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'''Piltdown Man forgery'''
= Geological Survey of England and Wales 1:50,000 map tile: Sheet 13 Bellingham - data sources =
== Timeline ==
== Introduction (From memoir) ==
At a meeting of the Geological Society of London, in December 1912, the fossil remains of what was claimed to be a new type of early human, Eoanthropus dawsoni, or ‘Piltdown Man’, were unveiled to the world.
It appeared that irrefutable evidence had been found at last for the sought-after ‘missing link’ between man and ape.
[[File:P222330.jpg|thumbnail|Crag Lough and Highfield Crags, Roman Wall. ]]
The Bellingham district includes much of the Roman Wall country, the Northumbrian lakes, North Tynedale and Redesdale—all areas of outstanding, unspoilt beauty. They are underlain by Carboniferous rocks, 1600 m thick which were laid down around 300 million years ago. In the south and east, 'Yoredale'; limestones, sandstones and shales with the intrusive dolerite of the Whin Sill form scarp and dip-slope features, but in the forested areas to the north and west thick boulder clay of Pleistocene age mantles most of the solid rock and forms its own distinctive drumlin topography.
This memoir is the first comprehensive published account of the geology of the district. After an introductory chapter, the stratigraphy of the Carboniferous rocks is described in detail, with comprehensive correlation diagrams of sections and boreholes together with complementary palaeontological identifications.
It was not until the 1950s that Piltdown Man was proved to be a forgery.
Accounts of the igneous rocks and structure of the region are followed by chapters on the Pleistocene and economic geology. Appendices list boreholes, shafts, measured sections and geological photographs and conclude with a comprehensive bibliography.
== Contribution and collaboration ==
===Previous research ===
Staff of the [http://www.nhm.ac.uk/ Natural History Museum] (previously the British Museum (Natural History)), the [http://www.geolsoc.org.uk/ Geological Society], and the British Geological Survey (previously H.M. Geological Survey) were all involved with Piltdown — from discovery to unmasking. Some have been implicated in the forgery itself.
For full references see the "[https://webapps.bgs.ac.uk/Memoirs/docs/B01495.html References]"
Archivists at the Natural History Museum, the Geological Society and the British Geological Survey pooled their resources to create a web-based exhibition telling the story of Piltdown Man’s discovery.
Reference to the geology of the district can be found in many early works but the first systematic study was the primary six-inch geological survey by Hugh Miller Jnr., and D. Burns between 1875 and 1878. The solid edition of their one-inch map was published in 1881 followed by the drift edition in 1883. This map was not accompanied by a detailed geological succession nor were any major lithological subdivisions of the Carboniferous shown. A descriptive memoir written by Miller was not published. Small areas on the eastern and western edges of the district were resurveyed by G. A. Burnett (1932–35) and J. B. W. Day, D. H. Land and D. A. C. Mills (1954–58) respectively.
This memoir is the first comprehensive description of the geology of the district (Figure 3), though a number of generalised descriptions have appeared in works which deal with wider regions (e.g. Lebour, 1889; Garwood, 1910; Smith, 1912; Hickling and others, 1931; Taylor and others, 1971). In addition, important contributions to knowledge of the Carboniferous rocks of the district include those by Tate (1867a), Lebour (1873, 1875a, b), Johnson (1959), Fowler (1966) and Frost (1969). Igneous rocks have been studied by Tate (1867a, b, 1870). Topley and Lebour (1877), Teall (1884a, b), Heslop and Smythe (1910), Weyman (1910), Holmes and Harwood (1928, 1929), Smythe (1930), Randall (1959a, b), and Ineson (1972). Mineral deposits have been described by Wilson and others (1922), Smith (1923) and Dunham (1948); and the drift deposits and glacial retreat phenomena by Dwerryhouse (1902) and Smythe (1908, 1912).
Memoirs describing adjacent areas include those by Miller (1887), Clough (1889), Trotter and Hollingworth (1932), Fowler (1936) and Day (1970).
The [https://cdn.knightlab.com/libs/timeline3/latest/embed/index.html?source=1CRfWO3BUSqqhI3tvNEmfEjtNySagoBiR2jPtc05vzGU&font=Default&lang=en&initial_zoom=2&height=650 Piltdown Timeline] reveals the history of the forgery and the identity of individuals that have been accused of complicity or culpability in the affair.
== Maps ==
The Piltdown story provides a cautionary lesson of how scientists can get things wrong and how science, when applied correctly, can reveal error and malpractice.
To view all published sheets for this areas visit the [https://webapps.bgs.ac.uk/data/maps/maps.cfc?method=listResults&MapName=&series=E50k&scale=&pageSize=100 Maps Portal].
== Further reading and detailed bibliography ==
=== Latest published maps for this area ===
If you want to find out more about Piltdown then the following books would be a good place to start:
| Drift sheet - [https://largeimages.bgs.ac.uk/iip/mapsportal.html?id=1001480 View full map] || Solid sheet - [https://largeimages.bgs.ac.uk/iip/mapsportal.html?id=1001481 View full map]
|}
Russell, Miles, ''The Piltdown Man forgery: Case Closed ''(The History Press, 2012)
=== Drift map details ===
{| class="wikitable"
| Map series: || Geological Survey of England and Wales 1:63,360/1:50,000 geological map series, New Series
|-
| Sheet number: || 13
|-
| Sheet title: || Bellingham.
|-
| Map type: || Drift
|-
| Scale: || 1:50 000
|-
| Publication year: || 1980
|-
| Author statement: || Original geological survey on the Six-Inch scale by H. Miller and D. Burns in 1875-1878. Published on the One-Inch scale as Old Series Sheet 106 NE in 1881 (Solid Edition) and 1883 (Drift Edition). Eastern margin resurveyed on the Six-Inch scale by G.A. Burnett in 1932-1935. Mineral Revision by K.C. Dunham in 1939-1945. Western margin resurveyed on the Six-Inch scale by J.B.W. Day, D.H. Land and D.A.C. Mills in 1954-59. W. Anderson, District Geologist. Resurveyed on the Six-Inch scale by D.V. Frost and D.W. Holliday in 1968-1975.
|-
| Published statement: || Published 1980. Print code: 3500/80.
|}
Spencer, Frank, ''The Piltdown Papers ''(Oxford University Press, 1990)
=== Solid map details ===
{| class="wikitable"
| Map series: || Geological Survey of England and Wales 1:63,360/1:50,000 geological map series, New Series
|-
| Sheet number: || 13
|-
| Sheet title: || Bellingham.
|-
| Map type: || Solid
|-
| Scale: || 1:50 000
|-
| Publication year: || 1980
|-
| Author statement: || Original geological survey on the Six-Inch scale by H. Miller and D. Burns in 1875-1878. Published on the One-Inch scale as Old Series Sheet 106 NE in 1881 (Solid Edition) and 1883 (Drift Edition). Eastern margin resurveyed on the Six-Inch scale by G.A. Burnett in 1932-1935. Mineral Revision by K.C. Dunham in 1939-1945. Western margin resurveyed on the Six-Inch scale by J.B.W. Day, D.H. Land and D.A.C. Mills in 1954-59. W. Anderson, District Geologist. Resurveyed on the Six-Inch scale by D.V. Frost and D.W. Holliday in 1968-1975.
|-
| Published statement: || Published 1980. Print code: 3500/80.
|}
Walsh, John, ''Unravelling Piltdown: The Science Fraud of the Century and Its Solution ''(Random House, 1996)
=== Six-inch maps ===
The following is a list of six-inch geological maps included in the area of 1:50000 Geological Sheet 13 with the date of survey for each map. The surveying officers are: G. A. Burnett, J. B. W. Day, D. V. Frost, D. W. Holliday, D. H. Land and D. A. C. Mills. Copies of the maps are deposited for public reference in the libraries of the London and Leeds Offices of the Institute of Geological Sciences. Uncoloured dyeline copies of those marked by an asterisk are available for purchase. Xerox copies of the remaining partially surveyed sheets are also available.
Weiner, J S, ''The Piltdown Forgery ''(Fiftieth Anniversary edition, with a new Introduction and Afterword by Chris Stringer, Oxford University Press, 2003)
[[File:BellinghamIndexto10kmaps.JPG|600px|Index to National Grid six-inch geological maps]]
For a more detailed study of the whole Piltdown story, BGS Historian David G Bate has compiled a large [https://nora.nerc.ac.uk/507543/ annotated bibliography].
| NY 77 NE* Blackaburn and Stonehaugh || Frost || 1972–73
|-
| NY 78.SW* Chirdon Burn || Holliday || 1973–74
|-
| NY 78 NW Falstone || Holliday || 1973
|-
| NY 78 NE Greenhaugh || Holliday || 1973
|-
| NY 86 NW Grindon Hill || Frost and Holliday || 1968
|-
| NY 86 NE Newbrough and Fourstones || Holliday || 1968
|-
| NY 87 SW* Sewingshields || Frost || 1968
|-
| NY 87 SE* Simonburn || Frost and Holliday || 1968–69
|-
| NY 87 NW* Warksburn || Frost || 1971
|-
| NY 87 NE* Birtley and Wark || Frost || 1970
|-
| NY 88 SW* Bellingham || Frost || 1972–73
|-
| NY 88 SE* Redesmouth || Frost || 1972
|-
| NY 88 NW Hareshaw || Frost || 1973
|-
| NY 88 NE West Woodburn || Frost || 1973
|-
| NY 96 NW Wall || Holliday || 1971
|-
|-
| style="vertical-align:top;" | 1859
| NY 96 NE Stagshaw || Burnett and Holliday || 1935, 1971
| style="vertical-align:top;" | Paving the way to Piltdown
| style="vertical-align:top;" | In 1859 Charles Darwin published ''On the Origin of Species''. One of the implications of this work, which he later developed in The ''Descent of Man'' (1871), was that human beings were descended from an ‘ape-like progenitor’. If true, there should be some evidence in the fossil record to support such an argument. The search for the ‘missing link’, an ape-man, had begun.
| style="vertical-align:top;" | Insert Image if available
|-
|-
| style="vertical-align:top;" | 1863
| NY 97 SW* Barrasford || Holliday || 1971
| style="vertical-align:top;" | Neanderthal Man (H. neanderthalensis)
| style="vertical-align:top;" | Fossil remains of ancient man had been found in Belgium (1829) and Gibraltar (1848), but had been either misinterpreted or ignored. In 1856 a human skullcap and partial skeleton of peculiar form were recovered from a cave in the Neander Valley (Neanderthal), near Düsseldorf. Thought to represent ‘a barbarous and savage race’, the remains were recognised in 1863 as a distinct species, Homo neanderthalensis. By the end of the 19th century many more examples of ‘Neanderthal Man’ had been discovered. It was clear however that despite the somewhat bestial appearance Neanderthal Man was anatomically only slightly removed from modern humans (Homo sapiens) and was not the ‘missing link’.
| style="vertical-align:top;" | Insert Image if available
|-
|-
| style="vertical-align:top;" | 1891
| NY 97 SE* Bingfield || Burnett and Holliday || 1934–35,1968,1971
| style="vertical-align:top;" | Java Man (Homo erectus)
| style="vertical-align:top;" | In 1891 Eugène Dubois found an ape-like skullcap, a human-looking thighbone and two molar teeth on the banks of the Solo River in eastern Java. He named his discovery Pithecanthropus erectus, meaning ‘upright ape-man’, believing it to be the ‘missing link’. Yet doubts were soon expressed concerning the geological age and mutual relations of the finds. Some scientists considered the skullcap to belong to a giant gibbon! It would be some 40 years before further discoveries in China and Java would confirm Java Man as an early primitive human, now reclassified as Homo erectus.
| style="vertical-align:top;" | Insert Image if available
|-
|-
| style="vertical-align:top;" | 1907
| NY 97 NW* Gunnerton || Frost || 1971
| style="vertical-align:top;" | Heidelberg Man (Homo heidelbergensis)
| style="vertical-align:top;" | In 1907 Daniel Hartmann discovered a fossil human jaw in a sandpit at Mauer in south-west Germany. The jaw was passed to Dr Otto Schoetensack of the University of Heidelberg who named it Homo heidelbergensis after the university. There was no doubt that the jaw, which lacked a modern chin, belonged to a primitive human far older than Neanderthal Man. The discovery of the Heidelberg jaw was received with great interest in England and Charles Dawson, a noted amateur archaeologist and geologist, set out to find England’s answer to Heidelberg Man. The stage was set for Piltdown Man to make his debut.
| style="vertical-align:top;" |
|-
|-
| style="vertical-align:top;" | 1908
| NY 97 NE* Hallington || Burnett and Holliday || 1932–34,1971–73
| style="vertical-align:top;" | The Piltdown Discovery
| style="vertical-align:top;" | Charles Dawson was steward of Barkham Manor, near Piltdown, and it was while attending a manorial court that he noticed workmen digging gravel for road-mending beside the driveway to the house. The gravel was not shown on the Geological Survey map of the time, and the deposit appeared to be the remnant of an old river-bed. He asked the workmen to keep a look out for any interesting fossils, and it was during one of his periodic visits, in about 1908, that the first Piltdown skull fragment was handed to him. According to Dawson, it was not until the autumn of 1911 that further fragments of the skull were recovered.
| style="vertical-align:top;" |
|-
|-
| style="vertical-align:top;" | February 14, 1912
| NY 98 SW* Ridsdale || Frost || 1972–73
| style="vertical-align:top;" | How’s that for Heidelberg?
| style="vertical-align:top;" | On 14 February 1912 Dawson wrote to the Keeper of Geology at the Natural History Museum, Arthur Smith Woodward, and mentioned a portion of a human skull that he had found in a gravel pit at Barkham Manor, near Piltdown in Sussex. Dawson said that it would ‘rival ''H. heidelbergensis'' in solidity.’ On 24 May 1912, Woodward received the Piltdown finds from Dawson‘s hands with the words ‘How’s that for Heidelberg?’
| style="vertical-align:top;" |
|-
|-
| style="vertical-align:top;" | June, 1912
| NY 98 SE* Great Bavington || Burnett and Holliday || 1932–33,1972–73
| style="vertical-align:top;" | Further Discoveries
| style="vertical-align:top;" | On 2 June, Smith Woodward, Dawson and Pierre Teilhard de Chardin, a French Jesuit priest and avid fossil collector, arrived at Barkham Manor to begin excavation of the gravel. They were assisted by a labourer, probably ‘Venus’ Hargreaves. Dawson discovered another fragment of the skull, while Teilhard de Chardin found a flint implement and part of a molar tooth of a primitive elephant identified at the time as ''Stegodon''.
| style="vertical-align:top;" | Dawson and Smith Woodward continued digging through June, July and August (Teilhard returned to France in early July). Three further skull fragments were discovered and more significantly a portion of an ape-like lower jaw. During the remainder of the season further flint implements, teeth of beaver, a mastodon (an extinct relative of the elephant) and a horse, along with a fragment of red deer antler were recovered.
| style="vertical-align:top;" |
|-
|-
| style="vertical-align:top;" | November 21, 1912
| NY 98 NE Raechester || Burnett and Holliday || 1933, 1973
|}
== Memoir ==
'''Geology of the country around Bellingham. Memoir for 1:50 000 geological sheet 13 by D.V. Frost and D.W. Holliday'''
| style="vertical-align:top;" | The Earliest Man?
Bibliographical reference: Frost, D.V. and Holliday, D.W. 1980. Geology of the country around Bellingham. Mem. Geol. Surv. G.B., Sheet 13, 112 pp.
| style="vertical-align:top;" | Rumours of the discovery were beginning to circulate widely and on 21 November 1912 the Manchester Guardian ran a story headed ‘The earliest man? Remarkable discovery in Sussex: a skull millions of years old’. The paper boldly asserted that ‘there seems to be no doubt whatever of its genuineness, and more than a possibility of its being the oldest remnant of a human frame yet discovered on this planet’.
| style="vertical-align:top;" | The Unveiling of Dawson’s Dawn Man
[https://pubs.bgs.ac.uk/publications.html?pubID=B01495 View original printed memoir]
| style="vertical-align:top;" | The official unveiling of the Piltdown finds took place on 18 December at a meeting ofthe Geological Society of London, in Burlington House, before a packed and expectantaudience. Dawson began by describing the geology of the Piltdown site and the circumstances of the discovery. He concluded that the human and associated finds were of early Pleistocene date (over 2 million years old). Smith Woodward then described the human (and animal) bones in some detail. The cranium, though exceptionally thick, resembled that of a modern human; yet the ape-like jaw made it necessary to regard the Piltdown find as a new type of hominid, which he named ''Eoanthropus dawsoni'' (Dawson’s Dawn Man).
| style="vertical-align:top;" |
|-
| style="vertical-align:top;" | December 18, 1912
| style="vertical-align:top;" | First Restoration of the Piltdown Skull
| style="vertical-align:top;" | Grafton Elliot Smith, Professor of Anatomy at the University of Manchester, to whom Smith Woodward had submitted a cranial cast for detailed examination, considered Piltdown man to possess ‘the most primitive and most simian [i.e. ape-like] human brain so far recorded.’ Displayed at the meeting was a plaster replica of Woodward’s conjectural restoration of the Piltdown skull, which had been prepared by Frank Barlow, a senior preparator at the Natural History Museum.
| style="vertical-align:top;" |
|-
| style="vertical-align:top;" | December 18, 1912
| style="vertical-align:top;" | By Far the Most Important Discovery Ever Made in England
| style="vertical-align:top;" | In the discussion that followed, Arthur Keith stated that the discovery of these human remains were ‘by far the most important ever made in England, and of equal, if not of greater consequence than any other discovery yet made, either at home or abroad’. On the other hand David Waterston, an anatomist at King’s College London, believed the jaw to be in all respects identical to that of a chimpanzee, and thus incompatible with the essentially human cranium.
| style="vertical-align:top;" |
|-
| style="vertical-align:top;" | 1913
| style="vertical-align:top;" | Canine Tooth
| style="vertical-align:top;" | The most significant find in the summer of 1913 was made by Teilhard de Chardin, who had returned to England in early August. On 30 August, Dawson, Smith Woodward and Teilhard de Chardin were making an intensive search for the missing teeth of the lower jaw when Teilhard de Chardin found an ape-like canine tooth, which proved to be of crucial importance in supporting Woodward’s conjectural restoration of ''Eoanthropus''.
| style="vertical-align:top;" |
|-
| style="vertical-align:top;" | July 3, 1913
| style="vertical-align:top;" | Discovery at Barcombe Mills
| style="vertical-align:top;" | In a letter to Smith Woodward, dated 3 July 1913, Dawson claimed to have ‘picked up the frontal part of a human skull this evening on a ploughed field covered with flint gravel’. He would only say that the location was a long way from Piltdown, but he thought that the skull, although not thick, might be a descendant of ''Eoanthropus''. The unnamed location is believed to be a hill above Barcombe Mills railway station, about six kilometres south of Barkham Manor. Nothing more would be heard of this ‘find’ until 1949!
| style="vertical-align:top;" |
|-
| style="vertical-align:top;" | 1914
| style="vertical-align:top;" | Anyone for Cricket?
| style="vertical-align:top;" | The 1914 season of excavations at Barkham Manor yielded no further human remains, but did result in one sensational discovery. Woodward had been watching a workman (probably Venus Hargreaves), who was using a pick, when he saw some splinters of bone scattered by a blow. He stopped the workman and soon uncovered a heavy blade of bone that had been carved and ‘looked rather like the end of a cricket-bat’. Dawson then succeeded in recovering another portion of the club-like implement.
| style="vertical-align:top;" |
|-
| style="vertical-align:top;" | June, 1914
| style="vertical-align:top;" | A Unique Discovery!
| style="vertical-align:top;" | It was clear that this strange implement had been carved out of theleg bone of an elephant. Nothing quitelike it had ever been found before. Its context, however, was a little curious, for it was discovered beneath the hedge which bounds the gravel pit at about a foot below the surface in dark vegetable soil. The pale-yellow clay adhering firmly to its surface indicated that it h ad come from the bottom of the gravel and must have been thrown against the hedge by one of the workmen; ‘with the other useless debris when they were digging gravel from the adjacent hole,’ as Dawson put it.
| style="vertical-align:top;" |
|-
| style="vertical-align:top;" | January 9, 1915
= BGS175: 175th Anniversary Science Symposium of the founding of the British Geological Survey, 28th September, Royal Institution, London =
| style="vertical-align:top;" | Dawson the ‘Wizard’ Produces ‘Piltdown II’
The British Geological Survey is the world's oldest national geological survey and commemorated its 175th anniversary in 2010.
| style="vertical-align:top;" | On 9 January 1915,Dawson wrote to Smith Woodward; ‘I believe weare in luck again! I have got a fragment of the left side of a frontal bone with portion of the orbit and root of nose... the general thickness seems to me to correspond to the right parietal of ''Eoanthropus''’.Dawson omitted to mention the location of his find, noting only that it came from a ploughed field (Smith Woodward appears however to have been aware of the general location).
| style="vertical-align:top;" |
|-
| style="vertical-align:top;" | July 30, 1915
The event was marked by a one-day science symposium on 28 September 2010.
The symposium showcased our world-class science and technologies, demonstrating their relevance, societal benefits and positive impacts in addressing 21st century challenges; including living with environmental change, energy and natural resource security, rising CO<sub>2</sub> emissions and geohazards.
| style="vertical-align:top;" | On 30 July 1915, Dawson wrote again to say that he had discovered a molar tooth of ''Eoanthropus ''from the same new locality. Shortly afterwards it appears that an unnamed friend found ‘part of the lower molar of an indeterminable species of rhinoceros, as highly mineralized as the specimens previously found at Piltdown itself’, as Smith Woodward later recounted. Yet the exact location of what came to be called Piltdown II (the Barcombe Mills material having been discounted) was never fully revealed to Smith Woodward, although he understood it to be at Netherhall Farm, between Sheffield Park and Fletching, about two kilometres north- west of Barkham Manor.
| style="vertical-align:top;" |
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| style="vertical-align:top;" | August 10, 1916
* Peak metal: Scarcity of supply or scare story?
* Bronze Age Mediterraneans may have visited Stonehenge
* Modelling of Icelandic volcanic ash particles
| style="vertical-align:top;" | Charles Dawson, 1864-1916
The event was attended by influential stakeholders including representatives from government, industry, academia, international geological surveys, students and the national media.
| style="vertical-align:top;" | On 10 August 1916, Charles Dawson died of septicaemia. He was 52 years of age.
| style="vertical-align:top;" |
|-
| style="vertical-align:top;" | 1917
| style="vertical-align:top;" | Woodward Announces Piltdown II
| style="vertical-align:top;" | Piltdown II (usually referred to as the Sheffield Park find) was revealed to the world at a Geological Society of London meeting on 28 February 1917. The existence of a second ''Eoanthropus ''consisting of ape- like molar associated with thick human skull fragments, all stained dark brown, provided conclusive evidence of the integrity of Piltdown I. It was enough to silence many of the critics.
| style="vertical-align:top;" |
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| style="vertical-align:top;" | 1917–1952
Guest speakers included Dr Marcia McNutt, and [https://www.plymouth.ac.uk/staff/iain-stewart Professor Iain Stewart].
| style="vertical-align:top;" | A Chapter Closes
Britain's best-known natural history film-maker, [https://en.wikipedia.org/wiki/David_Attenborough Sir David Attenborough], featured in the panel discussion to close the symposium.
| style="vertical-align:top;" | After Charles Dawson‘s death in 1916 there were no more finds at Piltdown. Smith Woodward continued to make regular visits to Barkham Manor and carried out further excavations, helped at times by Grafton Elliot Smith among others. Shortly after his retirement from the Natural History Museum he moved to Hayward‘s Heath in Sussex, from which he could more readily make visits to the site. Yet despite years of searching, the Piltdown gravels stubbornly refused to yield anything of significance.
| style="vertical-align:top;" |
|-
| style="vertical-align:top;" | 1920–1935</span>
About the British Geological Survey, 2010.
| style="vertical-align:top;" | New Finds from Asia
== Win a place at BGS175 ==
| style="vertical-align:top;" | During the 1920s and 1930s important finds of early hominids began to emerge from Africa and Asia. The discovery in China of ‘Peking Man’ (''Sinanthropus pekinensis''), along with further finds from Java, led anthropologists to recognise the validity of Dubois’ Java Man. Indeed, the essential similarities between these two hominids subsequently led to both being reclassified under ''Homo erectus''. Both Smith Woodward and Elliot Smith believed that the new finds supported their interpretation of ''Eoanthropus''. Smith Woodward suggested in 1935 that ''Sinanthropus'' and ''Eathropus'' had perhaps coexisted as eastern and western varieties of Dawn Man. Not everyone agreed however.
| style="vertical-align:top;" |
|-
| style="vertical-align:top;" | 1935–1936
The winners of a VIP day at the science symposium, featuring Sir David Attenborough, are listed in the table below.
| style="vertical-align:top;" | Swanscombe
{| class="wikitable"
| style="vertical-align:top;" | The status of Piltdown Man was also brought into question with the discoveries in 1935 and 1936 of early human cranial remains in association with stone tools at Swanscombe in north- west Kent. The discoveries were made by Alvan T. Marston, a London dentist, who had for two years past been searching the old ‘100 foot terrace’ deposits of the River Thames for Palaeolithic flint implements and fossil mammals. Arthur Keith professed the Swanscombe fragments to be those of early modern man (''Homo sapiens''), while Elliot Smith judged the new skull to be more primitive than Piltdown. The Swanscombe individual, who was probably a young woman, is now considered to be of Neanderthal affinity (''Homo neanderthalensis'').
| Jonathan Wyatt, SHROPSHIRE || Paul Colinese, LONDON
| style="vertical-align:top;" |
|-
|-
| style="vertical-align:top;" | 1936
| John Williams, SURREY || Sophie Hibben, KENT
| style="vertical-align:top;" | Piltdown Further Undermined
| style="vertical-align:top;" | There was another more serious problem raised by the Swanscombe finds. In 1925 Francis H. Edmunds of the Geological Survey was sent out to map the terrace deposits around Piltdown that had been omitted from earlier editions of the official geological map of the area. Edmunds was able to demonstrate that the Piltdown gravel closely correlated with the Thames ‘50-foot terrace’ and is thus younger than the Swanscombe terrace deposits. It appeared therefore that an ape- like ''Eoanthropus ''had coexisted with modern man! Clearly something was amiss. Alvan Marston became convinced that the ape-like Piltdown jaw could not possibly have belonged with the essentially human Piltdown cranium, but must be a chance association.
| style="vertical-align:top;" |
|-
|-
| style="vertical-align:top;" | 1938
| Lisa Allan, LONDON || Rob Flanders, CHESHIRE
| style="vertical-align:top;" | A Memorial to Piltdown
| style="vertical-align:top;" | Early in the 1920s a wooden memorial was erected on the site where the first ''Eoanthropus dawsoni ''had been found, and in 1938 Smith Woodward arranged for this to be replaced by a more permanent sandstone monolith. It was unveiled by Arthur Keith on 23 July 1938 and carries the following inscription: ‘Here in the old river gravel, Mr Charles Dawson, FSA, found the fossil skull of Piltdown Man 1912–1913. The discovery was described by Mr Charles Dawson and Sir Arthur Smith Woodward in the Quarterly Journal of the Geological Society 1913–15.’
| style="vertical-align:top;" |
|-
|-
| style="vertical-align:top;" | 1949
| Vince Piper, BUCKINGHAMSHIRE || Steven Cadman, SURREY
| style="vertical-align:top;" | Fluorine Testing
| style="vertical-align:top;" | In 1949 Kenneth P. Oakley of the Natural History Museum used a fluorine test to determine whether the Piltdown jaw and cranium were contemporaneous. Fossil bones and teeth accumulate fluorine over the course of time by absorption from circulating groundwater. By analysing the amount of fluorine contained in a sample of material it is possible to determine the relative ages of fossils. The test had already been used successfully on the Swanscombe finds. The Piltdown jaw and skull fragments yielded similar values of fluorine values and thus appeared to be contemporaneous. However, these values were much lower than those obtained from the Swanscombe individual, implying that Piltdown Man was of more recent geological age than originally thought.
| style="vertical-align:top;" |
|-
|-
| style="vertical-align:top;" | 1949
| Sahja Haji, LONDON || Litsa Breingan, LONDON
| style="vertical-align:top;" | Piltdown IIII
| style="vertical-align:top;" | In the spring of 1949 Dr Robert Broom, a South African palaeontologist, visited the Natural History Museum in order to re-examine the remains of the two skulls attributed to Piltdown Man. He found that the Museum possessed parts of a third fossil skull together with a molar tooth found by Charles Dawson in July 1913 near Barcombe Mills. Smith Woodward had evidently attached no importance to this find and only acquired it after Dawson’s death. Broom published a short notice, though he gave no detailed assessment of this previously unremarked material, but in a handwritten report submitted to the Natural History Museum he concluded that the remains probably represented a third individual of ''Eoanthropus dawsoni''.
| style="vertical-align:top;" |
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| style="vertical-align:top;" | December 3, 1951 — 12:00:00 am May 19, 1952
| Paul Dotteridge, HERTFORDSHIRE || Stephen Metheringham, BUCKINGHAMSHIRE
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| Milo Brook, OXFORDSHIRE || Catherine Unsworth, LONDON
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== About the day ==
| style="vertical-align:top;" | Britain’s First Geological National Nature Reserve
===Symposium agenda===
| style="vertical-align:top;" | The National Parks and Access to the Countryside Act of 1949 saw the creation of agovernment body, the Nature Conservancy, a forerunner of Natural England. Its aim was to identify and protect Britain’s most important fauna, flora, geological and physiographical features. The PiltdownSkull Site at Barkham Manor was one of the first sites to be considered for acquisition and listingas a National Nature Reserve (NNR). The site was acquired by the Nature Conservancy on 3 December 1951, and formally declared a NNR on 19 May 1952. Although just beaten in the race to become the nation’s first NNR by a site in Scotland, Piltdown would soon earn notoriety as the first NNR to be revoked!
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Download the oral programme 200 KB pdf
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| style="vertical-align:top;" | 1953
| style="vertical-align:top;" | Doubts About Authenticity
| style="vertical-align:top;" | In 1953 Joseph S. Weiner, Professor of Physical Anthropology at Oxford University, was able to examine the original Piltdown remains. He had developed doubts about their authenticity and the more he looked at them the more the doubts grew. Weiner discovered that the Natural History Museum had no record of the exact spot where the remains of Piltdown II had been found. These location details had been used to support the authenticity of the original Piltdown finds; this lack of provenance was of great importance.
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| style="vertical-align:top;" | 1953
| style="vertical-align:top;" | A Forgery Uncovered
| style="vertical-align:top;" | Weiner became convinced that the teeth in the jaw had been filed down and thisindicated deliberate fraud. He obtained some chimpanzee teeth which he filed down and stained artificially in order to replicate the Piltdown molars. After discussing it with Wilfrid Le Gros Clark, Professor of Anatomy at Oxford, it was decided to contact Kenneth Oakley at the Natural History Museum and inform him about theirsuspicions. Oakley checkedthe teeth and was ‘utterly convinced’ that they had been artificially abraded. Further examination revealed that the canine tooth had been stained using a mixture which included Vandyke brown paint.
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| style="vertical-align:top;" | November 21, 1953
===Keynote speakers and special guests===
| style="vertical-align:top;" | ‘The Biggest Scientific Hoax of the Century’
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| style="vertical-align:top;" | An announcement of the scientific team’s startling revelations appeared in The Times of 21 November 1953 under the headline ‘Elaborate Hoax’, and was quickly picked up by the popular press. A London evening newspaper, The Star, presented the story as ‘The Biggest Scientific Hoax of the Century’. No attempt was made at this stage to identify the perpetrator, but newspaper reports quickly homed in on Charles Dawson.
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| style="vertical-align:top;" | November 21, 1953–November 28, 1953
|'''Video presentation''': [https://www.youtube.com/watch?v=8NstzDgR4fE About the British Geological Survey - 175 years of geoscience]||
| style="vertical-align:top;" | Arthur Keith Accepts the Truth
| style="vertical-align:top;" | On the day of the press release, Oakley and Weiner visited Arthur Keith, who was now well into his eighties. On being appraised oftheir findings, Keith replied ‘You may be right, Weiner, and I must accept it, but it willtake me a little while to adjust to it.’ On 28 November Pierre Teilhard de Chardin wroteto Oakley from New York congratulating himon his solution of the Piltdown problem:‘Anatomically speaking, “''Eoanthropus''” was a kind of monster... Therefore I am fundamentally pleased by your conclusions,in spite of the fact that, sentimentally speaking,it spoils one of my brightest and earliest palaeontological memories.’
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| style="vertical-align:top;" | 1954–1955
|Sir David Attenborough wrote and narrated BBC's [https://www.youtube.com/watch?v=snuna3fLYAg Uncovering Our Earliest Ancestor] ||[[File:Attenborough Thumb Copyright IanSalvage.jpg]]
| style="vertical-align:top;" | Confirmation of the Fraud
| style="vertical-align:top;" | Over a period of several months the Piltdown remains were subjected to further tests. A full presentation of the scientific results was made at a meeting of the Geological Society on 30June 1954. The Piltdown jaw and canine were confirmed as being from a modern ape,probably a young female orang-utan. The exceptionalthickness of the skull(essentially that of a modernhuman) might be explainedas a pathological condition,although such thickened craniaare met with in some modern populations.
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| style="vertical-align:top;" | June 30, 1954
|Marcia McNutt, USGS Director, [https://www.youtube.com/watch?v=ISzUlINbB4o Introduction to The National Map]||[[File:Mcnutt USGS.jpg]]
| style="vertical-align:top;" | Foreign Source for Mammalian Fossils
| style="vertical-align:top;" | The mammalian fossil bones and teeth were found to have been derived from a variety of sources. A comparative analysis of the radioactivity of the bones and teeth from Piltdown and elsewhere (undertaken by S. H. U. Bowie and C. F. Davidson of the Geological Survey Atomic Energy Division) demonstrated that some of the material must have been obtained from a foreign source. Thus, it was determined that the ''Stegodon ''teeth had most likely come from a site in Tunisia, while one of the hippopotamus teeth closely matched examples from Malta. All of this material had been artificially stained.
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| style="vertical-align:top;" | June 30, 1954
|Professor Iain Stewart in the BBC's [https://www.youtube.com/watch?v=kphF71S5F0Q How Earth Made Us]. Iain tells the epic story of how the planet has shaped our history.||[[File:Stewart plymouth.jpg]]
| style="vertical-align:top;" | Cricket Bat Carved with Metal Blade
| style="vertical-align:top;" | The ‘cricket bat’ had been carved using a metal blade and after it had been already fossilised. The newly cut surfaces had been stained with an iron solution and then varnished to reproduce, as nearly as possible, the appearance of the remainder of the roughly fashioned bone.
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| style="vertical-align:top;" | 1955
| style="vertical-align:top;" | ‘Further Contributions to the Solution of the Piltdown Problem’
| style="vertical-align:top;" | All of the new evidence was presented in a concluding report from the Natural History Museum entitled ‘''Further Contributions to the Solution of the Piltdown Problem”'', issued 21 January 1955. The report concluded that ‘Not one of the Piltdown finds genuinely came from Piltdown.’ Within months of these latest revelations the last surviving principal protagonists in the Piltdown affair were dead. Arthur Keith died on 7 January, followed by Pierre Teilhard de Chardin on 10 April.
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== Presentations ==
== ‘A Most Elaborate and Carefully Prepared Hoax’ ==
Insert Video: Panel session
Those who had believed in the authenticity of Piltdown Man had been victims of ‘''a most elaborate and carefully prepared hoax’.''; The question remained: who had carried out such an audacious fraud?
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|'''Morning session A'''||
Presented here in the order in which they were publicly identified, are: Charles Dawson, Pierre Teilhard de Chardin, W. R. Butterfield, Venus Hargreaves, Grafton Elliot Smith, William J. Sollas, Martin Hinton, Arthur Conan Doyle, Samuel Woodhead, John T. Hewitt, Lewis Abbott, Frank Barlow, Arthur Keith, Chipper the goose (in jest!), Arthur Smith Woodward, and C. P. Chatwin.
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| Opening address || John Ludden, Executive Director, BGS
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| [https://www.youtube.com/watch?v=8NstzDgR4fE About the BGS - 175 years of geoscience]||
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| Twenty-first century survey || Denis Peach, Chief Scientist, BGS
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| Acuity, accuracy and application: from systematic geological mapping to responsive 3D+ surveys || Martin Smith, Head Geology & Landscape, BGS
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| From watercolour to web || Keith Westhead, Head Knowledge Exchange, BGS
| OneGeology: improving access to geoscience globally || Ian Jackson, Chief of Operations, BGS
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| North American liaisons || Garth Earls, Director, GSNI
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| style="vertical-align:top;" | 1955
| Arabian adventures: geological mapping and climate change in Arabia || Andrew Farrant, Geologist, BGS
| style="vertical-align:top;" | Charles Dawson (1864-1916)
| style="vertical-align:top;" | Dawson was a solicitor at Uckfield in Sussex, and a noted antiquarian and amateur geologist, being made a Fellow of the Geological Society of London in 1885 and of the Society of Antiquaries in 1895. He made many donations of Wealden fossils to the Natural History Museum. Dawson was ambitious for recognition and fame and fully expected the Piltdown discoveries to secure him fellowship of the Royal Society, an aspiration that was ultimately denied him. When the fraud was exposed in 1953, Dawson became an obvious suspect. He had been the motivating force behind the excavations and was always present when finds were made. After he died from septicaemia in 1916 there were no further discoveries. Since 1953 many of Dawson’s antiquarian ‘discoveries’ have been shown to be either fraudulent or suspect.
| style="vertical-align:top;" | Insert Image here
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| style="vertical-align:top;" | 1955
| Groundwater animals: extending our understanding of biodiversity in the UK || Louise Maurice, Groundwater ecologist, BGS
| style="vertical-align:top;" | Pierre Teilhard de Chardin (1881–1955)
| style="vertical-align:top;" | Teilhard de Chardin was a French philosopher and Jesuit priest who trained as a palaeontologist. He was studying at Hastings when he first met Dawson in 1909. Dawson invited him to the excavation at Piltdown in 1912, and in 1913 Teilhard discovered the canine tooth. He was still alive when the hoax was uncovered, but when questioned was reluctant to talk about it, which in 1954 aroused suspicion in the minds of the investigators. Those who have implicated Teilhard include Louis Leakey and Stephen Jay Gould, both of whom believed it possible that he had worked in collusion with Dawson. Leakey had no clear evidence to back up his suspicion, while Gould’s accusation was based on incomplete information. More recently the case against Teilhard has been revived by Francis Thackeray, who believes that Teilhard perpetrated a prank that went too far.
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| style="vertical-align:top;" | 1972
| Life just got complicated || Dr Phil Wilby, Geologist, BGS
| style="vertical-align:top;" | William Ruskin Butterfield (1872–1935)
| style="vertical-align:top;" | Butterfield was curator and librarian of Hastings Museum during the period of the Piltdown discoveries. In 1972 Guy van Esbroeck, in his book Pleine lumière sur l’imposture de Piltdown, accused Butterworth of being the Piltdown forger in collusion with Venus Hargreaves, the labourer employed at Barkham Manor. His argument is that Butterworth was greatly put out on learning through a chance remark from Teilhard de Chardin, in 1909, that Dawson had quietly appropriated a series of bones of the dinosaur Iguanodon from a Hastings quarry and presented them to the Natural History Museum at South Kensington. It is claimed that he carried out the ‘hoax’ in revenge. This theory seems to ignore the fact that Dawson had already made his first find at Piltdown probably in the previous year.
| style="vertical-align:top;" | Hargreaves was the labourer who did most of the digging at Piltdown. Apart from van Esbroeck’s assertion that Hargreaves assisted Butterfield by planting the fraudulent Piltdown assemblage (previous slide), Francis Vere had earlier intimated in his book The Piltdown Fantasy (1955) that the forger required an accomplice who worked at the site, by which he presumably meant Hargreaves.
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| style="vertical-align:top;" | 1972
| Predict or prepare: natural hazards and human disasters || David Kerridge, Head Earth Hazards & Systems, BGS
| style="vertical-align:top;" | Grafton Elliot Smith (1871-1937)
| style="vertical-align:top;" | Elliot Smith, born at Grafton in Australia, was Professor of Anatomy at University of Manchester, 1909–19, and University College London, 1919–37, and had a special interest in the anatomy of the human brain. In The Piltdown Men (1972) Ronald Millar accused Smith of perpetrating the forgery in order to provide support for his views on human evolution. The case made against him is convoluted and entirely circumstantial. Millar regards it as suspicious that Smith allowed Woodward to reconstruct the Piltdown skull incorrectly, as Smith was an expert on prehistoric human skulls. One is prompted to ask why, if implicated in the fraud, did Smith assist Woodward in his continuing attempts to look for further evidence at Piltdown long after Dawson’s death? Kenneth Oakley (in a private communication to Charles Blinderman) regarded Millar’s accusation as ‘absurd’, a view shared by many others.
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| style="vertical-align:top;" | 1978
| Groundwater, health and livelihoods in Africa || Alan MacDonald, Hydrogeologist, BGS
| style="vertical-align:top;" | William Johnson Sollas (1849-1936)
| style="vertical-align:top;" | Sollas was Professor of Geology at Oxford. In 1978 he was accused of complicity in the Piltdown forgery by his former assistant at the university, Prof. J. A. Douglas (died 1978). Douglas was convinced that Sollas had directed the hoax through Dawson in order to revenge himself on Smith Woodward, who he regarded as a bitter enemy. Douglas’s evidence consisted of nothing more than his memory of the arrival of a package for Sollas containing potassium ‘bichromate’, and of Sollas borrowing apes’ teeth from the university’s Department of Human Anatomy. According to Douglas the whole thing had ‘started as a joke and then got out of hand’. It has been suggested that Douglas may have harboured a grudge against Sollas, who un-obligingly retained his professorship to the age of 87 before yielding the Chair to Douglas.
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| style="vertical-align:top;" | 1978
| Marine exploration || Robert Gatliff, Head Marine Geoscience, BGS
| style="vertical-align:top;" | Martin Hinton (1883-1961)
| style="vertical-align:top;" | Hinton worked as a volunteer in the Natural History Museum from 1910-15. From 1921 to 1936 he worked in the Zoology Department retiring in 1945. In 1953, Hinton wrote to The Times saying that he and others at the Museum had always believed the jaw to be that of a chimpanzee. In the following year he told the BBC that the forgery had been an inside job but would not name the forger, who was still alive. In 1978 a trunk bearing Hinton's initials was found at the Museum. Inside were bones and teeth, stained and carved in the same way as the Piltdown fossils and artefacts. It has been argued that Hinton could have sourced the orangutan jaw from the collections at the Museum, in which case it seems odd that he always professed the jaw to be that of a chimpanzee!
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| style="vertical-align:top;" | 1983
| Carbon capture and storage (CCS):demonstrating the concept || Andy Chadwick, Head CO2 Storage Research, BGS
| style="vertical-align:top;" | Arthur Conan Doyle (1859-1930)
| style="vertical-align:top;" | In 1983, American archaeologist John H. Winslow put forward the theory that Doyle had carried out the hoax. Doyle lived about seven miles from Piltdown, knew Dawson and Smith Woodward and was a qualified doctor, so could have had the scientific knowledge. He visited the Piltdown excavation in 1912 and is said to have been there on other occasions. His motive for the hoax, according to Winslow, was to fool the scientific community in revenge for their crusade against spiritualism, of which Doyle was to become a committed supporter. Doyle is also described as ‘a man who loved hoaxes, adventure, and danger’. Yet the case brought against him is based entirely on supposition.
At the same time the discoveries at Piltdown were being made, Doyle was writing ''The Lost World'', involving the discovery of dinosaurs and apemen on a plateau in South America. Of the latter, Lord John Roxton, a character in the novel, is made to say: ‘Missin’ Links, and I wish they had stayed missin’. A map of the plateau is claimed by Winslow to resemble the Weald in Sussex, with the centre corresponding to the gravel pits at Piltdown, while the figure of Professor Summerlee, described in the novel as an expert in the field of comparative anatomy, acerbic in manner and with a thin goat-like beard, is claimed to be based on Arthur Smith Woodward. Thus, Winslow concludes that ‘the Piltdown hoax was inspired by, or developed hand-in-hand with, the plot of The Lost World.’
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| style="vertical-align:top;" | 1985
| Future energy: renewable energy dividends from our coal mining legacy || Diarmad Campbell, Chief Geologist, Scotland, BGS
| style="vertical-align:top;" | Samuel Allinson Woodhead (c. 1872-1943)
| style="vertical-align:top;" | Woodhead accompanied Dawson to make an unsuccessful search of the Barkham Manor pit in 1908, and also undertook an analysis of a small fragment of the Piltdown skull at Dawson’s request. He was present at the excavations on a number of occasions. From a letter written by his sons, it seems that Woodhead suspected foul play by Dawson but would not speak of the matter. Two other, earlier letters state that Woodhead not only was present when the Piltdown jaw was found but himself discovered the canine tooth — this recollection appears in reality to relate to the finding by Woodhead of a beaver tooth in October 1913. The case against Woodhead was put forward by Peter Costello in November 1985 but seems to be based on a distorted reading of the above-mentioned letters.
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| style="vertical-align:top;" | 1986
| Keynote: The human planet || Iain Stewart, Professor of Geosciences, Communication, University of Plymouth
| style="vertical-align:top;" | John Theodore Hewitt (1868-1954)
| style="vertical-align:top;" | The revelation by Costello concerning Samuel Woodhead’s supposed involvement in the Piltdown fraud (previous slide) prompted a recollection from Mrs Elizabeth Pryce, a summary of which appeared in the March 1986 issue of the journal Antiquity. In 1952–3 she had been a neighbour of J. T. Hewitt, Professor of Chemistry at Queen Mary College, London, who revealed that ‘he and a friend had made the Piltdown Man as a joke’. Long before this, in 1898, Hewitt had disagreed with Dawson over the significance of a natural gas discovery at Heathfield in Sussex. Dawson got Woodhead to undertake an independent analysis, the result of which supported Dawson’s argument and was subsequently proven correct. It appears that Woodhead and Hewitt later came into contact as fellow council members of the Society of Public Analysts, possibly in late 1911. From this connection, Peter Costello quickly constructed a scenario in which Hewitt obtains the faked Piltdown assemblage while Woodhead salts the site in order to make a fool of Dawson. Apart from Hewitt’s supposed ‘confession’, there is no real evidence to back up his story. It may be noted that Hewitt was described by his obituarist as having had ‘a strong sense of humour.’
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| style="vertical-align:top;" | 1986
| '''Afternoon session B'''||
| style="vertical-align:top;" | Lewis Abbott (1853-1953)
| style="vertical-align:top;" | In his eminently readable book, The Piltdown Inquest (1986), Charles Blinderman examined the principal suspects and concluded that ‘Lewis Abbott has the best credentials to be the Piltdown hoaxer.’ Abbott was a jeweller at Hastings who established a reputation as an amateur prehistorian and supporter of the existence of primitive pre-Palaeolithic (Pliocene) man. He was thus a firm and vociferous believer in the authenticity of the much disputed ‘implements’ called ‘eoliths’, all of which were credited to ‘Pliocene Man’. Abbott was inclined to be bombastic and self important and was quick to claim credit for recognising the significance of Dawson’s discoveries at Piltdown. Abbott genuinely believed in the reality of Piltdown Man, and it is hard to see how his own self-seeking ambition could have been advanced by planting the Piltdown assemblage to the obvious advantage of Dawson.
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| style="vertical-align:top;" | 1990
| Malthus revisited? Population growth, environmental change and resource limits || Andrew Bloodworth, Head Minerals & Waste, BGS
| style="vertical-align:top;" | Frank Oswell Barlow (1880-1950)
| style="vertical-align:top;" | Caroline Grigson, curator of the Odontological Museum of the Royal College of Surgeons, suggested in 1990 that Frank Barlow, a preparator the Geology Department at the Natural History Museum, could have been Dawson’s accomplice. Barlow was responsible for making the Piltdown casts, from the sale of which he derived some financial benefit. Why, for example, did he not notice or draw attention to the evidence of artificial abrasion on the teeth? He could have supplied the Piltdown jaw from un-catalogued material held at the museum. Dawson may have sought Barlow’s advice on the preservation and hardening of fossil material. Yet any suggestion of connivance between them amounts to mere speculation, having as its basis the commonly held view that Dawson was incapable of creating the forgery alone.
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| style="vertical-align:top;" | 1990
| Looking forward to making predictions: BGS’s role in the next decade and beyond. || Andrew Hughes, Hydrogeologist, BGS
| style="vertical-align:top;" | Arthur Keith (1866-1955)
| style="vertical-align:top;" | At the time of the Piltdown discoveries, Keith was Conservator of the Hunterian Museum of the Royal College of Surgeons. He played a large part in the often heated debate surrounding the interpretation of the Piltdown finds, and he was still alive when the forgery was made public in 1953. In 1990 Frank Spencer accused Keith of being the Piltdown forger in his book Piltdown: a Scientific Forgery. The accusation was later reinforced by Philip Tobias. Yet the evidence against Keith is easily dismissed, being either of an inconsequential nature or based on incomplete information. News of the forgery came as a grave blow to Keith, who wrote a few weeks before his death lamenting that he had been so completely deceived by the ‘honest’ countenance of Dawson, a man for whom he had had the greatest respect.
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| style="vertical-align:top;" | 1990
|'''Panel session'''||
| style="vertical-align:top;" | ‘Chipper’ the goose (fl. 1912-1913)
| style="vertical-align:top;" | At least two writers have suggested, presumably in jest, that Chipper the goose was involved in the Piltdown fraud. Chipper was a frequent and somewhat threatening presence around the site and features in several photographs taken during the Barkham Manor excavations. It has been suggested, for example, that Chipper’s ferocious antics provided an appropriate distraction that enabled the forged items to be dropped surreptitiously onto the rain-washed spreads of gravel! The legacy of Piltdown, along with its increasing list of suspects, continues to grow ever more bizarre—yet it has its lighter moments!
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| style="vertical-align:top;" | 1994
|Featuring: Sir David Attenborough, Marcia McNutt (Director, USGS) Iain Stewart (Chair), Randy Parrish (Head of NIGL), Kathryn Goodenough (Geologist, BGS), Mike Ellis (Head of Climate Science, BGS).||
| style="vertical-align:top;" | Arthur Smith Woodward (1864-1944)
| style="vertical-align:top;" | In 1994 American physical anthropologist Gerell M Drawhorn put forward the theory that Smith Woodward may have colluded with Dawson on the forgery. Woodward’s motive was to enhance his reputation and improve his chances of being appointed Director of the Natural History Museum. While ambition alone is hardly sufficient to implicate Woodward in the forgery, it might have blinded him to any misgivings he should have entertained over some aspects of the Piltdown evidence - notably, for example, Dawson’s reluctance to identify the precise location of Piltdown II. Yet Woodward continued to dig at Piltdown for many years after his retirement, dictating his last book The Earliest Englishman shortly before his death.
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| style="vertical-align:top;" | 2003
|'''Closing remarks'''||
| style="vertical-align:top;" | Charles Panzetta Chatwin (1887-1971)
| style="vertical-align:top;" | Chatwin progressed from boy attendant at the Natural History Museum (1902–11), to Librarian at the Geological Society (1913–19), lecturer in palaeontology at the University of Liverpool (1919–20) and palaeontologist at the Geological Survey (1920–47). In 1975, Kenneth Oakley (one of the team that exposed Piltdown in 1953–55) privately named Chatwin as a possible conspirator, though his views were not made public until 2003. Chatwin’s motive would have been his dislike of Smith Woodward. Oakley came to believe that Chatwin had marshalled Hinton and others from the Museum, with the connivance of Dawson, to perpetrate a vengeful prank on Woodward, though what benefit Dawson was supposed to have derived from the exposure of this prank is left unexplained. Oakley met Chatwin in the 1950s and asked him about the Piltdown forgery. Chatwin apparently said ‘No, I am not talking about that’ and hurried off.
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|Closing remarks by Jon Gluyas (BGS Board Chair), and BUFI poster prize presentation.||
The Piltdown forgery has also found its way into popular culture via TV, theatre, film, literature and music. Film and Television
== Edward Greenly (1861–1951) ==
In the first episode of ''Quatermass and the Pit ''(BBC, 1958) the palaeontologist Matthew Roney (Cec Linder) who is excavating the remains of ape-men in Knightsbridge says that if he is wrong. A pub in Piltdown used to be called the ‘Piltdown Man’ in his conclusions, ‘They‘ll stick me alongside the Piltdown forgeries as a horrid warning.’
Cofir am [[Edward Greenly D.Sc.|Edward Greenly]] yn bennaf am ei arolwg daearegol o Ynys Môn, gwaith y bu wrthi am bron pum mlynedd ar hugain o’i fywyd.
In the ITV science fiction thriller ''Undermind, ''(1965) one character refers to a scandal involving a compromising diary as ‘the biggest hoax since the Piltdown Man’.
Image caption: Edward Greenly. Llun trwy garedigrwydd Terry Williams
In 1987 the BBC series QED produced ''Murder on the Bluebell Line ''starring Hugh Fraser as Sherlock Holmes and Ronald Fraser as Doctor Watson. In this docudrama Holmes and Watson investigate the Piltdown forgery and the possible suspects including Arthur Conan Doyle.
== Edward Greenly (1861–1951) ==
In 2009 a script for a proposed film ''The Wizard of Sussex ''was produced. This is described as a satire that centres on Charles Dawson and his discovery. Theatre
Campwaith pennaf [[Edward Greenly D.Sc.|Edward Greenly]] oedd cwblhau arolwg daearegol manwl o Ynys Môn. Cyhoeddwyd ''The Geology of Anglesey'' ([https://pubs.bgs.ac.uk/publications.html?pubID=B01782 Volume 1] and [https://pubs.bgs.ac.uk/publications.html?pubID=B06824 Volume 2]) mewn dwy gyfrol yn 1919 ac yna yn 1920 fap daearegol ar y raddfa un fodfedd i’r filltir. Er bod rhannau o’r gwaith wedi’u diweddaru yn ystod y degawdau dilynol, erys ei astudiaeth yn glasur o fri rhyngwladol.
In 2009 the Steppenwolf Theatre Company produced the play ‘Fake’ which was based on the forgery. This is set in 1914 at a meeting at Arthur Conan Doyle’s house that includes Dawson, Woodward and Teilhard de Chardin and in 1953 when the forgery is revealed. Literature and poetry
=== Mapio Môn ===
The discovery of Piltdown Man may have been one of the things that inspired Arthur Conan Doyle to write ''The Lost World ''(1912).
Wrth fapio ynys Môn, gwnaeth Greenly ddefnydd mawr o syniadau tectonig a ddatblygodd wrth iddo fynd i’r afael â gwaith maes cynharach yn Ucheldiroedd yr Alban. Roedd tair prif broblem yn ei wynebu: prinder brigiadau da, yn enwedig mewn ardaloedd mewndirol allweddol bwysig; presenoldeb creigiau gorchuddiol clytiog yn cuddio yn aml y baslawr Cyn-Gambriaidd hŷn; a phresenoldeb toriadau tectonig megis ffawtiau a chylchfaoedd croesrym a oedd yn aml yn rhwystro’r gwaith o gydberthyn gwahanol ddilyniannau o greigiau. Chwaraeodd ei wraig Annie Greenly (Barnard gynt), a oedd yn rhannu ei ddiddordeb mewn daeareg a diwinyddiaeth, rôl hollbwysig drwy baratoi’r mynegai i’w gyfrol.
It has been suggested that Rudyard Kipling’s short story ''Dayspring Mishandled ''(1928) may have been influenced by Piltdown. It concerns a forged Chaucer manuscript.
Ganed Greenly ym Mryste ac fe’i haddysgwyd yng Ngholeg Clifton. Bu’n fyfyriwr yng Ngholeg y Brifysgol, Llundain, cyn ymuno â’r Arolwg Daearegol yn 1889. Yn gyntaf, bu gofyn iddo baratoi arolwg o Ucheldiroedd gogledd-orllewin yr Alban. Daeth yn ffrind agos ac yn gydweithiwr i [[Benjamin Neeve Peach - biographical information|Ben Peach]] yr oedd ei archwiliadau wedi bod yn gyfrwng i ddatrys adeiledd cymhleth yr Alban (gan gynnwys adnabod a sylweddoli arwyddocâd Gwthiad Moine). Rhoddodd Greenly y gorau i’w waith gyda’r Arolwg yn 1895 er mwyn iddo, o’i ben a’i bastwn ei hun. roi cychwyn ar ei arolwg o Ynys Môn.
''Anglo-Saxon Attitudes ''by Angus Wilson (1956) was partly inspired by Piltdown. The novel features the archaeological excavation of the tomb of an Anglo-Saxon bishop. An idol which is uncovered is later revealed to be a fake. The book was adapted for television in 1992.
=== Cyfraniadau pwysig i ddaeareg ===
''Mask of the Jaguar ''by Jessica North (1981) is centred on a priceless Mayan jaguar mask of jade, bone and gold. At one point two ch aracters discuss a discovery in England that ‘fooled experts for years until new scientific tests unmasked the fraud’ and ‘the little man who must have perpetrated it―a respected, scholarly gentleman who had nothing―absolutely nothing!―to gain.’
Yn gydnabyddiaeth am ei gyfraniadau pwysig i ddaeareg, cafodd Edward Greenly ei dderbyn yn aelod er anrhydedd o gymdeithasau daearegol Caeredin a Lerpwl, a Chymdeithas Hynafiaethwyr Môn. Dyfarnwyd iddo Fedal Lyell, fawr ei bri, y Gymdeithas Ddaearegol yn 1920, medal Cymdeithas Ddaearegol Lerpwl yn 1933 a doethuriaeth er anrhydedd Prifysgol Cymru yn 1920.
''Skullduggery ''by Peter Marks (1987) is a fictional treatment of the forgery and features, Charles Dawson, Arthur Smith Woodward, Teilhard de Chardin, Kenneth Oakley, Conan Doyle and Oscar Wilde.
Ar y cyd â Howel Williams, cyhoeddodd [[Edward Greenly D.Sc.|Greenly]] ''Methods of Geological Surveying'' yn 1930 a’i hunangofiant ''A Hand through Time: Memories Romantic'' and ''Geological'' a ymddangosodd yn 1938. Bu farw ym Mangor yn 1951 ac yn briodol iawn fe’i claddwyd ym mynwent Llangristiolus, Ynys Môn. Mae ei fedd wedi’i gyfnodi’n Safle Geoamrywiaeth o Bwysigrwydd Rhanbarthol (RIGS).
== Table ==
The novel ''The Piltdown Confession ''by Irwin Schwartz (1994) is narrated by Charles Dawson, features Teilhard de Chardin and Conan Doyle and includes a murder mystery.
In 2018, Nick Flittner published ''Piltdown Man: The Man Who Never Was'', a poem that tells the story of the forgery from various points of view including those of Arthur Smith Woodward, Charles Dawson, Venus Hargreaves, J S Weiner and even Piltdown Man himself!
=Geologists' Association photograph albums [Green bound]=
''The Pilgrimage of Piltdown Man'' by Mike O’Leary (2019) is described as “…the story of Link, a cryptid, a knitted-together Piltdown Man...” Music
These two key albums of the GA focus on photographs of members.
In the early 1960s there was a rock and roll instrumental group called The Piltdown Men. They were from California and their singles included ‘Brontosaurus Stomp’ and ‘Goodnight Mrs Flintstone’.
The first volume contains portraits of early GA members and then photographs of individuals or groups of members taken on GA field excursions 1922–1977.
On Mike Oldfield’s ‘Tubular Bells’ (1973) he is listed as playing ‘Piltdown Man’ which refers to some unintelligible vocalisation he does on the album.
The second volume contains photographs of individuals or groups of members taken on GA field excursions 1979 to 1996.
Geological Survey of England and Wales 1:50,000 map tile: Sheet 13 Bellingham - data sources
Introduction (From memoir)
Crag Lough and Highfield Crags, Roman Wall.
The Bellingham district includes much of the Roman Wall country, the Northumbrian lakes, North Tynedale and Redesdale—all areas of outstanding, unspoilt beauty. They are underlain by Carboniferous rocks, 1600 m thick which were laid down around 300 million years ago. In the south and east, 'Yoredale'; limestones, sandstones and shales with the intrusive dolerite of the Whin Sill form scarp and dip-slope features, but in the forested areas to the north and west thick boulder clay of Pleistocene age mantles most of the solid rock and forms its own distinctive drumlin topography.
This memoir is the first comprehensive published account of the geology of the district. After an introductory chapter, the stratigraphy of the Carboniferous rocks is described in detail, with comprehensive correlation diagrams of sections and boreholes together with complementary palaeontological identifications.
Accounts of the igneous rocks and structure of the region are followed by chapters on the Pleistocene and economic geology. Appendices list boreholes, shafts, measured sections and geological photographs and conclude with a comprehensive bibliography.
Reference to the geology of the district can be found in many early works but the first systematic study was the primary six-inch geological survey by Hugh Miller Jnr., and D. Burns between 1875 and 1878. The solid edition of their one-inch map was published in 1881 followed by the drift edition in 1883. This map was not accompanied by a detailed geological succession nor were any major lithological subdivisions of the Carboniferous shown. A descriptive memoir written by Miller was not published. Small areas on the eastern and western edges of the district were resurveyed by G. A. Burnett (1932–35) and J. B. W. Day, D. H. Land and D. A. C. Mills (1954–58) respectively.
This memoir is the first comprehensive description of the geology of the district (Figure 3), though a number of generalised descriptions have appeared in works which deal with wider regions (e.g. Lebour, 1889; Garwood, 1910; Smith, 1912; Hickling and others, 1931; Taylor and others, 1971). In addition, important contributions to knowledge of the Carboniferous rocks of the district include those by Tate (1867a), Lebour (1873, 1875a, b), Johnson (1959), Fowler (1966) and Frost (1969). Igneous rocks have been studied by Tate (1867a, b, 1870). Topley and Lebour (1877), Teall (1884a, b), Heslop and Smythe (1910), Weyman (1910), Holmes and Harwood (1928, 1929), Smythe (1930), Randall (1959a, b), and Ineson (1972). Mineral deposits have been described by Wilson and others (1922), Smith (1923) and Dunham (1948); and the drift deposits and glacial retreat phenomena by Dwerryhouse (1902) and Smythe (1908, 1912).
Memoirs describing adjacent areas include those by Miller (1887), Clough (1889), Trotter and Hollingworth (1932), Fowler (1936) and Day (1970).
Maps
To view all published sheets for this areas visit the Maps Portal.
Geological Survey of England and Wales 1:63,360/1:50,000 geological map series, New Series
Sheet number:
13
Sheet title:
Bellingham.
Map type:
Drift
Scale:
1:50 000
Publication year:
1980
Author statement:
Original geological survey on the Six-Inch scale by H. Miller and D. Burns in 1875-1878. Published on the One-Inch scale as Old Series Sheet 106 NE in 1881 (Solid Edition) and 1883 (Drift Edition). Eastern margin resurveyed on the Six-Inch scale by G.A. Burnett in 1932-1935. Mineral Revision by K.C. Dunham in 1939-1945. Western margin resurveyed on the Six-Inch scale by J.B.W. Day, D.H. Land and D.A.C. Mills in 1954-59. W. Anderson, District Geologist. Resurveyed on the Six-Inch scale by D.V. Frost and D.W. Holliday in 1968-1975.
Published statement:
Published 1980. Print code: 3500/80.
Solid map details
Map series:
Geological Survey of England and Wales 1:63,360/1:50,000 geological map series, New Series
Sheet number:
13
Sheet title:
Bellingham.
Map type:
Solid
Scale:
1:50 000
Publication year:
1980
Author statement:
Original geological survey on the Six-Inch scale by H. Miller and D. Burns in 1875-1878. Published on the One-Inch scale as Old Series Sheet 106 NE in 1881 (Solid Edition) and 1883 (Drift Edition). Eastern margin resurveyed on the Six-Inch scale by G.A. Burnett in 1932-1935. Mineral Revision by K.C. Dunham in 1939-1945. Western margin resurveyed on the Six-Inch scale by J.B.W. Day, D.H. Land and D.A.C. Mills in 1954-59. W. Anderson, District Geologist. Resurveyed on the Six-Inch scale by D.V. Frost and D.W. Holliday in 1968-1975.
Published statement:
Published 1980. Print code: 3500/80.
Six-inch maps
The following is a list of six-inch geological maps included in the area of 1:50000 Geological Sheet 13 with the date of survey for each map. The surveying officers are: G. A. Burnett, J. B. W. Day, D. V. Frost, D. W. Holliday, D. H. Land and D. A. C. Mills. Copies of the maps are deposited for public reference in the libraries of the London and Leeds Offices of the Institute of Geological Sciences. Uncoloured dyeline copies of those marked by an asterisk are available for purchase. Xerox copies of the remaining partially surveyed sheets are also available.
NY 66 NE Tipalt Burn
Day
1954
NY 67 SE* Wileysike
Day
1954
NY 67 NE* Churnsike
Mills
1954–58
NY 68 SE* Christy's Crags
Mills
1957–58
NY 68 NE Whickhope
Land
1958
NY 76 NW Edges Green
Frost
1973
NY 76 NE Broomlee and Greenlee
Frost
1973
NY 77 SW* Grindon Green
Frost
1970
NY 77 SE* Shepherdshield
Frost
1968–69
NY 77 NW* Green Moor
Holliday
1974
NY 77 NE* Blackaburn and Stonehaugh
Frost
1972–73
NY 78.SW* Chirdon Burn
Holliday
1973–74
NY 78 NW Falstone
Holliday
1973
NY 78 NE Greenhaugh
Holliday
1973
NY 86 NW Grindon Hill
Frost and Holliday
1968
NY 86 NE Newbrough and Fourstones
Holliday
1968
NY 87 SW* Sewingshields
Frost
1968
NY 87 SE* Simonburn
Frost and Holliday
1968–69
NY 87 NW* Warksburn
Frost
1971
NY 87 NE* Birtley and Wark
Frost
1970
NY 88 SW* Bellingham
Frost
1972–73
NY 88 SE* Redesmouth
Frost
1972
NY 88 NW Hareshaw
Frost
1973
NY 88 NE West Woodburn
Frost
1973
NY 96 NW Wall
Holliday
1971
NY 96 NE Stagshaw
Burnett and Holliday
1935, 1971
NY 97 SW* Barrasford
Holliday
1971
NY 97 SE* Bingfield
Burnett and Holliday
1934–35,1968,1971
NY 97 NW* Gunnerton
Frost
1971
NY 97 NE* Hallington
Burnett and Holliday
1932–34,1971–73
NY 98 SW* Ridsdale
Frost
1972–73
NY 98 SE* Great Bavington
Burnett and Holliday
1932–33,1972–73
NY 98 NW East Woodburn
Frost
1973
NY 98 NE Raechester
Burnett and Holliday
1933, 1973
Memoir
Geology of the country around Bellingham. Memoir for 1:50 000 geological sheet 13 by D.V. Frost and D.W. Holliday
Bibliographical reference: Frost, D.V. and Holliday, D.W. 1980. Geology of the country around Bellingham. Mem. Geol. Surv. G.B., Sheet 13, 112 pp.
BGS175: 175th Anniversary Science Symposium of the founding of the British Geological Survey, 28th September, Royal Institution, London
The British Geological Survey is the world's oldest national geological survey and commemorated its 175th anniversary in 2010.
The event was marked by a one-day science symposium on 28 September 2010.
The symposium showcased our world-class science and technologies, demonstrating their relevance, societal benefits and positive impacts in addressing 21st century challenges; including living with environmental change, energy and natural resource security, rising CO2 emissions and geohazards.
Peak metal: Scarcity of supply or scare story?
Bronze Age Mediterraneans may have visited Stonehenge
Modelling of Icelandic volcanic ash particles
The event was attended by influential stakeholders including representatives from government, industry, academia, international geological surveys, students and the national media.
Acuity, accuracy and application: from systematic geological mapping to responsive 3D+ surveys
Martin Smith, Head Geology & Landscape, BGS
From watercolour to web
Keith Westhead, Head Knowledge Exchange, BGS
Keynote: Facing tomorrow’s challenges with integrated science
Marcia McNutt, Director, USGS
Morning session B
OneGeology: improving access to geoscience globally
Ian Jackson, Chief of Operations, BGS
North American liaisons
Garth Earls, Director, GSNI
Arabian adventures: geological mapping and climate change in Arabia
Andrew Farrant, Geologist, BGS
Groundwater animals: extending our understanding of biodiversity in the UK
Louise Maurice, Groundwater ecologist, BGS
Life just got complicated
Dr Phil Wilby, Geologist, BGS
Afternoon session A
Predict or prepare: natural hazards and human disasters
David Kerridge, Head Earth Hazards & Systems, BGS
Groundwater, health and livelihoods in Africa
Alan MacDonald, Hydrogeologist, BGS
Marine exploration
Robert Gatliff, Head Marine Geoscience, BGS
Carbon capture and storage (CCS):demonstrating the concept
Andy Chadwick, Head CO2 Storage Research, BGS
Future energy: renewable energy dividends from our coal mining legacy
Diarmad Campbell, Chief Geologist, Scotland, BGS
Keynote: The human planet
Iain Stewart, Professor of Geosciences, Communication, University of Plymouth
Afternoon session B
Malthus revisited? Population growth, environmental change and resource limits
Andrew Bloodworth, Head Minerals & Waste, BGS
Looking forward to making predictions: BGS’s role in the next decade and beyond.
Andrew Hughes, Hydrogeologist, BGS
Panel session
Featuring: Sir David Attenborough, Marcia McNutt (Director, USGS) Iain Stewart (Chair), Randy Parrish (Head of NIGL), Kathryn Goodenough (Geologist, BGS), Mike Ellis (Head of Climate Science, BGS).
Closing remarks
Closing remarks by Jon Gluyas (BGS Board Chair), and BUFI poster prize presentation.
Cofir am Edward Greenly yn bennaf am ei arolwg daearegol o Ynys Môn, gwaith y bu wrthi am bron pum mlynedd ar hugain o’i fywyd.
Image caption: Edward Greenly. Llun trwy garedigrwydd Terry Williams
Edward Greenly (1861–1951)
Campwaith pennaf Edward Greenly oedd cwblhau arolwg daearegol manwl o Ynys Môn. Cyhoeddwyd The Geology of Anglesey (Volume 1 and Volume 2) mewn dwy gyfrol yn 1919 ac yna yn 1920 fap daearegol ar y raddfa un fodfedd i’r filltir. Er bod rhannau o’r gwaith wedi’u diweddaru yn ystod y degawdau dilynol, erys ei astudiaeth yn glasur o fri rhyngwladol.
Mapio Môn
Wrth fapio ynys Môn, gwnaeth Greenly ddefnydd mawr o syniadau tectonig a ddatblygodd wrth iddo fynd i’r afael â gwaith maes cynharach yn Ucheldiroedd yr Alban. Roedd tair prif broblem yn ei wynebu: prinder brigiadau da, yn enwedig mewn ardaloedd mewndirol allweddol bwysig; presenoldeb creigiau gorchuddiol clytiog yn cuddio yn aml y baslawr Cyn-Gambriaidd hŷn; a phresenoldeb toriadau tectonig megis ffawtiau a chylchfaoedd croesrym a oedd yn aml yn rhwystro’r gwaith o gydberthyn gwahanol ddilyniannau o greigiau. Chwaraeodd ei wraig Annie Greenly (Barnard gynt), a oedd yn rhannu ei ddiddordeb mewn daeareg a diwinyddiaeth, rôl hollbwysig drwy baratoi’r mynegai i’w gyfrol.
Ganed Greenly ym Mryste ac fe’i haddysgwyd yng Ngholeg Clifton. Bu’n fyfyriwr yng Ngholeg y Brifysgol, Llundain, cyn ymuno â’r Arolwg Daearegol yn 1889. Yn gyntaf, bu gofyn iddo baratoi arolwg o Ucheldiroedd gogledd-orllewin yr Alban. Daeth yn ffrind agos ac yn gydweithiwr i Ben Peach yr oedd ei archwiliadau wedi bod yn gyfrwng i ddatrys adeiledd cymhleth yr Alban (gan gynnwys adnabod a sylweddoli arwyddocâd Gwthiad Moine). Rhoddodd Greenly y gorau i’w waith gyda’r Arolwg yn 1895 er mwyn iddo, o’i ben a’i bastwn ei hun. roi cychwyn ar ei arolwg o Ynys Môn.
Cyfraniadau pwysig i ddaeareg
Yn gydnabyddiaeth am ei gyfraniadau pwysig i ddaeareg, cafodd Edward Greenly ei dderbyn yn aelod er anrhydedd o gymdeithasau daearegol Caeredin a Lerpwl, a Chymdeithas Hynafiaethwyr Môn. Dyfarnwyd iddo Fedal Lyell, fawr ei bri, y Gymdeithas Ddaearegol yn 1920, medal Cymdeithas Ddaearegol Lerpwl yn 1933 a doethuriaeth er anrhydedd Prifysgol Cymru yn 1920.
Ar y cyd â Howel Williams, cyhoeddodd GreenlyMethods of Geological Surveying yn 1930 a’i hunangofiant A Hand through Time: Memories Romantic and Geological a ymddangosodd yn 1938. Bu farw ym Mangor yn 1951 ac yn briodol iawn fe’i claddwyd ym mynwent Llangristiolus, Ynys Môn. Mae ei fedd wedi’i gyfnodi’n Safle Geoamrywiaeth o Bwysigrwydd Rhanbarthol (RIGS).
Table
Geologists' Association photograph albums [Green bound]
These two key albums of the GA focus on photographs of members.
The first volume contains portraits of early GA members and then photographs of individuals or groups of members taken on GA field excursions 1922–1977.
The second volume contains photographs of individuals or groups of members taken on GA field excursions 1979 to 1996.
