Newsletter - March 2012
The full, illustrated newsletter is available as a pdf for download.
Text extracts are given below.
Welcome to the March Newsletter. Before you delve into the contents of the following pages, I would
like to take the opportunity to thank Mary Howie, who stepped down after the February AGM after many
years as the Newsletter Editor for the MGA. Throughout the years she has delivered an excellently
edited newsletter, as I'm sure you'll agree, and she'll definitely be a hard act to follow.
Other changes in the council are the new president Peter del Strother and new vice president Ray
Burgess, as well as myself as new newsletter editor. Peter replaces Tony Adams who stepped down
after another excellent presidential address, this time on "Geology and the Geologist in Crime and
The rehousing of Percy the Plesiosaur after a succesful appeal forms a large part of this edition of the
newsletter, with contributions from David Gelsthorpe, the Curator of Earth Sciences at Manchester
Museum and the MGA's Mary Howie. Also included are two interesting book reviews, and of course the
list of the MGA's outdoor events and a provisional indoor programme for 2012/2013.
Many thanks to all those who have contributed to this edition of the newsletter. Anyone wishing to
contribute to the next edition please email me your articles before 1 June.
Finally, many congratulations to Alex Brierley, who has been awarded this year's MGA GCSE Geology
Prize at Altrincham Grammar School for Boys.
Introducing our new President
I am delighted to have been elected president of the MGA. I should like to
start by thanking Tony Adams for steering our association through a very
successful two years. I should also like to thank Chris Arkwright, who has
recently retired from Council, for her contribution. The MGA would not
function were it not for the unsung contribution of many Council members
over a great number years; thank you, all of you!
My personal background has been in the manufacture of lime and cement. My interest in geology,
which a few years ago turned into a qualification, predates my involvement in the cement industry. In
recent years I have been managing core drilling for investigation of future limestone and clay reserves
for cement manufacture. How lucky for me that what started as a hobby turned into a work activity.
I look forward positively to the programme of lectures and field excursions that has been arranged by
members of MGA council.
Peter del Strother
Introducing our new Vice President
I have been at the University of Manchester since 1992, currently
as a senior lecturer. I'm an isotope geochemist and spend a lot of
my time in the laboratory using mass spectrometers. My interests
range from dating lunar rocks to diamonds, mineral deposits and
understanding chemical cycling of elements in the earth's crust
and mantle. I have recently carried out fieldwork in Iceland,
Azores and Antarctica. I'm looking forward to being part of the
MGA on Facebook
Firstly, thanks to everyone who has renewed their subscriptions this year. Renewals are nearly
complete, but we still have around 20 people who haven't renewed yet. Please ensure that you get
your subscriptions in during the next couple of weeks in order to maintain your membership for 2012.
Many thanks to those members who have switched to receiving their newsletters via email - if anyone
else wishes to change to this format, please contact either myself or James Jepson.
Finally, we've recently set up a Facebook group, which can be found here
here or by going to Facebook and searching for "Manchester Geological Association". Facebook is a site which (amongst other things) allows groups to maintain contact with their members, letting them know about events and updates. We hope to
publicize our events through this group, as well as updating you with articles of geological interest, and
events at other places and societies. You need to have a Facebook sign on to use the site, which can
be set up at Facebook in a couple of minutes. The advantage of this group is that it will allow us to contact you with updates and events in-between newsletter editions.
If the Facebook group is successful, we may look to expanding our reach into Twitter and a blog in
Percy the Plesiosaur
Percy the Plesiosaur, recently described as a new species Hauffiosaurus tomistomimus by Dr Roger Benson and colleagues in 2011 (Palaeontology; 54(3):547-571), has now been rehomed in his new case. Below is an email
of thanks to MGA members for help with the Percy Appeal from Rosemary Broadhurst and Family.
I am writing to thank the MGA for all their help and the very generous donation towards the Percy Appeal. The donation meant the whole project could be completed in a very short time and we are all happy that such a
valuable specimen is now safe again.
We have had really positive feed-back since the opening from many different sources and we will continue to
spread the information about Percy (and the MGA), whenever we can.
With Best Wishes,
Rosemary and Family.
Percy the Plesiosaur has a new case!
On 9 February 2012 The Manchester Museum opened a
fantastic new case housing Percy the Plesiosaur, one of its
most popular fossils. The new case was the culmination of a
fundraising partnership with the family of the late Fred
Broadhurst, who led the team who discovered it. Generous
donations from the Broadhurst family, members of
Manchester Geological Association and other private donors
raised over £28,000.
Percy is one of the most complete plesiosaurs ever
discovered and is of international importance as a type
Unfortunately, the old case was not airtight, which meant
damp air could enter the case putting the specimen at risk of
being destroyed by pyrite decay. The case also had large
heavy glass panels which meant it was almost impossible for
researchers to see the specimen at close quarters.
The new case gave us the opportunity to solve all these
problems and for the first time, tell the inspiring story of the
discovery by Manchester University students. Percy now
delights visitors in the stunning new case, which is
environmentally controlled, ensuring his long term future. The
case provides easy access for researchers and the new
panels describe the discovery of this amazing fossil.
The museum would like to thank all the generous donors and
everyone who was involved in the project.
Curator of Earth science collections, The Manchester Museum
Welcome back, Percy!
Percy has a new home in The Manchester Museum's fossil gallery in a
super, dehumidified case along with a small pal. Many of Fred
Broadhurst's friends, ex-colleagues and former students gathered at the
museum on 9 February to welcome him back.
Over a glass of wine and a nibble or two, Dr John Pollard gave us a
resumé of Percy's discovery and subsequent adventures, and
Rosemary Broadhurst spoke eloquently about Fred, his discoveries and
the fund raising to provide the new case.
Percy was found, by chance, by Fred Broadhurst and his students in
1960 on a winter field trip, between the tides on the Yorkshire coast. The
student who found him, thought that his snout was a belemnite, and
hacked it out of the rock. Closer inspection showed that it was a huge
Plesiosaur. Fred and his students then spent many days, in very
adverse weather conditions excavating Percy from his rocky tomb and
transporting him, still encased in his rocky matrix, pulling him up the
steep and crumbling cliffs.
A few months after that I was in one of Fred's Extra Mural classes, and
well remember the black and white slides of Percy's journey, strapped to
a sledge/stretcher, being dragged up the crumbling cliffs at Ravenscar...
in the February rain and sleet!
Percy came "over the road" from the geology department
in the Williamson Building to The Manchester Museum in
2001, into a glass case, but since then Percy has had a
rather chequered career.
He suffered from "pyrite disease", thought at one time to be
connected with bacterial action, and bits of him were
anointed with Savlon... his head was taken to bits and was
missing for quite some time... being conserved!
At one time it was thought that he would have to be
"disarticulated" and stored in bits in the cellar, along with
other fine specimens. However, Fred Broadhurst's family
and friends were determined that this should not happen,
and thanks to vigorous fund raising by Andy Broadhurst
and others Percy is now installed in his new, dehumidified
(the only way to preserve him) case for all to enjoy - and
yes at floor level so that even the very smallest visitor can
get up close to this amazing sea monster!
This poem about Percy's career was written by Harry Holliday, a museum volunteer for many
Supplied by Mary Howie
There was a fine reptile in the days of yore,
Whose name was Percy the Plesiosaur.
Young Perce was agile and lived in the sea,
He had fish for his dinner and fish for his tea.
His body was sleek, and shaped like a craft,
He carried four paddles, Two fore and Two aft.
Now Perce when young, millions of years ago,
Swam in the sea surf both above and below.
Whilst moving coastwise upon his way,
At Ravenscar Rocks he stopped to play
And he whilst there met, oh what a surprise,
His very last dinner then soon his demise!
Over the years between then and now,
Bone became rock, fossilised that's how.
A few more years he still had to wait,
Before being spotted by Fred and his mate.
For in 1960 whilst doing a hard trip,
His nose was spotted, just near the tip.
All fourteen foot six was dug out with care,
Then back to Manchester to his new lair,
But after some time there was trouble again,
Pyrite decay it was found was to blame.
A bath in Ammonia soon put him right,
A nice dry atmosphere, bones will keep tight.
Now Perce after spending 30 years with us,
Is on the move again, but this creates a fuss.
From Geology to Museum he is now to go,
For a better outlook, and to be on show.
It's hoped he'll get some rest at long last,
Creating interest about his distant past.
"Perce me old lad", said the powers that be,
"You must go to Bristol for your M.O.T.
The lads down south will soon have you fixed,
They just rang to say that the polyfilla's mixed.
So cheer up old son, you're off back to the sea,
Where once you had fish for your dinner and tea."
A message from Bristol said Percy's all done,
His body's all cradled in plastic, my son.
So off Simon went to bring Percy home,
Fixed up a treat to the smallest wee bone.
But was our Perce happy, he wasn't, not he,
He had rather liked Bristol and fish for his tea.
His new home's not ready, but soon he will be
Laid in his glass case, for visitors to see.
His body all sleek, still shaped like a craft,
He lies on the softness of a glass fibre raft.
Children and visitors can gaze in with pride,
He's only one sadness, there's no place to hide.
"Crumbs", thought our Perce, "here's one for the book,
Laid here like a lettuce, whilst all the kids look.
I'm not a bit happy, I'd much rather be,
Back at the seaside with fish for my tea."
"Ungrateful old Percy", said the powers that be,
"You'll lie there and like it for all comers to see.
Providing you're good though, who knows what might be,
You may still get fish for your dinner and tea."
Harry Holliday, 2001
Former Manchester Museum volunteer
Plates vs Plumes: A Geological Controversy by Gillian R. Foulger|
Wiley-Blackwell - 2010
Since the inception of the mantle plume hypothesis in 1971, the advent of new
evidence has precipitated revisions of the hypothesis. In the opinion of Gillian
Foulger, author of 'Plates vs Plumes: a Geological Controversy', these revisions
have rendered the hypothesis unfalsifiable, and as such, it is currently of little
scientific value. This detailed and well argued book presents an alternative theory;
that mantle melting anomalies are driven by established plate tectonic processes.
This review serves as an assessment of the book's utility for teaching, and not a
specific comment on the 'plates vs plumes' debate.
The book begins with an introduction to both theories before dealing with specific topics of interest to
the debate, including chapters on petrology and geochemistry, seismology and volcanology. Each
chapter is concisely introduced to better place the reader within the argument, and ends with a series of
'exercises for the student'. These consist of questions to focus the student's reading of the previous
chapter. While these questions are sometimes a little broad in scope, they support the text and are by
no means unimportant - questions such as 'are "hot spots" hot?' are central to the debate. The text is
abundantly illustrated with schematic figures and well presented graphs in both colour and black and
white, which a geology teacher (or examiner) would find particularly useful.
In order to assess properly this complex debate, it is clearly necessary for the author to address
complex issues. Despite the challenging material, which may be beyond the interest of the non-technical
reader, the author introduces and outlines deftly such technical concepts as are necessary, and the
comprehensive reference list ably directs the interested reader to further material.
In spite of the apparently even handed title, this book unashamedly sets out to banish the plume
model and its proponents to the same fate as those who unwisely argued against Wegener's theory of
Continental Drift over a century ago. In its place, the author presents a new model in which she clearly
has overwhelming confidence. While one admires the conviction required to challenge the established
scientific order, the partiality of the text is a little constricting from time to time. With this said, the book
does introduce readers to topics at the forefront of current research, and provides a valuable insight into
is 'how science works' and the nature of academic debate.
While the author may not convince every sceptical reader to abandon the mantle plumes hypothesis,
and the 'plumes or plates' debate will no doubt rumble on, she has certainly produced here an excellent,
up-to-date synthesis of both arguments. Part detailed text book, part personal crusade for parity, this
book serves not only as a comprehensive (if a little biased) guide through the debate, but also an
excellent introduction to the many aspects of Earth Sciences. The complex and occasionally esoteric
nature of the discussion will find a willing readership amongst teachers, undergraduate university
students, and beyond though the price may put some off. Further references can be found here.
Department Of Earth Science and Engineering, Imperial College, London
Origin of Mountains by Cliff Ollier and Colin Pain|
Routledge - 2000
The Origin of Mountains by Cliff Ollier and Colin Pain is a book to start you
thinking in a new fashion about mountains and how they formed. You may think
it's simple - mountains were formed by folding rocks - but once you have read
this highly innovative book you will understand that such a simple idea can't
explain many of the world's mountains. It's much more complicated and reading
this book may mean you will never look at mountains in the same way again.
The theory that plate tectonics causes mountains to form by folding rocks is a widely held concept
used in many geology books and TV programmes. Ollier and Pain examine this commonly held
perception of folding and try to demonstrate with numerous examples from the field how folds are
unrelated to mountain formation. In most mountains any folding happened many millions of years
before they were formed. In other examples deeply folded layers are found under flat plains. Their
conclusion is that folding is not the cause of mountain formation.
Having dismissed the simple view of folding causing mountains they present the evidence that
mountains follow a standard sequence of formation. Firstly most mountains start as a flat low lying
plain. These are then pushed up to form high level plateaus. Eventually, erosion of the plateaus forms
mountains over millions of years. Many examples of the various stages of this sequence of mountain
formation are given throughout the book from high level plateaus, then plateaus highly eroded at the
edges and finally to a nearly completely formed mountain. Snowdon, the highest mountain in Wales, is
given as an example that shows the final remnants of an old surface at the top and it's something I
intend to examine in more detail on my next visit.
The book seems to contain examples from (what must surely be) virtually every mountain in the
world. These are divided into a number of different chapters. There are also numerous diagrams and
pictures to illustrate the concepts discussed. Most of the ideas and concepts are related to various
scientific papers and there is a comprehensive index if you wish to look at the data in more depth.
Chapter 10 examines a group of mountains that the authors say have been "...generally ignored in
plate tectonic theory...". These are mountains like the Drakenberg, the Eastern Highlands of Australia
and the Appalachians, found on passive continental margins. Once again the authors aren't
disconcerted that these mountains don't fit any grand theory of mountain folding and simply examine
the facts about the mountains. This seems to naturally lead on to the next chapter about drainage from
plains and planation surfaces and what this can tell us.
One of the main points made by the authors is that most of the mountains of the world have been
formed comparatively recently in geological timescales (within the last 5 million years or so) and this
comparatively recent formation once again doesn't fit in with plate tectonics with its much longer
timescale of a hundred million years or so. They also believe they can see periods of quiet tectonic
activity followed by intense periods of world-wide mountain building. But why this should be is still a
Indeed, though the authors make a very strong case for the process of mountain formation they do
not present any firm conviction about the cause of this formation. Why are various sections of land
thrust upwards to form plateaus? The authors give a table of twenty possible causes of tectonic uplift.
For many I fear this would be off-putting but for me it is refreshing to find scientists who are prepared to
say they don't know everything. After all if we knew everything then science would be very boring since
there wouldn't be anything left to discover. As the authors note in the final chapters, the time is ripe for
a renewed interest in the origin of mountains.