By M. R. Smith, G. West, P. G. Fookes, J. Lay, I. Sims, L. Collis
In 1985, the Geological Society released Aggregates because the first quantity in its Engineering Geology detailed booklet sequence. It met with instant acclaim, being presented the Brewis Trophy by means of SAGA in 1986 and drawing the subsequent evaluate from the Canadian Geotechnical magazine in 1988: This ebook is normally a well-researched, informative and worthwhile consultant to the site, sampling and trying out of aggregates. in case your paintings comprises using aggregates, purchase this ebook and browse no additional; this quantity can be a necessary and worthwhile reference that you'll use for a few years. In 1989, the operating occasion whose paintings had ended in the book of Aggregates was once reconvened to revise, replace and expand their document. each one bankruptcy used to be reviewed through self sufficient referees. the second one and significantly stronger variation, released in 1993 and reprinted in 1998, represented the distillation of an unlimited physique of data and adventure held not just through the participants of the operating social gathering, but in addition via many foreign specialists, scientists and engineers who contributed as reviewers, referees and corresponding authors. additionally to be had: ordinary Stone, Weathering Phenomena, Conservation recommendations and Case reports - ISBN 1862391238 construction Stone Decay: From prognosis to Conservation - detailed e-book no 271 (Geological Society distinctive booklet) - ISBN 1862392188 The Geological Society of LondonFounded in 1807, the Geological Society of London is the oldest geological society on the earth, and one of many greatest publishers within the Earth sciences.The Society publishes a variety of top of the range peer-reviewed titles for teachers and execs operating within the geosciences, and enjoys an enviable foreign attractiveness for the standard of its work.The many components during which we post in include:-Petroleum geology-Tectonics, structural geology and geodynamics-Stratigraphy, sedimentology and paleontology-Volcanology, magmatic stories and geochemistry-Remote sensing-History of geology-Regional geology publications
Read or Download Aggregates: Sand, Gravel and Crushed Rock Aggregates for Construction Purposes, 3rd Edition (Geological Society Engineering Geology Special Pub. No.17) PDF
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Additional info for Aggregates: Sand, Gravel and Crushed Rock Aggregates for Construction Purposes, 3rd Edition (Geological Society Engineering Geology Special Pub. No.17)
2. Much of the crushed igneous rock aggregates in Britain is produced from fine- to medium-grained basic rocks (dolerite and basalt) and, to a lesser extent, from fine-grained acidic rocks (felsite, porphyry and microgranite); increasing amounts come from certain of the coarse-grained rocks (granite and diorite) worked in large quarries. Many quarries are, however, located in small intrusions of dolerite and basalt, for example in Wales and the Welsh Borders, in Devon, and in the Carboniferous Limestone of the Pennines in Derbyshire.
Repeated freezing and thawing breaks off flakes and fragments from exposed rock surfaces by 'icewedging' in fractures and joints and by inducing differential movements in the rock mass. The mechanical disintegration of rocks in upland areas may produce large amounts of predominantly angular rock debris or talus. In the absence of running water and where slopes are steep, large-scale accumulations of debris near to the angle of rest (screes) may provide a ready source of coarse aggregate material, though it must be remembered that it may have been adversely affected by long exposure to weathering and any disturbance by working may render the loose material unstable and therefore hazardous.
The main occurrences and centres of extraction (Ashworth 1975) are in the Mendip Hills (Quarry Management and Products 1975; A1-Jassar & Hawkins 1991), around the northern rim of the Bristol coalfield, in the uplands at the periphery of the South Wales coalfield and in North Wales, in the Derbyshire Dome (Harrison & Adlam 1984), on the borders of the Lake District, in North Yorkshire and Lancashire and to a minor extent in Scotland. In the north Pennines, several thin limestone beds are interbedded with soft sandstone and shale (Yoredale facies).