Water supply maps for northern France created by British military geologists during World War II: precursors of modern groundwater development potential.

Slides:



Advertisements
Similar presentations
The Geology and Geological History of Vancouver Island Steven Earle, PhD Department of Geology Malaspina University-College Nanaimo, British Columbia,
Advertisements

The Geology & Geological History of Vancouver Island Steven Earle.
Natural Resources Bedrock Geology Coastlines. Natural Resources Nova Scotia Geology Precambrian to Carboniferous: undifferentiated intrusive rocks Precambrian:
Sedimentary Structures
Chapter 8 Fetter, Applied Hydrology 4 th Edition, 2001 Geology of Groundwater Occurrence.
The Geologic Timescale A calendar of geologic time.
Hydrogeology in the Limpopo Basin
EBS101 ENGINEERING GEOLOGY DR HAREYANI ZABIDI
Geology 1023 Cordillera and Appalachians. Orogenic (mobile) belts At the edges of continents Platform sequence that gets buckled by collision Also volcanism,
Models of the Earth Section 3 Section 3: Types of Maps Preview Key Ideas Topographic Maps Topographic Maps and Contour Lines Index Contour, Contour Interval,
Lecture Outlines Physical Geology, 12/e
Lesley A. Sebol, P. Barkmann, E. Johnson, F.S. Fitzgerald & W. Curtiss
Geology of Arkansas.
Advance Seismic Interpretation Project
by Aitor A. Ichaso, and Robert W. Dalrymple
Chapter 3 Section 3 Types of Maps Objectives
Quarterly Journal of Engineering Geology and Hydrogeology
Maps of eroded thicknesses of Triassic, Jurassic and Cretaceous sediments: (a) eroded thickness of the Triassic; (b) Lower and Middle Jurassic; (c) Upper.
by S. P. Gregory, L. D. Maurice, J. M. West, and D. C. Gooddy
DO NOW Pick up notes and Review #11. Turn IN Review #10.
Geology of Groundwater Occurrence
CLIMATE - HYDROGEOLOGY
Cordillera and Appalachians
Merged map showing the Late Jurassic tectonic framework of the Danish Central Graben after Ineson et al. Merged map showing the Late Jurassic tectonic.
Harry Williams, Historical Geology
Chapter 1 Introduction to engineering geology and geomorphology of glaciated and periglaciated terrains by C. J. Martin, A. L. Morley, and J. S. Griffiths.
by V. J. Banks, S. H. Bricker, K. R. Royse, and P. E. F. Collins
Steered Molecular Dynamics Studies of Titin I1 Domain Unfolding
Flip-flop detachment tectonics at nascent passive margins in SE Afar
by Jashar Arfai, and Rüdiger Lutz Petroleum Geology Conference
Quarterly Journal of Engineering Geology and Hydrogeology
The engineering geology of the Nottingham area, UK
The early Quaternary North Sea Basin
Late Cenozoic geological evolution of the northern North Sea: development of a Miocene unconformity reshaped by large-scale Pleistocene sand intrusion.
Introduction to Geohazards of Central China
Quarterly Journal of Engineering Geology and Hydrogeology
Location and Rock Type of
Quarterly Journal of Engineering Geology and Hydrogeology
Depth plot of maximum vertical hydraulic fracture propagation from all known shale gas operations in the Marcellus Shale from 2001 to 2010, with the base.
Journal of the Geological Society
Chapter 1 An overview of the petroleum geology of the Arctic
Middelburgse kade peat dyke: (a) cross-section; (b) comparison between hydraulic head predictions; (c) comparison between predictions and measurements;
Figure 1 – Soil Boring Locations
Merged map showing the Late Jurassic tectonic framework of the Danish Central Graben after Ineson et al. Merged map showing the Late Jurassic tectonic.
Liberation of selenium from alteration of the Bowland Shale Formation: evidence from the Mam Tor landslide by John Parnell, Liam Bullock, Joseph Armstrong,
Mine water rebound in South Nottinghamshire: risk evaluation using 3-D visualization and predictive modelling by S. Dumpleton, N. S. Robins, J. A. Walker,
Newbury slope: (a) slope cross-section and soil water retention and hydraulic conductivity function properties for the modelled London Clay; (b) history.
Quarterly Journal of Engineering Geology and Hydrogeology
Journal of the Geological Society
Shrinkage limit test results and interpretation for clay soils
Calculated maturity (vitrinite reflectance values: Sweeney & Burnham 1990) at the top of the Posidonia Shale unit over four time steps: (a) modelled maturity.
Simplified cross-section illustrating internal structure and inferred stratigraphy of the South Chukchi and North Chukchi basins. Simplified cross-section.
Petroleum Geology Conference
A continental-scale geochemical atlas for resource exploration and environmental management: the National Geochemical Survey of Australia by P. de Caritat,
Quarterly Journal of Engineering Geology and Hydrogeology
Advances in engineering geology in the UK 1950–2018
An inclined Vulcanian explosion and associated products
(a) Outcrop evidence of overpressure along the Sagaing Fault: sandstones injected into a bedded Miocene sandstone. (a) Outcrop evidence of overpressure.
Map showing approximate limits of Northern Hemisphere ice sheets at the present day and during the Last Glacial Maximum (LGM). Map showing approximate.
Rafts of chalk emplaced within shallow marine sands and gravels of the Wroxham Crag Formation, exposed in the cliff face at Sidestrand, Norfolk; the upper.
Schematic cross-section for the Outer Wash, showing the ground conditions interpreted by the British Geological Survey (1991). tk, Undivided Mesozoic Strata.
(a) Southern Scotland and northern England coalfield exposure and locality of the Greenburn surface mine and (b) regional mineral resource geology of the.
Cropwell Bishop gypsum quarry.
NW–SE section across Figure 2 showing the regional dip (exaggerated) of the post-Palaeozoic strata and the NW-facing scarp slopes of the Permian strata.
What is the Status of Groundwater Science in Africa?
Hydrogeology of Ledgeview
Maps of Australia showing the location of the NGSA sample sites (dots) and (a) labelled geological regions of Australia (Blake & Kilgour 1998), and (b)
Quarterly Journal of Engineering Geology and Hydrogeology
Editorial by Eddie Bromhead, and Daren Gooddy
by Richard C. Ghail, and Jamie R. Standing
Presentation transcript:

Water supply maps for northern France created by British military geologists during World War II: precursors of modern groundwater development potential maps by N.S. Robins, E.P.F. Rose, and J.C. Clatworthy Quarterly Journal of Engineering Geology and Hydrogeology Volume 40(1):47-65 February 13, 2007 © 2007 The Geological Society of London

Top: geological map of northern France, simplified from part of 1:1000 000 scale GSGS 4452 map of 1943, with grid indicating coverage of water supply maps at scale of 1:250 000 prepared in 1944 (see Table 3). Top: geological map of northern France, simplified from part of 1:1000 000 scale GSGS 4452 map of 1943, with grid indicating coverage of water supply maps at scale of 1:250 000 prepared in 1944 (see Table 3). Bottom: larger-scale geological map for part of this region (approximately equivalent to sheets 3a & 8, 4 and 1), similarly simplified, showing coverage of water supply maps at scale of 1:50 000 prepared in 1943–44 (see Table 1). N.S. Robins et al. Quarterly Journal of Engineering Geology and Hydrogeology 2007;40:47-65 © 2007 The Geological Society of London

Diagrammatic geological cross-section WSW–ENE across part of Normandy (sheets 7F/1 to 8E/5 of Fig. 1, bottom), with major towns (named in upright font) and rivers (italic). Diagrammatic geological cross-section WSW–ENE across part of Normandy (sheets 7F/1 to 8E/5 of Fig. 1, bottom), with major towns (named in upright font) and rivers (italic). Key: grey stipple – basement; t2 – Triassic sandstones and conglomerates; j2 – massive (Jurassic) oolitic limestones; j3+2 – mixed sequence including (later Jurassic) marls, clays, sandstones and limestones; c2 – Chalk overlying Greensand and Gault Clay (all Cretaceous). After Aldwell et al. (1978), by kind permission. N.S. Robins et al. Quarterly Journal of Engineering Geology and Hydrogeology 2007;40:47-65 © 2007 The Geological Society of London

Diagrammatic geological cross-section W–E through the town of Caen (cf. Diagrammatic geological cross-section W–E through the town of Caen (cf. Fig. 2), showing principal aquifers. After Bigot (1932). Shallow boreholes are indicated in alluvium flooring the valley of the River Orne and in Quaternary loess (limon) as well as bedrock, with indication of original rest water level. Armorican basement is successively overlain by: the Lias (Lower Jurassic clays and subordinate limestones); ‘oolites’ (a unit 20–25 m thick, of Middle Jurassic Aalenian to Bajocian age, currently regionally described (Rioult et al. 1991) in terms of three formations: the Malière, 7–8 m of marly biomicrite with cherts and glauconite; overlain by Ferruginous Oolite, 0–2 m of fossiliferous condensed ironshot oolite; and Sponge Limestone, 8–20 m predominantly of ‘white oolite’ containing sponge spicules); the ‘blue bed’ (the current Port-en-Bessin Marl Formation, 8–28 m of early Bathonian marls alternating with limestones, a unit thickening westwards from Caen); the Caen Limestone Formation (fine biodetrital limestone). This is overlain regionally by cross-bedded bioclastic limestone, currently designated the Creully Formation, and by three similar formations which alternate with thin clayey limestones. This mid-late Bathonian limestone sequence is some 68–84 m in total thickness. Unit (b) contains the ‘Nappe Bajocienne’, (d) the ‘Nappe Vésulienne’, of Bigot (1932), cited in Table 2 herein as the Bajocian and Bathonian aquifers respectively. N.S. Robins et al. Quarterly Journal of Engineering Geology and Hydrogeology 2007;40:47-65 © 2007 The Geological Society of London

Map area from sheet 7E/5 Creully, a 1:50 000 scale water supply map prepared for a militarily significant area of Mid-Jurassic rocks. Map area from sheet 7E/5 Creully, a 1:50 000 scale water supply map prepared for a militarily significant area of Mid-Jurassic rocks. See Figure 1 for regional setting, legend based on marginalia. From an original map courtesy of the Lapworth Museum of Geology, but showing in addition sites of 10 boreholes, numbered as in Table 2. N.S. Robins et al. Quarterly Journal of Engineering Geology and Hydrogeology 2007;40:47-65 © 2007 The Geological Society of London

Map area from sheet 7F/1 Caen, a 1: 50 000 scale water supply map prepared for a militarily significant area of Mid-Jurassic rocks. Map area from sheet 7F/1 Caen, a 1: 50 000 scale water supply map prepared for a militarily significant area of Mid-Jurassic rocks. See Figure 1 for regional setting, legend based on marginalia. From an original map courtesy of the Lapworth Museum of Geology, but showing in addition sites of 9 boreholes, numbered as in Table 2. N.S. Robins et al. Quarterly Journal of Engineering Geology and Hydrogeology 2007;40:47-65 © 2007 The Geological Society of London

Map area plus legend from sheet 7F/4 Le Havre, a 1: 50 000 scale water supply map prepared late in the production sequence for a militarily significant area of Cretaceous rocks: see Figure 1 for regional setting and text for transcription of legend. Map area plus legend from sheet 7F/4 Le Havre, a 1: 50 000 scale water supply map prepared late in the production sequence for a militarily significant area of Cretaceous rocks: see Figure 1 for regional setting and text for transcription of legend. Courtesy of the Lapworth Museum of Geology. N.S. Robins et al. Quarterly Journal of Engineering Geology and Hydrogeology 2007;40:47-65 © 2007 The Geological Society of London

Map area, including legend, for sheet 9D/5 Dieppe, a 1: 50 000 scale water supply map prepared early in the production sequence for a significant port area of Cretaceous rocks: see Figure 1 for regional setting. Map area, including legend, for sheet 9D/5 Dieppe, a 1: 50 000 scale water supply map prepared early in the production sequence for a significant port area of Cretaceous rocks: see Figure 1 for regional setting. Courtesy of the Lapworth Museum of Geology. N.S. Robins et al. Quarterly Journal of Engineering Geology and Hydrogeology 2007;40:47-65 © 2007 The Geological Society of London

Map area, including legend, for sheet 49 Boulogne, a 1: 50 000 scale water supply map prepared early in the production sequence for a significant port area predominantly of Jurassic and Cretaceous rocks: see Figure 1 for regional setting. Map area, including legend, for sheet 49 Boulogne, a 1: 50 000 scale water supply map prepared early in the production sequence for a significant port area predominantly of Jurassic and Cretaceous rocks: see Figure 1 for regional setting. Courtesy of the Lapworth Museum of Geology. N.S. Robins et al. Quarterly Journal of Engineering Geology and Hydrogeology 2007;40:47-65 © 2007 The Geological Society of London

Map area of sheet 4 Havre-Amiens, an example of the 1: 250 000 scale water trace map series prepared by British military geologists in 1944: see Figure 1 for regional setting, Figure 7 for part of the area at more detailed scale. Map area of sheet 4 Havre-Amiens, an example of the 1: 250 000 scale water trace map series prepared by British military geologists in 1944: see Figure 1 for regional setting, Figure 7 for part of the area at more detailed scale. Courtesy of the Lapworth Museum of Geology. N.S. Robins et al. Quarterly Journal of Engineering Geology and Hydrogeology 2007;40:47-65 © 2007 The Geological Society of London