[168]: Prof. Hughes' Geography of Cambridgeshire, p. 106.
[169]: See my Roman Britain, p. 266.
[170]: This "bush" is actually a group of young elms.
[174]: The Chantry Priests, of whom there were two in Barrington, often acted as village schoolmasters, the Chantries themselves serving as classrooms.
[175]: See p. [221]. The gravel here is older than that at Grantchester.
[176]: So called because full of green grains of "glauconite," which appear to be the internal casts of the shells of foraminifera. This bed, however, is not the true Upper Greensand, but "riddlings" from it.