Published online by Cambridge University Press: 01 May 2009
In the broad Alluvial tract which borders the Ouse between Oakley and Clapham, north of Bedford, there is a gravel-pit in which a small anticline of the Great Oolite was abruptly encountered amidst the regularly stratified river-deposits. The pit is situated immediately north of the Oakley road and east of the Midland Railway.
page 439 note 1 Read before the Meeting of the British Association, Cambridge, August, 1904.
page 440 note 1 See Kendall, P. F. Professor:“Eighth Report of Committee on Erratic Blocks of the British Isles,” Rep. Brit. Assoc. for 1903.Google Scholar