few weeks ago that it was no longer available. I have managed to find two alternative ways to access it online.

The first (and probably the best) is via an information site on Tuatapere, a town not far from Gemstone Beach. The site is called “On Natures Edge – Tuatapere” and its “What’s Here” section has a brief page on Gemstone Beach www.onnaturesedge.co.nz/tuatapere/whats-here/gemstone-beach. This page has a link to Thornton’s booklet (see below). Clicking on the link brings up a pdf file of the booklet, the same file as used to be available on Peter Thornton’s website. By clicking here, you can go directly to the pdf.

The second alternative source is through StudyLib.net (see below) – click here. It can take a little time to load, and initially the pages look small, but it appears to be a good reproduction. You can scroll down through the pages within the file, and can zoom in to a size that suits you. The links in the Contents page are shortcuts to other pages, as in the pdf file in “On Nature’s Edge”.

Note that the booklet itself contains 74 pages, each side of each sheet being numbered. The pdf files, however, counts two facing pages as only one page, reducing the page numbers by half.

Alternatives to Plastic Pellets as Tumbling Media: Reviewing the Advice – Part One

One of the issues facing rotary tumble polishers like myself is the use of “media” in a barrel. As RockTumbler.com puts it: Tumbling media has four functions: 1) it delivers grit to hard-to-reach rock surfaces; 2) it is used to cushion fragile rock materials during the tumbling process; 3) it is used to improve the tumbling action in the tumbler barrel; and 4) it is used as a filler to make up for lost [or inadequate] volume. An instruction booklet that comes with Lortone tumblers, “Professional Gemstone Tumbling”, refers on page 8 only to the use of plastic pellets as an option that can be considered, especially during the latter two stages of tumbling (see photos above right). My supplier, Rotorua Lapidary, stocks plastic pellets and offers them as an integral part of tumble polishing (see here). I have incorporated them into my tumbling routine, always using a few even with coarse grit, increasing the number with each stage. Item 8 in my Posts on What Do I Need to Start Tumble Polishing Stones Myself? And What Will It Cost Me? explains my use and storage of plastic pellets. I am very careful not to lose pellets down the drain when rinsing stones from the barrel, assiduously checking for them even where the water drains onto the ground outside my tumbling shed. However, once I became aware that tumbling especially with coarser grit actually wears away the pellets, no doubt releasing microscopic bits of plastic into the environment, I started to have second thoughts. I would like to minimise the amount of plastic I am responsible for in the environment. The following is my initial research into alternative tumbling media, looking at the advice and information given by various sources.

A good starting point for research on any tumble polishing matter is Steve Hart’s “Modern Rock Tumbling”, published in the USA in 2008, what I have called “the best rock tumbling book around”. Hart mentions the use of plastic pellets but states that he prefers ceramic media (see photos above). [He also notes that if he does use plastic pellets, it tends to be mainly for the later stages of tumbling, and he uses them only once before relegating them for use at earlier stages.] On pages 27-28, Hart writes: I have learned to use non-abrasive ceramic shapes in assorted sizes in order to make up for any errors in making up the “perfect” assortment of sizes and to act as a cushion for brittle batches. Use 1 to 2 tablespoons of ceramic shapes for every pound of rocks to start – then make up for lost volume with the shapes [if necessary]. I bought some of Hart’s ceramic shapes in 2016 from his Little Red Store located in California. I used them on a 320 grit load but thought they might have damaged a couple of stones. So I set them aside and have not yet come back to them, partly because the plastic pellets work so well. I have seen comments on the Facebook Group “New Zealand Lapidary, Rocks, Minerals, Fossils” by people who have found ceramic media to work effectively for them.

One rock tumbling retailer in the US, who runs the RockTumbler.com website, summarises the use of plastic pellets versus ceramic media here in the following way: Plastic pellets were the most popular tumbling media from the 1960s through the 1990s. They were used to cushion the stones and reduce bruising caused during tumbling. Today most people use ceramic media, but some have used plastic pellets for decades and still prefer them for rotary tumbling. Ceramic cylinders smooth the tumbling action and this results in less bruising of the stones. Ceramic media is also hard and more effective at grinding and shaping stones. When ceramic media became popular in the early 2000s, most people who tried it stopped using plastic media – because ceramics were more convenient. When using plastic pellets, the pellets can only be used with one size of grit – because tiny particles of grit become embedded within them. When using ceramic pellets, the rock mud and the grit rinse right off of the stones between tumbling steps. Here is the verdict of our customers: Today we sell over 10 times more ceramic media than plastic media. One way to expand our knowledge of the alternatives to plastic pellets is to ask, What did tumble polishers use before plastic pellets? It is worth consulting older literature for the answer.

Mainly in the first year of my tumble polishing, I managed to buy a few older books on tumble polishing, primarily from Great Britain, the United States and New Zealand. The following three paragraphs summarise the kind of advice given in some of them. Firstly, two New Zealand books: Lyn and Ray Cooper’s (1966) “New Zealand Gemstones” does not mention tumbling media when going through the various stages, though noting that smaller stones can be used as fillers. When discussing how to tumble softer stones, their section on obsidian states (pages 55-56): The polish consists of 2 lb of tin oxide, 1 lb of sugar and 1 cup of Rinso to each 10 lb of stones… Various overseas publications suggest the use of fillers such as plastic pellets for obsidian and soft stones; we do not recommend them. We have used plastic pellets and found that our Rinso and sugar additives give exactly the same, if not better results. Natalie Fernandez (1981), in “The New Zealand Rockhound”, also mentions “hard small beach stones” as a filler (page 126). On the same page, when discussing the polishing stage, she writes: Suitable fillers if required at this stage are saw-dust, shavings, rubber strips, even walnut shells and kitty litter. She goes on to add a note about role of sugar: Adding a little sugar slightly thickens the mixture which keeps the polishing material in suspension.

Next, to look at four British books (see photos above). In “Pebble Polishing” (1972), Edward Fletcher does not mention tumbling media when he provides instructions for the various stages of tumbling. However, for the polish stage, he mentions on page 69 that “wallpaper adhesive” can be used to prevent the cracking and scratching of stones when “any harsh banging or unrhythmical striking of pebbles together” is heard: Add a small amount of wallpaper adhesive to the mixture. The aim is to thicken the liquid in the barrel so that it cushions the fall of each pebble. Do not make the mixture too thick, otherwise the effectiveness of the polishing agent could be reduced. A thin cream consistency is ideal…It also increases the time you must allow for the polish to do its work because movement inside the barrel is reduced owing to the greater viscosity of the thickened liquid. A polishing stage of four days without paste might take seven days if paste is added. Secondly, Del Fairfield’s (1973) “Lapidary” mentions quite a range of tumbling media though for use only at the polish stage: It is customary to add a quantity of soft material to the barrel to provide cushioning during the polishing process and also to carry the polishing material. Various materials have their advocates, including leather, wood, hardboard, plastic granules, cork crumbs etc. Leather, for instance, should be heavy soling leather cut into 1/2-inch squares, and wood should be in 1/2-inch cubes. This additional material should be about one-third the volume of the stones, and when stones, cushions and slurry [tin oxide or cerium oxide] are all mixed up there should be an adequate coating over everything but not much spare slurry (page 16). Thirdly, V.A. Firsoff and G.I. Firsoff, in “The Rockhound’s Handbook” (1975), also recommend the use of “small pea-sized stones” which “ensure more intimate contact between the main charge [stones] and the abrasive” (page 181). They mention the use of “vermiculite” to cushion the stones at the polishing stage (page 182). Vermiculite is a hydrous phyllosilicate mineral (see Wikipedia), a mica-like mineral, and one of its commercial uses is as an addition to potting soil in containers, helping to improve drainage and moisture retention. Finally, Eric Shore includes the following comments in his “Lapidary for Pleasure and Profit” (1978) when discussing the polish stage: Additives either of cubes of hardwood, pieces of felt, or leather should be added to the charge [stones, polish powder and water] to give a cushioning effect whilst tumbling. These will help prevent chipping 0f sharper edges and points and also act as a polisher when rubbing against the stones. If leather is used, thick pieces are better than thin, as the latter tend to cling to the barrel and not mix with the stones (page 84). He also mentions that sawdust can be used, along with detergent, in the final burnish.

An Australian book published in 1965, Bill James “Collecting Australian Gemstones”, actually mentions “plastic granules” to prevent damage during polishing for “special” stones (page 97), but is silent on tumbling media for the routine stages for most stones (see photos above). A book published in the USA in 1977 mentions tumbling media, and gives mainly similar advice to the British authors reviewed above. “The Complete Book of Rock Tumbling” by Christopher Hyde and Richard Matthews has a section on “Buffering Agents”: These are used to carry the abrasive and also to prevent severe impact of one stone against the other… Such materials include wood chips, plastic pellets, sawdust, sugar and wallpaper paste… Old-timers often had their own favorite additives, which helped to make rock tumbling a mysterious art. These included products such as walnut shells, rice hulls and even banana peels. Although such things may work, we don’t recommend using them (pages 33-34).

In Part Two in this Series (not yet available), I will review some contemporary internet information on tumbling media.

Tips on Using “Maps Past”

In Maps as a Resource: New Zealand’s “Maps Past”, Part One and Part Two, I demonstrate ways in which the “Maps Past” website provides maps of interest to researchers. The following is a step-by-step introduction to using the website for those who might find it useful.

Step One: Go to http://www.mapspast.org.nz. The following (or something similar) is likely to open as the home page:

01 home page

The next two steps are aimed at getting rid of unnecessary material from the screen before zeroing in on a location of interest.

Step Two: Get rid of the “Select basemap” pop-up menus by clicking on the “x” on it (circled in black on the image below): 

02 home page base map pop up

Step Three: Remove the text material from the lefthand side of the page by clicking on “Mapvv” (partly circled in black in the image below) which is on the righthand margin at the top:

03 home page margin

This then should leave you with a map of New Zealand  and seven icons at the left top of the page:

04 home page simple

The seven icons are:

05 icons

From left to right:

White plus and minus signs on blue background = Zoom in/Zoom out.

Three layers icon = “Select basemap” = Brings up list of 14 options, most of them decades.

Cog icon = “Map options, Coordinate format” = Brings up list of 11 options.

White i in blue circle = “Show mapsheet details for current series when you click on the map”.

Clipboard list with white i in blue circle on bottom right corner = “List all available mapsheets at point you click on the map”.

Magnifying glass with three arrows = “Zoom to extent of current mapsheet/series”.

Two chain links = “Show URL of currently displayed map”.

Below I will discuss the use of four of these icons – the first, second, fourth and fifth. I have found that I can achieve what I want through using these four. 

Step Four: Use the “Zoom in” icon (white plus sign on blue background at top left of screen) to zoom in to the location you want to examine. You are likely to also need to move the map to bring your intended location to the centre of the screen – move the cursor to somewhere on the screen, click and hold, then move the cursor – this will move the map. I have chosen to zoom in on Riverton at the bottom of the South Island (see below). At the bottom right hand of the screen are some figures, the scale of the map on screen, the map sheet or series, and co-ordinates of the cursor. In this case, for example, there is “Scale = 1 : 27K” (27K = 27000) and “NZTM2000” map series. This information may or may not ever be of use to you.

06 Riverton11

 

Step Five: Once you have zoomed in to the location you want, at the scale or level of detail you want, you can then click on the “Select basemap” icon (three layers icon) at the top left to choose which map you want to see.

 

07 Riverton select basemap start1111

I decided to try to find the earliest map. I clicked on the fourth last map “NZMS13 1899”. The list then disappeared and the screen went blank. This means such a map does not exist. I clicked again on the “Select basemap” icon to bring the list of maps up again, and clicked on “NZMS13 1909”. Same blank result. When I next clicked on “NZMS13 1919”, the following map came up:

08 Riverton 1919

 The 1929 map was the same. The 1949 map was not at a good level of detail:

09 Riverton 1949

But the 1959 map was a good one:

10 Riverton 1959

And we could go on, choosing more recent maps or the air photo…

Step Six: Finding out what maps are available for the location. To do this, you click on the icon of a clipboard list with white i in blue circle on bottom right corner – this is to “List all available mapsheets at point you click on the map”. This icon turns green when you click on it. You then click on a point on the map and a popup list appears which you can scroll down. This lists all maps that have been published or are available for this location. 

11 Riverton map series avail

The earliest map listed for Riverton is Series: NZMS13 Sheet: SD58, Printed: 1910. This will be why no map came up earlier for 1909 but one came up for 1919 when I was using the  “Select basemap” icon. 

Step Seven: Finding out which map you are viewing. When a map is on the screen, you can use the icon of the white i in blue circle = “Show mapsheet details for current series when you click on the map”.

12 Riverton map being viewed

 

This icon also turns green when you click on it. You then click on a point on the map and a popup list appears which identifies the map that is being shown. In the case above, the 1910 map is identified even though the map came onto the screen originally when I was using the “Select basemap” icon and had chosen “NZMS13 1919” from its menu list. In other words, the decade menu list that appears when you click the  “Select basemap” icon does not mean that the map that comes up was published the year shown (1919 in this case) but it may have been earlier (1910 in this case).

It was the use of these steps that helped me obtain the material discussed in the Posts Maps as a Resource: New Zealand’s “Maps Past”, Part One and Part Two, and which has proved useful in my local history and family research.

Maps as a Resource: New Zealand’s “Maps Past”, Part One

Over the past few months, I have been doing some research on the district in which I grew up, around Waikaka in Southland, and on the members of my family who first settled there in the 1870s and their involvement in farming and gold dredging. This is an area I return to from time to time, and from which I collect stones. Recently I have been seeing what is available online in terms of historical maps. One very useful website I have discovered is “Maps Past”  http://www.mapspast.org.nz which, oddly enough, does not have a page giving details of who has produced the site.

The opening page of “Maps Past” presents a map of New Zealand, and it is possible to zoom into any particular part of the country. Then you are able to click on different dates (set as decades, starting at 1899 with only 1939 not available) and bring up maps from that time of the area on your screen. Sometimes as you go from one decade to another, the same map will be presented, depending on when new maps were constructed. I will illustrate this by showing the different maps available for Waikaka and the area to the south which includes “The Mains”, the farm on which I grew up. 

There are nine different maps that are available for the Waikaka area, one of which is a recent aerial photo. The following are thumbnails that will expand when clicked on (there is a “View full size” underneath the expanded image in the viewer – you may need to scroll down to see it):

This first part of this Topic will deal with the first four of these maps. The other five are dealt with in Maps as a Resource: New Zealand’s “Maps Past”, Part Two. Note that the following map images are not expandable – use the thumbnail above for a more detailed view of any of the maps.

The first map is for the decade ending in 1899. It is actually from a map of the Chatton Survey District published in 1888:

001 - NZMS13 1899

It is interesting to note the areas around Waikaka designated as “Auriferous Reserve” and “Gold Reserve”, and the area of dots to the southeast of the town labelled “GOLD WORKINGS” (though it is very difficult to see this label). Gold had been discovered near Waikaka in 1867 and the following 60 years saw various phases of panning, mining, sluicing and dredging. Section 30 of Block 3, located directly south of Waikaka, just below the centre of the map, was bought in April 1876 by Hugh Paterson, my great-great-grandfather. This was the beginnings of “The Mains” farm.

The second map is for the decade ending in 1929. It is actually from a map of the Chatton Survey District published in 1929:

002 - NZMS13 1929

One noticeable addition to the map is the Waikaka Branch Railway, constructed in 1907 and 1908 to provide faster transport of agricultural produce to markets. It was the last of the branch lines authorised in northern Southland. In “Waikaka Saga” (1962), Evans refers to James Paterson, my great-grandfather, as one of the “well-known characters” (page 191) on the train, one of the local land-owners who traveled to Gore (about 25 kms away) on Saturdays to do business. “All of these men were intensely interested in politics, religion, world affairs, agriculture, and so on. Even before the train had pulled out of Waikaka station, the argument had started and they had forgotten to buy their tickets, and so scrambled on at the last moment…[They] used to have great arguments and discussions on the train, so much so that it became quite an institution.” The railway line ran through “The Mains”, with the Pullar Railway Station (Siding) located just on the southern boundary of the farm. It is reported in the Mataura Ensign on 27 July 1909 that James Paterson was given 50 acres of the Waikaka Commonage (mining reserve) to compensate for part of The Mains being cut off from access to water. Due to competition from roading, the Waikaka Branch Railway closed on 9 September 1962 (Wikipedia). 

In the middle of “The Mains” was a rail bridge across the “Waikaka Stream”. Soon after the line opened, Leonard Paterson, my grandfather, traveled to high school in Gore by train which would slow down by this bridge so he could hop on (“Paterson Family Reunion 2002”, page 24). He was also a passenger on the final train from Waikaka in 1962, standing sixth from the right in the photo below, his wife Annie to his right. They had retired to live in Gore in 1957.

school centennial p71 last train
Source: “Waikaka and District Schools Centennial 1883-1983 Pictorial”, page 71

The third map is for the decade ending in 1959. It is actually from a map of the NZMS1 series published in 1946, the S161 “Heriot” Sheet. This is a topographic map, showing relief, using contour lines, whereas the previous two are land survey maps primarily concerned to present farm land boundaries. 

003 - NZMS1 1959

This is the same map with the approximate boundary (in black) of “The Mains”:

003 - NZMS1 1959 - Copy

Note that the road running east of the boundary of “The Mains” is called “Turnbulls Road” (after a prominent family) . In later maps this becomes “Turnbull Road”. Note also that “Tailings” are indicated in “The Mains” to the left of the railway line. Elsewhere on the map is reference to “Workings” and “Old Workings”.  These are old gold dredge tailings and sluicing areas. Most of the flat land along the west and east branches of the Waikaka Stream as far south as McNab (21 kms) was heavily dredged between 1896 and 1926. As reported in an entry on “Gold-Dredging in the Waikaka Valley” in “The New Zealand Mining Handbook” of 1906, “By means of a separating-box soil and sand are distributed over the tailings, which are left perfectly level, and when sown with clover and grass yield excellent grazing” (page 198).  In “Golden Reflections: A History of Waikaka Valley” (1992), J.F. McArthur reports: “Dredging operations disturbed the whole valley floor, which was completely turned over to the depth of 12 to 14 feet [3.7 to 4.3 metres]” (page 366). He refers to how the dredges lifted the top soil of the area about to be dredged and placed it, using an extended chute, over the area previously dredged (page 367). It has been claimed that much swampy land was improved considerably by gold dredging. Certainly I remember the tailings on “The Mains”, although prone to drying out in summer, provided great free-draining winter grazing and grew excellent lucerne (alfalfa). 

The fourth map is for the decade ending in 1969. The “Maps Past” website indicates this is based on the NZMS1 series “Heriot” Sheet published in 1957, again a topographic map:004 - NZMS1 1969

However, only parts of the railway line are indicated even though it was not removed until after 1962, when I remember my father dismantling the section that ran through “The Mains”. Maybe this is actually based on a later map. A new “Old Workings” label appears on the map to the south of “The Mains” boundary. These old gold dredge ponds on the Waikaka Stream existed even prior to the previous map.  I used to fish for trout there often as a boy, and we called it Turnbull’s Dam as it is located on Turnbull’s farm (even though it is a couple of ponds through which the river flows rather than a dam). It is interesting to note on this map that the road in the south-east corner is called “Sandy Knowes Road”. On later maps this becomes  the “Kelso Maitland Road” before becoming “Glenkenich Road”. Meanwhile, the road in the north-east is on this map called the “Waikaka Kelso Road” (the “Kelso” part can’t be read on this segment) and on the next map is called “Sandy Knowes Road”. (On all maps, “Garden Gully Road” connects these two roads.) There is potential confusion here for local historians when local people or documents refer to Sandy Knowes.

This Topic is continued in Maps as a Resource: New Zealand’s “Maps Past”, Part Two, where the next five maps are discussed. Another Post sets out Tips on Using “Maps Past” to assist you if you are not sure what to do to get started in using the website. 

“Down to the Earth’s Core”: A Documentary

I recently saw part of an animated documentary on National Geographic about what can be found as you move from the Earth’s surface to its centre. “Down to the Earth’s Core”, a 90 minute film released in 2012, uses often spectacular computer generated imagery. An earthquake inside the San Andreas Fault is shown, along with an erupting volcano and bizarre cave-dwelling creatures. Earth’s extraordinary history is laid bare, layer by layer. A number of fascinating stories are told in the course of the journey downwards, such as how prehistoric forests became modern-day fuel and how dinosaurs experienced cataclysmic death. Eventually the planet’s super-heated liquid core is reached. 

Some of the highlights for me are listed below, along with how many minutes they can be found into the YouTube video above: the Carlsbad Caverns of New Mexico, 240 metres below the surface (at 9.00 minutes); a cave of giant crystals, 300 metres deep (at 20.17 minutes); the layer of extraterrestrial iridium rock at 550 metres and its link to dinosaur extinction (at 25.45 minutes);  the accumulation of gold deposits nearly 2 kms down (at 34.22 minutes); the formation of amethyst quartz crystals at 3.9 kms (at 38.42 minutes); and how diamonds came to be, at 240 kms down (at 1 hour 8.40 minutes).