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Sediment dynamics in the Castleton karst, Derbyshire, U.K.
Author(s) -
Bottrell Simon,
Hardwick Paul,
Gunn John
Publication year - 1999
Publication title -
earth surface processes and landforms
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.294
H-Index - 127
eISSN - 1096-9837
pISSN - 0197-9337
DOI - 10.1002/(sici)1096-9837(199908)24:8<745::aid-esp8>3.0.co;2-l
Subject(s) - geology , karst , sedimentary depositional environment , sediment , geochemistry , clay minerals , cave , uranium , geomorphology , archaeology , structural basin , paleontology , materials science , metallurgy , history
Chemical and mineralogical data are presented for a suite of 59 sediment samples collected from the P8 and Speedwell cave systems (and mineralogical data are presented for a further six surface sediments) in the Castleton karst catchment, Derbyshire, England. Sediments are grouped according to age and depositional environment and these groups show distinctive mineralogical and chemical characteristics. Clay mineralogy is effective at distinguishing different sediment sources for ancient and modern sediments which are derived from pre‐Devensian tills and Devensian solifluction deposits, respectively. Major element chemistry reflects these differences in clay mineral content, while trace elements demonstrate the importance of abrasion of ore minerals in conduits in the aquifer which follow mineral veins, even under natural, pre‐mining conditions. Clay minerals are confirmed as the host for uranium in uranium‐rich ancient sediments. Consideration of organic carbon and hydrogen concentrations shows that plant material is the dominant source of organic material in the modern sediments. Copyright © 1999 John Wiley & Sons, Ltd.