No CrossRef data available.
Published online by Cambridge University Press: 01 May 2009
In 1891, Frank S. Goodwin, Esq., of Bakewell, Derbyshire, presented to the British Museum (Natural History) a pair of antlers of red-deer, with fragments of the calvarium attached, which had been obtained, with other cervine remains, from a tufaceous deposit of comparatively modern date near Bakewell, Derbyshire.
page 50 note 1 Tuft (tufa) is a stone formed by the (calcareous) deposit left by water passing through beds of sticks, roots, vegetables, etc., of which there is a large stratum at Matlock Bath,inthis county.
page 51 note 1 See also “British Deer and their Horns,” by Millais, J. G., p. 96, fig. 2, and p. 105. (Roy. 4to; Sotheran & Co., 1897.)Google Scholar