Editorial
David Green
The Future of the UKJMM
Following the retirement of Jean Spence and Mick Wolfe, who have been
indispensable members of the team for many years, there has been some
uncertainty as to the future of the UK Journal of Mines & Minerals.
We are pleased to report that the UKJMM will continue in its current
form. With the support of subscribers, authors and advertisers, we will
continue to develop the journal as a repository of information about
British mineralogy.
UKJMM Issue 32 will be the last to be covered by current subscriptions.
New subscriptions will begin from issue 33 with an additional option
to pay using Paypal via the UKJMM website. Further details and information
will be included in the next issue and on our website www.ukjmm.co.uk.
The Williams Collection
Many of us must have dreamed at one time or another of finding a collection
full of fine old time mineral specimens. Courtnenay Smales has had the
good fortune to discover and restore such a collection, which belongs
to the Williams family of Caerhays Castle, Cornwall. Caerhays castle
is situated in 120 acres of beautiful gardens in a secluded valley above
Porthluny Cove. The gardens are one of Britains horticultural
treasure houses, with a glorious collection of camellias, magnolias
and rhododendrons.
The mineral collection at Caerhays was assembled between 1780 and 1890,
in the heyday of Cornish mining, by several generations of the Williams
family. It grew to be very large, ranking with the collections of Philip
Rashleigh and Joseph Carne as one of the finest in Cornwall. There were
considerable donations in 1893 to institutions including the Natural
History Museum, London, the Camborne School of Mines and the Royal Institution
of Cornwall, but some specimens were retained. These were dispersed
to a number of locations and largely forgotten. Some specimens were
piled five or six high in boxes and at first seemed a lost cause, but
careful curatorial and identification work by Courtenay Smale gradually
revealed many museum-quality specimens including remarkable copper secondaries
from the mines of the Gwennap area, where the Williams family were mine
owners. As well as Cornish material, superb specimens from the Caldbeck
Fells, Leadhills-Wanlockhead, Derbyshire and further afield came to
light. A small selection is figured on the frontispiece.
The gardens at Caerhays are open from 14th February to 5th June between
10 am and 5 pm, but the castle, where the mineral display is housed,
is only open between 14th March and 30th May on weekdays from 12 noon
to 4 pm. A visit is highly recommended. Further details are available
at www.caerhays.co.uk.
Dolyhir Special Edition
As with the last issue, this edition of the UKJMM is given over in
its entirety to a single article. We apologise to authors who have articles
awaiting publication, and hope to produce a second issue of the journal
with more varied content within the year. Dolyhir Quarry is one of the
most important new British discoveries of the last decade, with numerous
rare and unusual minerals, and we believe a full, well illustrated description
is justified!
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A superb old time classic specimen from the
Williams family collection at Caerhays Castle. The largest modified
cubic crystal on the blue fluorite is 35 x 31 x 28 mm. This specimen
is unlabelled but is likely to be from Wheal Gorland, Gwennap,
Cornwall.
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The Mineralogy Of Dolyhir Quarry,
Old Radnor, Powys, Wales
Tom F. Cotterell
David I. Green
Neil Hubbard
John S. Mason
Roy E. Starkey
Andrew G. Tindle
Dolyhir Quarry near Old Radnor in Powys is developed in rocks of the
Old Radnor Inlier, a kilometre-scale fault bounded block that lies within
the Church Stretton Fault Zone. The quarry exposes Silurian algal limestones
of the Dolyhir Limestone Formation, which unconformably overlie Neoproterozoic
clastic sediments of the Yat Wood and Strinds formations. Mineralisation
includes a limestone hosted lead-copper vein containing major primary
tennantite, galena and baryte, with minor greenockite and enargite.
Oxidation of this assemblage has produced supergene minerals including
anglesite, azurite, cerussite, malachite, olivenite and tyrolite and
rare arsentsumebite, gartrellite, otavite, segnitite and zincolivenite.
Supergene enrichment processes have deposited a variety of copper sulphide
minerals in the limestone including chalcopyrite, covellite, djurleite,
roxbyite, spionkopite, yarrowite and probable geerite. Rich azurite
and malachite commonly surround the copper sulphides. Realgar occurs
as disseminations in fractures and joints in black shale of the Yat
Wood Formation and in Silurian conglomerate. Vein hosted barium carbonate
mineralisation comprises alstonite, barytocalcite, paralstonite and
witherite. Fracture assemblages in the basement rocks contain anatase,
baryte, calcite, edingtonite, harmotome, quartz, synchysite-(Ce) and
ewaldite. Ore minerals are uncommon in the basement rocks, they include
chalcopyrite, enargite, galena, luzonite, pyrite, sphalerite, tennantite
and rarely proustite, wurtzite and xanthoconite. The vein assemblage
in the Dolyhir Limestone is probably of the Mississippi Valley Type,
but it is unlike any nearby locality. The realgar deposit is unique
in Britain. The limestone hosted copper mineralisation records complex
supergene enrichment and is unusually species-rich. The barium mineralisation
is also complex and includes unusual paragenetic sequences. The mineralisation
that has developed in fractures in the basement rocks is influenced
by the local lithology and is diverse in comparison to other British
localities. Dolyhir Quarry is the first British locality for ewaldite,
geerite, roxbyite and xanthoconite and the first Welsh locality for
arsentsumebite, gartrellite, luzonite, otavite, paralstonite, proustite,
realgar, segnitite, wurtzite, yarrowite and zincolivenite. These rare
species and complex parageneses make it one of the most important mineralogical
sites in Britain.
57 pages.
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| A grey pyramidal alstonite crystal,
2.6 mm tall, showing striations and re-entrant twinning lines on the
pyramid faces. Photo David Green. |
Hemimorphic pyramidal crystal of
ewaldite, 1.3 mm tall with a large stepped pinacoid termination. Photo
David Green. |
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Beautiful dark red proustite crystal 1.1 mm long from location
15. Neil Hubbard collection, photo David Green.
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A euhedral double terminated prismatic azurite crystal 2 mm long
on partly oxidised sulphide matrix from location 5. Steve Plant
collection, photo David Green.
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Double page spreads from the article
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