Hostname: page-component-586b7cd67f-rcrh6 Total loading time: 0 Render date: 2024-11-27T21:50:41.646Z Has data issue: false hasContentIssue false

On River Sand from the Ure and the Ouse above York

Published online by Cambridge University Press:  01 May 2009

Extract

The sand described in the following notes was dredged from the mid-channel of the river at the following places:—Swale Nab, Dunsforth, Aldwark Bridge, below Linton Lock, and Beningbrough. Two samples were also obtained from the Nidd at points 100 and 200 yards respectively from its confluence with the Ouse. For comparative purposes sand from the banks and alluvial flat of the Swale above Ainderby Steeple is likewise included.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1926

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

1 Lewis, H. P., “The Occurrence of Detrital Barytes in the Permian Basal Sand at Nitticarhill”: Geol. Mag., Vol. LX, 1923, p. 307. H. C. Versey, “The Beds Underlying the Magnesian Limestone in Yorkshire”: Proc. Yorks. Geol. Soc., vol. xx, 1925, p. 200.CrossRefGoogle Scholar