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In September 1940, 42nd Geological Section of the South African Engineer Corps moved from Kenya to an operational base near Cairo in Egypt, continuing to serve within the British Army's Middle East Command but with leadership by the newly-promoted Major Gordon Lyall Paver (1913–1988). The main part of the Section was employed to support the British 8th Army and operations west of the River Nile, particularly in the Western Desert of Egypt and Libya to Tunisia but also from bases elsewhere in Egypt, with surveys principally by means of electrical earth resistivity: guiding the deployment of Boring Sections Royal Engineers and other units in drilling boreholes from which to abstract potable groundwater. Detachments with similar roles were also employed further east of the Nile, in Sinai, Palestine, Transjordan, Syria and Lebanon, Iraq and Iran. In the Mediterranean region more generally, from 1943 additional deployments included Malta, Sicily and Cyprus, and later Greece. As conflict in North Africa came to an end in the spring of 1943, and so as to promote the use of geology and geophysics (rather than water diviners) as the best means for guiding the choice of sites for boreholes, Paver led teaching of a military training course in geophysical survey methods and the compilation of an authoritative textbook. In early 1945, as conflict in the European Theatre of Operations entered its final months, Paver assisted planning in England for potential deployment of the Section to the Far East and for the development there of an enhanced military geological staff—although hostilities came to an end before these plans materialized. Towards the end of his service, Paver completed for publication the final six of an 11-part series of articles on 'Water supply in the Middle East campaigns' that placed much military hydrogeological information on permanent public record. Demobilized in February 1946, Paver returned to a career as a consultant geophysicist, notably promoting 'resistivity' surveys to locate 'underground water', surveys including significant fieldwork in Egypt, Pakistan and Cyprus that developed his wartime skill base. He had pioneered and mostly directed the use of electrical earth resistivity surveys in support of British military operations during World War II and begun to influence a generation of Royal Engineers through his textbook: re-printed by the United Kingdom's War Office in April 1945 to facilitate its long-term and wider use. Military honours were duly bestowed upon him for 'gallant and distinguished services' during the war. [ABSTRACT FROM AUTHOR]

42nd Geological Section of the South African Engineer Corps was a unique unit that supported British armed forces during World War II. It was co-founded and led for most of the war by Gordon Lyall Paver (1913–1988), one of the few 'British' officers serving specifically as geologists during the war to achieve the rank of major. Born in South Africa at Johannesburg and in his early years educated there at St. John's College, from 1926 Paver was educated in England, at Charterhouse School until admitted in 1931 to Pembroke College in the University of Cambridge, where he studied chemistry, geology and mineralogy. He graduated in 1934 and returned to South Africa, being appointed to the Geological Survey of South Africa as one of its first geophysicists and contributing to magnetometric and gravimetric surveys in the Transvaal region, expertise used in 1938 to 1940 to draft his thesis for a PhD degree (awarded in 1942). Although married in 1939 and briefly employed as a consultant geophysicist, in August 1940 Paver was one of the first three geoscientists to be mobilized as officers to found 42nd Geological Section, at Zonderwater near Pretoria in South Africa. After only a month's military training, at the end of September the Section and its vehicles deployed by rail and sea to a base near Nairobi in Kenya for operational service in East Africa, with 'Acting Captain' Paver as its Second-in-Command. Detachments from the Section were widely deployed in Kenya and later in Italian and British Somaliland (present-day Somalia) and also in Abyssinia (present-day Ethiopia) for surveys by means primarily of electrical earth resistivity but also vertical force magnetometer. These guided drilling of wells by another unit of the South African Engineer Corps to abstract potable groundwater— thereby facilitating troop concentrations and forward movements in arid or semi-arid regions during the 'British' Army's East African Campaign. Members of the Section also compiled geological maps of Kenya at scales of 1:1,000,000 and 1:2,000,000 and pioneered a military geological unit created within the East African Engineers that supported British forces in the region from 1941 to 1945. The Campaign drew to a victorious close during 1941 and, from the end of August, the Section was re-deployed northwards to a base near Cairo in Egypt. It continued to serve within the British Army's Middle East Command but with leadership now by Paver, promoted 'Acting Major' from 31 August and in December 'mentioned in despatches' for his earlier distinguished service in East Africa. [ABSTRACT FROM AUTHOR]

The term 'military geology', translated from German after earlier use in French and Spanish publications, entered the English language via American publications from 1917 onwards, initially after the USA entered World War I. It was widely used in the USA and, in direct or indirect translation, in several European countries additional to Germany and Austria thereafter, but not in the United Kingdom—although military applications of geology had been perceived and utilized by the British Army for much of the previous century. However, the term was used and its scope defined on the basis of operational experience at a meeting in Brussels on 28 February to 1 March 1945 as World War II drew to an end, a meeting seemingly unique for the War in that it comprised five 'British' geologist officers of field rank: the South African Major Gordon Lyall Paver, English Major Frederick William Shotton, Australian-born but Canadian-educated English Major John Leonard Farrington, English Squadron Leader John Francis Kirkaldy, and Welsh Major David Ronald Arthur Ponsford. Their purpose was to review wartime use of 'military geology' in the British Army, and to make recommendations for a more efficient British military geological service in the future, especially in the Far East after the war in Europe entered its final phase. The meeting generated a four-page closely-typed unpublished 'Memorandum: Military geology in the British services' (now preserved in England in the Lapworth Museum at the University of Birmingham and in The National Archives, Kew, near London). This included a very brief summary of the British Army's deployment of geologists within western Europe, East Africa, the Middle East, North Africa and the Mediterranean region, and India. Those present brought together long experience from all these campaign areas except India (and the Far East in general). That deficiency was made good later in the year, on 7 December 1945, when Eric J. Bradshaw, Superintending Geologist of the Strategic Branch of the Geological Survey of India, completed an 81-page typed unpublished 'Military geology: Memorandum of post-war policy' (accessible in England at Birmingham, at Kew, and at the British Geological Survey, Keyworth). This with its 23 pages of appendices records details of wartime work in India and discussions held by the author there and in the United Kingdom following the end of hostilities in Europe on 8 May 1945. It re-defines the scope of 'military geology' for British armed forces in terms of water (resources, floods and drainage), stone and miscellaneous mineral resources, soils, engineering projects (reconnaissance, stability and excavations), terrain, 'photo-geology' and several miscellaneous applications. The memorandum proposed a grandiose organization of 151 geologist officers plus ancillary staff for British military geology postwar. That organizational scheme was not adopted—but by 1945 the term 'military geology' had clearly extended from American to significant British use. [ABSTRACT FROM AUTHOR]

During the nineteenth century, geology was perceived by the British Army as a military science, and two geological survey departments outside Great Britain were pioneered by Royal Engineer officers in the rank of captain: J. W. Pringle, J. E. Portlock and Henry James nearly successively in Ireland between 1826 and 1846; H. G. Lyons in Egypt from 1896 to 1898 and then, as a civilian, until 1909. During World War I, the Welsh-born Australian T. W. Edgeworth David and the Canadian R. W. Brock served on attachment to the Royal Engineers in the rank of major, David as the senior of two geologists in appointment as such with the British Army in France and Belgium 1916–1919, Brock in Palestine 1918–1919. (David was rewarded by promotion to lieutenant-colonel ten days before the end of hostilities). During World War II, between 1939 and 1945, W. B. R. King, F. W. Shotton, J. V. Stephens, W. A. Macfadyen, J. L. Farrington and D. R. A. Ponsford plus the South Africans H. F. Frommurze and G. L. Paver (and possibly also H. Digby Roberts) all achieved the rank of major whilst in appointment as geologists serving with British forces, complemented in the Far East by Majors A. J. Haworth and A. N. Thomas supervised by E. J. Bradshaw for the Indian Army. (King was rewarded with promotion to lieutenant-colonel in October 1943, when released from the Army to take up appointment as Woodwardian Professor of Geology at the University of Cambridge). During the remaining twentieth century, N. L. Falcon, D. R. A. Ponsford, A. W. Woodland, A. F. Fox, Frank Moseley, R. M. S. Perrin, S. C. L. Hobden, L. R. M. Cocks and J. C. Eaton became geologist majors in the British reserve army, and five majors were promoted to be geologist lieutenant colonels: T. G. Miller 1964–1967, N. F. Hughes 1967–1970, P. I. Manning 1971–1972, E. P. F. Rose 1978–1987 (colonel 1987–1990) and M. S. Rosenbaum 1995–2001. Thereafter, a post for a geologist lieutenant colonel became established in the British reserve army, an appointment held by R. I. L. Dow 2006–2011, S. R. S. Matthews 2011–2014, M. H. K. Bulmer 2014– 2019, A. G. Craig 2019–2022, and S. R. S. Matthews again from 2022, each supported by one or two geologist majors. In 200 years, about 21 British military geologists achieved the final rank of major and only 11 the higher rank of lieutenant colonel (the highest rank yet to be attained by a geologist to serve operationally as such in the British Army). Overall, they helped to pioneer and to promote an innovative range of military applications of geology. [ABSTRACT FROM AUTHOR]

During the Second World War, the central Mediterranean island of Malta was famously besieged by the Italian navy and intensively bombed by Italian and later German air forces, from June 1940 until Allied victory in North Africa in May 1943 brought an end to the siege. It was then scheduled as a staging post to support the Allied invasion of Sicily from North Africa in July 1943 and of mainland Italy from Sicily in September. From 1941 until 1945, two Tunnelling Companies Royal Engineers, overlapping in succession, excavated underground facilities safe from aerial or naval bombardment. In 1943 and then 1944–1945, two Boring Sections Royal Engineers in succession drilled wells to enhance water supplies, initially for increased troop concentrations. Borehole site selection was guided in 1943 by the Director of the Geological Survey of Great Britain (Edward Battersby Bailey: 1881–1965) and by geologists Captain Frederick William Shotton (1906–1990) and Major Gordon Lyall Paver (1913–1988). In 1944, it was guided by geologist Captain Howard Digby Roberts (1913–1971), leading a detachment from 42nd Geological Section of the South African Engineer Corps that pioneered earth resistivity surveys on the island. Overall, these military studies generated a new but unpublished geological map of the island at 1:31,680-scale and refined knowledge of its geological structure: a much faulted but otherwise near-horizontal Oligo-Miocene sedimentary sequence. Further refinement was achieved as a consequence of the 1944–1945 drilling programme, led principally by geologist Captain Thomas Owen Morris (1904–1989) of the Royal Engineers. By 1945, this had helped to develop an improved water supply system for the island, and plans to develop groundwater abstracted from a perched upper aquifer (in the Upper Coralline Limestone and underlying Greensand formations, above a 'Blue Clay') as well as from the main lower aquifer, near sea level (in the Globigerina Limestone and/or underlying Lower Coralline Limestone formations). [ABSTRACT FROM AUTHOR]

Malta, an island in the central Mediterranean Sea, was fortified as a base for the Knights Hospitaller 1530–1798 and to provide major harbours for the British Royal Navy after 1813. Men with British military associations (all subsequently to attain some distinction in public and/or academic life) were amongst the many pioneers of Maltese geology who established the essence of its outcrop stratigraphy and structure: a circa 300-metre-thick sequence of near-horizontal mid-Cenozoic fossiliferous limestones punctuated by a 'blue clay/marl', cut by a series of major faults and penetrated by several caves and fissures whose infill contained significant remains of Pleistocene vertebrates. Between 1843 and 1856, Lieutenant (later Vice-Admiral) Thomas Abel Brimage Spratt (1811–1888) defined major units in the bedrock sequence, Colonel (later Major-General) Sir William Reid (1791–1858) promoted publication of a geological memoir, and a 1:31,680-scale geological map prepared by the 3rd Earl of Ducie on a Royal Engineers topographical base map was published under Royal Engineer auspices. Mostly between 1860 and 1866, Captain (later Professor) Frederick Wollaston Hutton (1836–1905) and Surgeon (later Deputy Surgeon-General and Professor) Andrew Leith Adams (1827–1882) made field observations that refined earlier interpretations of stratigraphy and structure and generated revised but small-scale maps. They also collected specimens that facilitated specialist identifications of Malta's fossil faunas, including foraminifera by Thomas Rupert Jones (1819–1911), Professor of Geology at the Royal Military College, Sandhurst. Rock specimens were sent in 1888 by Surgeon-Captain David (later Surgeon-General Sir David) Bruce (1855–1931) and the former engineer Lieutenant (and later Professor) Osbert Chadwick (1844–1913) to the pioneer oceanographer John (later Sir John) Murray (1841–1914). They stimulated Murray's benchmark study 1889–1890 of Malta's sedimentary sequence and fossil foraminifera, and their palaeoenvironmental interpretation, plus his compilation of a 1:129,254-scale geological map. These prompted extensive local studies and collection of macrofossil specimens by schoolmaster (later Lieutenant-Colonel) John Henry Cooke (1862–1933). By the end of the century, representative Maltese fossils had been presented for specialist study and identification or description to major museums in England, Scotland and Italy, facilitating improved correlation of Maltese strata with Oligo-Miocene successions elsewhere. [ABSTRACT FROM AUTHOR]

Military applications of geology became apparent within the United Kingdom during the nineteenth century, and were developed during the First World War and more extensively during the Second, incidentally by some officers with links to Canada. In the nineteenth century, three Royal Engineer major-generals with geological interests had served there briefly: Joseph Ellison Portlock (1794–1864) helped to stem invasion of Upper Canada by the United States Army in 1814, pioneer geological survey in Ireland from 1826, and promote knowledge of geology amongst British Army officers; Frederick Henry Baddeley (1794–1879) helped to pioneer geological studies in south-east Canada in the 1820s; Richard John Nelson (1803–1877) served in Canada after mapping the geology of Jersey in 1828 and making geological observations in Bermuda. During the First World War, Tannatt William Edgeworth David (1858–1934), a Welsh-born Australian and from 1916 to 1918 the senior of two geologists serving with the British Army on the Western Front, had a Canadian military family link through his mother; and Reginald Walter Brock (1874–1935), Dean of Applied Science at the University of British Columbia and a distinguished Canadian geologist, interrupted his career for infantry service in Europe but was used as a geologist from mid-1918, in Palestine. During the Second World War, the British military geologist Frederick William Shotton (1906–1990) provided geological advice to, amongst other units, Canadian forces who generated thematic maps for parts of northern France that predicted 'going' (conditions affecting cross-country vehicle mobility) to follow the D-Day Allied landings in Normandy. In 1943, Thomas Crawford Phemister (1902–1982), Professor and Head of the Department of Geology and Mineralogy at the University of Aberdeen in Scotland but from 1926 to 1932 an associate professor at the University of British Columbia, as an 'emergency' Royal Engineers captain founded the Geological Section of the Inter-Service Topographical Department, a unit whose reports and thematic maps provided terrain intelligence for Allied forces in both Europe and the Far East from a base in England, within the University of Oxford. John Leonard Farrington (1906–1982), an undergraduate student from 1923 to 1928 of Brock and/or Phemister at the University of British Columbia, co-founded the Section and soon succeeded Phemister as its head, from 1944 to 1945 in the rank of major. Soon after 1945, military geologists became established in continuity within the British Army. [ABSTRACT FROM AUTHOR]

The year 2019 marks the 80th anniversary of the start of the Second World War and the 75th anniversary of the Allied landings in Normandy: respectively the first major conflict in which geologists were deployed professionally in uniform by opposing sides from the start of hostilities, and the first successful major amphibious assault whose planning was significantly influenced by geologists. 'Military geology' had become established within major world powers as a discipline relevant to military operations, following its initial development in the First World War. The term in English had entered scientific literature via publications in the USA from 1917 onwards, initially by Joseph Ezekiel Pogue, Jr (1887–1971). This followed use of 'Militärgeologie' from 1913 by Walter Kranz (1873–1953) in Germany, a term subsequently used also in Austria-Hungary, although mostly replaced by 'Kriegsgeologie' in both nations from 1915 and by 'Wehrgeologie' from about 1935. However, 'géologie militaire' was in French use even earlier, notably in the sub-titles of books by an infantry officer, Joseph-Charles-Auguste Clerc (1840–1910), on the French Alps in 1882 and the Jura mountains in 1888. This term complemented use of 'géographie militaire', a name in use since 1836 for a subject whose study was given impetus in France by defeat in the Franco-Prussian War of 1870–1871. In recent years 'military geoscience' has come into more popular use, reuniting military geology with geography and embracing associated disciplines. [ABSTRACT FROM AUTHOR]

'Bill' Wager, after undergraduate and postgraduate studies at the University of Cambridge, became a lecturer at the University of Reading in southern England in 1929. He was granted leave in the 1930s to participate in lengthy expeditions that explored the geology of Greenland, an island largely within the Arctic Circle. With friends made on those expeditions, he became in June 1940 an early recruit to the Photographic Development Unit of the Royal Air Force that pioneered the development of aerial photographic interpretation for British armed forces. He was quickly appointed to lead a 'shift' of interpreters. The unit moved in 1941 from Wembley in London to Danesfield House in Buckinghamshire, known as Royal Air Force Medmenham, to become the Central Interpretation Unit for Allied forces—a 'secret' military intelligence unit that contributed significantly to Allied victory in World War II. There Wager led one of three 'shifts' that carried out the 'Second Phase' studies in a three-phase programme of interpretation that became a standard operating procedure. Promoted in 1941 to the rank of squadron leader in the Royal Air Force Volunteer Reserve, he was given command of all 'Second Phase' work. Sent with a detachment of photographic interpreters to the Soviet Union in 1942, he was officially 'mentioned in a Despatch' on return to England. By the end of 1943 the Central Interpretation Unit had developed into a large organization with an experienced staff, so Wager was allowed to leave Medmenham in order to become Professor of Geology in the University of Durham. He resigned his commission in July 1944. Appointed Professor of Geology in the University of Oxford in 1950, he died prematurely from a heart attack in 1965, best remembered for his work on the igneous rocks of the Skaergaard intrusion in Greenland and an attempt to climb Mount Everest in 1933. [ABSTRACT FROM AUTHOR]

The central text of this paper has been transcribed directly from the handwritten, unpublished 'Abstract of Notes' by Tannatt William Edgeworth David (1858-1934), an Australian geologist of great distinction, from which he lectured at the Geological Society of London on 26 February 1919. He was then en route home to Australia after serving on the Western Front, across parts of Belgium and northern France, in the First World War--as the senior of two geologists at General Headquarters, British Expeditionary Force. His text provides the first overall account of military applications of geology on a battlefield by any geologist to serve as such in action with British troops. An introduction, illustrations, references, footnotes and concluding discussion have been added by E. P. F. Rose to amplify (and slightly amend) David's hastily-compiled personal record. [ABSTRACT FROM AUTHOR]

Edward Battersby Bailey (1881-1965), Director of the Geological Survey of Great Britain, visited the 6-km² Gibraltar peninsula twice in 1943, in transit from/to England and the Mediterranean island of Malta. He spent only five days in total On Gibraltar, but submitted two influential reports to its Fortress Headquarters, guided by rock features exposed by recent quarrying. On his recommendation, a deep borehole was drilled below the northern isthmus in an attempt to locate a supposed aquifer in Cenozoic sandstones believed to extend south from Spain, and A. L. Greig (a graduate of Imperial College, London, serving locally in the ranks of the Royal Engineers) prepared a new geological map (at 1:5,280) and a report to help guide tunnel excavation within the bedrock. Between 1945 and 1948, Lieutenant (later Captain) G. B. Alexander (a graduate of the University of Cambridge also serving in the Royal Engineers) generated a much more detailed map (at 1:2,500) of the bedrock plus superficial deposits, together with associated diagrams and geotechnical reports. These unpublished documents, and fossils collected during their preparation, influenced a re-interpretation of Gibraltar (as the remnant of an overturned limb of a klippe of Early Jurassic dolomitic limestone thrust into position during the Betic-Rif Orogeny), published by Bailey in 1953. A report to accompany Alexander's map was never completed, but documents constituting the most complete record known of his Gibraltar work are now preserved within the archives of the British Geological Survey. Reserve army officers later compiled a geological map of Gibraltar (at 1:10,000) published by the Royal Engineers in 1991. Thereafter, as garrison strength became greatly reduced, work under military auspices was increasingly superseded by civilian research. [ABSTRACT FROM AUTHOR]

The 1860s marked a period of intense early interest in the antiquity of man, and so cave archaeology, in England and elsewhere. Systematic cave archaeology was initiated on Gibraltar in 1863 by a former infantry officer, Frederick Brome, the governor of the military prison, and his discoveries prompted cave exploration and local geological interest by two young British Army officers stationed on the Rock: Alexander Burton-Brown of the Royal Artillery and the subsequently more famous Charles (later Sir Charles) Warren of the Royal Engineers. On the recommendation of Sir Charles Lyell, President of the Geological Society of London, Brome's excavated material was sent to England for study by George Busk and Hugh Falconer: both palaeontologists of considerable distinction. The new discoveries drew attention to the 'Gibraltar Skull', presented to the Gibraltar Scientific Society by Lieutenant Edmund Flint of the Royal Artillery in 1848 but recognized only after description of Homo neanderthalensis from Germany in 1864 as a relic of that extinct species--one of the most complete Neanderthal skulls known. Detailed topographical mapping of the Gibraltar peninsula by Charles Warren and interest in Gibraltar geology generated by cave studies led to the first geological survey of the Rock--by Andrew (later Sir Andrew) Crombie Ramsay and James Geikie of the "British" Geological Survey, in 1876. The first 'overseas' project to be undertaken by the Survey, this was historically significant because its purpose was primarily hydrogeological and it generated an atypically large-scale (1:2,500) geological map. The map and its 1877-1878 descriptive accounts, which featured Quaternary superficial sediments in more detail than the Jurassic limestone bedrock, were to guide development of Gibraltar's fortress infrastructure for the next sixty-five years. [ABSTRACT FROM AUTHOR]

The rocky peninsula of Gibraltar juts south from Spain at the western entrance to the Mediterranean Sea. Long famous as a landmark, it was ceded to Great Britain by the Treaty of Utrecht in 1713, and progressively developed as a naval and military base. Thomas James, a Royal Artillery officer stationed on Gibraltar from 1749 to 1755, was the first member of the British garrison to publish geological observations on the Rock, within a book of 1771 completed in New York. His military career culminated after active service against revolutionary Americans, finally in the rank of major-general, but with no further known contributions to geology. The Scotsman Ninian Imrie of Denmuir, an officer of the First Regiment of Foot (The Royal Scots), served on Gibraltar within the period 1784 to 1793, and was the first to publish an account specifically on its geology, in the Transactions of the Royal Society of Edinburgh in 1798. A career soldier, he achieved the rank of lieutenant-colonel before retiring to Scotland, and to amateur geological studies influenced by active membership of Edinburgh's Wemerian Natural History Society. James Smith of Jordanhill, near Glasgow, served in Great Britain in the Renfrewshire Militia during the Napoleonic Wars but, benefiting from a family fortune, later spent much time as a yachtsman and scholar of wide interests and influence. His studies on Gibraltar, published by the Geological Society of London in 1846, were the first to attempt a tectonic interpretation of the Rock's geological history, and to record local evidence for Quaternary sea level change. [ABSTRACT FROM AUTHOR]