1
Book reviews Geology of the country around Hitchin (sheet memoir 221 (England and Wales» , P. M. Hopson, D. T. Aldiss and A. Smith, 1996, HMSO, London, xi + 153 pp. ISBN a II 8845 18 7 (PB), £55.00. The geological memoir for the Hitchin area is part of the increasing output of the British Geological Survey. New memoirs are appearing much more rapidly than they used to after the publication of the geological map for an area, often within a year or two. Inside the front cover there is a useful summary of the geological succession and the thicknesses of the units in the Hitchin District. The first chapter describes the geographi- cal setting, and summarizes the history of research along with a brief geological history of the area. The solid forma- tions, when exposed at the surface, range from the Lower Cretaceous Woburn Sands and Gault in Bedfordshire to the northwest, though the Upper Cretaceous Chalk sequence which underlies northern Hertfordshire to the small Tertiary outliers in the southeast of the map. On top of these solid formations large parts of the area are covered by much younger Quaternary drift deposits. The next chapter is on the concealed formations beneath the district with the borehole and geophysical evidence for the nature of the Jurassic and Palaeozoic formations with, at depth, the Precambrian rocks of the Midlands Microcraton. There is a useful table of the physical properties of the main rock units along with plots of the geology and level of the Pre-De vonian and Permian surfaces. The chapter on the Lower Cretaceous formations adds to the information on the subject in the 1994 memoir for the adjacent Leighton Buzzard sheet, with some useful tables and figures - surprising, considering the poor and limited area of their outcrop. A large amount of information is contained in the chapter on the Chalk. The old lower, middle and upper subdivisions have been kept, because the resistant Melbourn rock at the base of the Middle Chalk and the Chalk Rock at the base of the Upper Chalk form positive topographic features that can be traced durin g field mapping . There is a good discussion of the Cambridge Greensand that is now considered to form the base of the Lower Chalk, along with all the other units of the Chalk sequence. After general descriptions there are very detailed notes and diagrams for many locations in the district. The short chapter on the Tertiary beds includes the results of a borehole drilled to help with the surveying of these outlying deposits and their relationship to those in the rest of the London Basin and beyond. Proceedings of the Geologists ' Association . 109, 159-1 60. The chapter on the Quaternary is very extensive and is divided into Pre-Anglian, Anglian and Post-Anglian sections. The Letchworth Gravel is described for the first time, and it is suggested that it was deposited by a Pre- Anglian stream drainin g southward through the Hitchin Gap into the Thames Basin. The glaciotectonic Chalk rafts of the Barkway and Therfield area south of Royston are described in terms of the Anglian ice impin ging on the Chalk escarp- ment, and this section complements the recent paper by Hopson (1995). The sequence of events in the glacial history of the Hitchin Gap is set out in a series of clear diagrams along with descriptions of the material filling the channels. The chapter on structure starts with geophysical and satellite lineament s which seem to reveal very little about the surface geology but suggest possibilities about the nature of the basement rocks below the area. In the Chalk a northwest-trending fault along Lilley Bottom intersecting the Chalk escarpment at Barton-Ie-Clay is suggested, though it could be a monoclinal roll, and it has not been marked on the published 1:50 000 geological map. At the end of the chapter there is a good detailed map showing the faultin g of the Melbourn Rock at the base of the Midd le Chalk ju st to the west of Hitchin. The economic geology chapter has an interesting section on the exploitation of the Cambridge Greensand for calcium phosphate, with a note that John Lawes made a fortune from this and as a result found ed Rotham sted Experiment al Station . There is a table of all the known landfill sites in the area and what they are filled with, along with a note on the generation of landfill gas at Arlesey by rotting household waste. The hydrology of the area is discussed in some detail, along with the problems of aquifer pollution. Overall, the Hitchin memoir contain s a surprising amount of well set out information, much of which was collected in the recent survey of the area, but at £55.00 it is far too expensive. It is a great pity that excellent memoirs such as this, as a result of the government's forcing near-market economics on the BGS, have to be priced at such a high level, becau se they will have a much more limited public circulation than they deserve . REFERENCE HOPSON, P. M. 1995. Chalk raft s in Anglian till in north Hertfordshire, Proceedings of the Geologists ' Association, 106. 151- 8. DAVID NOWELL 2 Tudor Road, New Barnet, Hens 0016-7878/98 $10·00 © 1998 Geologists' Association

P.M. Hopson, D.T. Aldiss, A. Smith,Editors, , Geology of the country around Hitchin (sheet memoir 221 (England and Wales)) (1996) HMSO,London xi + 153 pp. ISBN 0 11 884518 7 (PB),

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Page 1: P.M. Hopson, D.T. Aldiss, A. Smith,Editors, , Geology of the country around Hitchin (sheet memoir 221 (England and Wales)) (1996) HMSO,London xi + 153 pp. ISBN 0 11 884518 7 (PB),

Book reviews

Geology of the country around Hitchin (sheet memoir 221(England and Wales» , P. M. Hopson, D. T. Aldiss and A.Smith, 1996, HMSO, London, xi + 153 pp. ISBN a II8845 18 7 (PB), £55.00.

The geo logica l memoir for the Hitchin area is part of theincreasing output of the British Geological Survey. Newmemoirs are appearing much more rapidly than they used toafter the publication of the geological map for an area, oftenwithin a year or two.

Inside the front cover there is a useful summary of thegeological succession and the thicknesses of the units in theHitchin District. The first chapter describes the geographi­cal setting, and summarizes the history of research alongwith a brief geological history of the area . The solid forma­tions, when exposed at the surface, range from the LowerCretaceous Woburn Sands and Gault in Bedfordshire to thenorthwest, though the Upper Cretaceo us Chalk sequencewhich underlies northern Hertfordshire to the small Tertiaryoutliers in the southeast of the map. On top of these solidformations large parts of the area are covered by muchyounger Quaternary drift deposits.

The next chapter is on the concealed formations beneaththe district with the boreho le and geophysica l evidence forthe nature of the Jurassic and Palaeozoic formations with, atdepth , the Precambrian rocks of the Midlands Microcraton.There is a useful table of the physical propert ies of the mainrock units along with plots of the geology and level of thePre-De vonian and Permian surfaces.

The chapter on the Lower Cretaceous formations adds tothe information on the subject in the 1994 memoir for theadjacent Leighton Buzzard sheet, with some useful tablesand figures - surprising, considering the poor and limitedarea of their outcrop.

A large amount of information is contained in the chapteron the Chalk. The old lower, middle and upper subdivisionshave been kept, because the resistant Melbourn rock at thebase of the Middle Chalk and the Chalk Rock at the base ofthe Upper Chalk form positive topographic features that canbe traced during field mapping . There is a good discussionof the Cambridge Greensand that is now considered to formthe base of the Lower Chalk, along with all the other unitsof the Chalk sequence. After general descriptions there arevery detailed notes and diagrams for many locations in thedistrict.

The short chapter on the Tertiary beds includes the resultsof a borehole drilled to help with the surveying of theseout lying deposits and their relationship to those in the restof the London Basin and beyond.

Proceedings of the Geologists ' Association . 109, 159-1 60.

The chapter on the Quaternary is very extensive and isdivided into Pre-Anglian , Anglian and Post-An gliansections. The Letchworth Gra vel is described for the firsttime, and it is suggested that it was deposited by a Pre­Anglian stream drainin g southward through the Hitchin Gapinto the Thames Basin. The glaciotectonic Chalk rafts of theBarkway and Therfield area south of Royston are describedin terms of the Anglian ice impin ging on the Chalk escarp­ment , and this section complements the recent paper byHopson (1995). The sequence of events in the glacialhistory of the Hitchin Gap is set out in a series of cleardiagrams along with descriptions of the material filling thechannels.

The chapter on structure starts with geophysical andsatellite lineament s which seem to reveal very little aboutthe surface geology but suggest possibil ities about thenature of the basement rocks below the area. In the Chalk anorthwest-trend ing fault along Lilley Bottom inter sectingthe Chalk escarpment at Barton-Ie-Clay is suggested,though it could be a monoclinal roll, and it has not beenmarked on the published 1:50 000 geological map. At theend of the chapter there is a good detailed map show ing thefaultin g of the Melbourn Rock at the base of the Midd leChalk ju st to the west of Hitchin.

The economic geology chapter has an interesting sectionon the exploitation of the Cambridge Greensand for calciumphosphate, with a note that John Lawes made a fortune fromthis and as a result founded Rothamsted Experiment alStation . There is a table of all the known landfill sites in thearea and what they are filled with , along with a note on thegeneration of landfill gas at Arlesey by rotting householdwaste. The hydrology of the area is discussed in somedetai l, along with the problems of aquifer pollution.

Overall, the Hitchin memoir contains a surprising amountof well set out information, much of which was collected inthe recent survey of the area, but at £55 .00 it is far tooexpensive. It is a great pity that excellent memoirs such asthis, as a result of the government's forcin g near-marketeconomics on the BGS, have to be priced at such a highlevel, becau se they will have a much more limited publiccirculation than they deserve .

REFERENCEHOPSON, P. M. 1995. Chalk raft s in Anglian till in north

Hertfordshire, Proceedings of the Geologists ' Association, 106.151- 8.

DAVID NOWELL2 Tudor Road, New Barnet , Hens

0016-7878/98 $ 10·00 © 1998 Geologists ' Associa tion