PayPal-Standard-Logo
Home Subscribe Advertise About Us Contact Us downloads Links


Click on a title below to view the abstract

EDITORIAL
David Green
MINERAL NEWS
Mick Wolfe
GREYSTONE QUARRY, CORNWALL
Nick Elton • David Green • Jeremy Hooper • Stefan Weiss

Front cover of UKJMM No. 24.
56 pages, full colour.

 

UKJMM No. 24
Shipping:

Editorial
Digital Micro-Photography

David Green

There have been major improvements in the technology used in digital cameras recently and for the first time they rival photographic film in terms of the quality of images that can be recorded. Digital cameras can routinely produce images that are good enough for publication and are widely used by collectors and mineralogists to record both sites and specimens. We trialled a number of digital images in the article on fluorite from the Rogerley Mine, Weardale, in the last edition of this journal. Green fluorite from the northern Pennines is difficult to record on photographic film and the digital technique had the advantage that it gave much better colour rendition. Other coloured fluorites from northern England are also problematic, the famous blue fluorite from Florence Mine in west Cumbria commonly registers a dirty pink on film (the photo in issue 22 of this journal was laboriously altered to produce a more realistic match to the specimen). Scorodite and pharmacosiderite from Cornwall almost never photograph properly, perhaps due to some small difference in the response function of the human eye when compared to film. They do work as digital images.

Digital photography is inexpensive and virtually instantaneous and digital photos will be increasingly used to illustrate articles. The images generated by most digital cameras are too small to produce the front covers of journals, but more than adequate for printing at single column width. Colour images in the UKJMM are printed at 350 dpi (dots per inch). This means that an image printed at single column width (about 80 mm) needs to be a little over a thousand pixels across, well within the capabilities of modern cameras.

Digital cameras are also very useful when combined with microscopes in high magnification photography. Most collectors have used a stereomicroscope at one time or another and almost all of us take a hand lens when collecting in the field. It is hard not to be impressed by the beauty and perfection of crystalline specimens at high magnification, but photography in this size range is beset with difficulties. Anyone working at high magnification has two major problems to contend with: resolution and depth of field. These are additional to the normal problems of specimen photography, which boil down to choosing the specimen and lighting it properly. Photography at high magnification is a compromise between resolution and depth of field. Reduce the aperture too much (by shooting at a high f-number or inserting a pinhole into the microscope system) and the image goes soft (low resolution due to diffraction). Work at full aperture and the resolution is good but the depth of field is miniscule so almost nothing appears in focus. That is why most successful high magnification photos are of flat specimens or isolated single crystals.

Digital technology provides a way to cheat the laws of optics by combining multiple images of minute specimens. Image processing software makes it possible, though not easy, to combine only those bits of the image that are in focus. A single composite image can be made at high resolution with good depth of field from a stack of images by taking only those parts that are in focus. This technique is not new, but it is only recently with the advent of cheap digital cameras and image processing software that it has come within range of amateurs. In principle, the procedure is simple. Beginning with the uppermost crystals in focus the photographer works carefully down through the specimen producing a stack of digital images one on top of the other. These can be combined by hand in standard image processing software or using CombineZ, a freeware program which is available via the internet. Which of these options is best depends on the type of specimen being photographed, highly detailed images tend to work better with CombineZ, while those with a few blocky single crystals, or with a very large depth, are best done by hand.

Microcrystalline assemblages are an important facet of mineralogy, often comprising rare and unusual mineral species, but photographic difficulties mean they are not commonly figured. Digital techniques should go some way toward alleviating the problem. Methods are still at the development stage but we intend to produce a dedicated article in the near future when several different optical systems have been tested. In the meantime, a few illustrations are included on the facing page to show the improvement in image quality which is possible using the technique.

Left. Carminite crystals to 0.5 mm from the Kintore Opencut, Broken Hill, New South Wales, Australia. This image was generated from eight separate digital slices using the freeware program CombineZ. Bernie Day collection.
Right. Azurite crystals 2.5 mm tall from Dolyhir Quarry, Powys, Wales. This image is a manually combined composite of ten separate slices.

 

Back to the top


Famous British Mineral Localities:
Greystone Quarry, Lezant,
Cornwall

Nick Elton
David Green
Jeremy Hooper
Stefan Weiss

At Greystone Quarry, lead-copper-zinc veins cut a structurally complex metasedimentary sequence which is pervasively intruded by dolerite sills. The veins contain major primary quartz, with calcite, chalcopyrite, dolomite, galena and sphalerite. Supergene alteration has produced a diverse assemblage of secondary minerals including anglesite, aurichalcite, caledonite, cerussite, dundasite, hemimorphite, hydrocerussite, leadhillite, linarite, malachite, mimetite, plumbojarosite, pyromorphite, rosasite, vanadinite, and wulfenite many of which are rare in southwest England. The supergene mineral suite contains the only Cornish descloizite, crocoite and schmeiderite and the first British vauquelinite. The east-west veins at Greystone Quarry are mineralogically and structurally distinct from the north-south lead and zinc bearing cross-courses which are well known in southwest England. They are probably associated with late-stage Variscan deformation.
20 pages.

Leadhillite crystals
Wulfenite

Left: Tabular slightly corroded leadhillite crystals 6 mm across with minor linarite in quartz matrix. Peter Golley specimen, photo David Green.
Centre: Transparent yellow cerussite crystals to 1.5 mm on limonitic matrix. Richard Bell collection, photo David Green.
Right: An orange wulfenite crystal 0.3 mm across from Greystone Quarry. Photo David Green.


Double page spreads from this article.

Back to the top


The Petrography of the Zinc-Lead-Copper Ores at
Crow Island, Killarney, Ireland

Rob Ixer

Crow Island, close to Killarney, Ireland is the smallest and least tectonized of three related polymetallic deposits emplaced in the Carboniferous Ballysteen Limestone Formation that were mined in the eighteenth and nineteenth centuries. The mineralization comprises sphalerite-galena-pyrite-chalcopyrite-arsenopyrite-tennantite with trace amounts of electrum. The ore records an early metasomatic replacement phase of mineralization one that is all but obliterated in the ores from the other two deposits at Ross Island and Muckross Mine.
6 pages.

Back to the top


The Development of Supergene Lead Mineralisation
in Central Wales

John Mason

The in situ alteration of hypogene vein galena to cerussite, pyromorphite and wulfenite is of widespread occurrence in the formerly important lead-mining district of Central Wales. Detailed fieldwork over many years has shown that this supergene lead mineralisation can be divided into two texturally and paragenetically distinct assemblages. Of relatively restricted occurrence is a highly evolved, coarsely crystalline assemblage that is developed in particularly permeable lode systems. This assemblage is commonly associated with extensive bleaching of wallrock and the complete oxidation of primary sulphides. Of more widespread occurrence is a microcrystalline assemblage associated with partly oxidised sulphides in relatively unbleached wallrock. The cited evidence is used to advance a theory for the genesis of supergene lead mineralisation in Central Wales. The coarsely crystalline assemblages are thought to be the surviving remnants of pre-glacial oxidation zones, produced by deep weathering during Mesozoic to Tertiary times and now largely removed by glacial erosion. The microcrystalline assemblages are more probably the product of geologically recent alteration, post-dating the last glaciation.
12 pages.

Left: Massive coarsely crystalline cerussite from the dumps at Frongoch Mine. Steve Rust specimen.
Centre:
Coarsely crystalline pyromorphite on quartz from the main pipe, Bwlchglas Mine. Specimen is 55 mm tall.
Right: Early coarse cerussite overgrown by later microcrystalline pyromorphite with minor bipyramidal orange wulfenite. Specimen from Bwlchglas mine, John Mason collection.
Photos David Green.


A double page spread from this article.

 

Back to the top


Apatite Crystals from the Coal Measures
of Northern England

Tim Neall

Apatite crystals are described from two localities in the Coal Measures (Upper Carboniferous) of Northern England, near Gateshead, Northumberland and Sheffield, South Yorkshire. They occur in open fractures in septarian nodules as small tabular crystals associated with a variety of other minerals including dickite, siderite, carbonates and sulphides.
1 page.

Back to the top