The works of William Hogarth : with descriptions and explanations /

Mode of access: Internet.

William Hogarth,

"A catalogue of paintings by, or attributed to, Hogarth": p. [327]-352.

The works of William Hogarth : (including the 'Analysis of beauty,') elucidated by descriptions, critical, moral, and historical; (founded on the most approved authorities.) To which is prefixed Some account of his life /

"The analysis of beauty" has special t.-p.

William Hogarth;

Appendix IV: The literary remains of "Ald Hoggart," the painter's uncle, p. 206-209.

Hogarth,

Mode of access: Internet.

Hogarth's works : with life and anecdotal descriptions of his pictures /

Mode of access: Internet.

Hogarth /

Includes index.

Hogarth illustrated from his own manuscripts;

Mode of access: Internet.

W. Hogarth's Zeichnungen : nach den Originalen in Stahl gestochen /

"William Hogarth's Zeichnungen, mit der vollständigen Erklärung von Dr. Franz Kottenkamp."--T.p., vol. 2.

English humorists of the eighteenth century : Sir Richard Steele, Joseph Addison, Laurence Sterne, Oliver Goldsmith /

"With introductions from Thackeray's English humorists'."

Thesaurus graecae poese[o]s siue Lexicon graeco-prosodiacum ; versus, et synonyma ... epitheta, phrases, descriptiones, etc ... De poesi, seu prosodia graecorum tractatus /

Mode of access: Internet.

Sketches of the principal picture-galleries in England, with a criticism on "Marriage a-la-mode.".

Published anonymously. By William Hazlitt. Cf. Halkett and Laing.

The analysis of beauty, written with a view of fixing the fluctuating ideas of taste.

Paging of 1st ed. (1753) printed in margins: xxii, 153 p.

Works complete.

Mode of access: Internet.

Drying front in a sloping aquifier: nonlinear effects

The profiles for the water table height h(x, t) in a shallow sloping aquifer are reexamined with a solution of the nonlinear Boussinesq equation. We demonstrate that the previous anomaly first reported by Brutsaert [1994] that the point at which the water table h first becomes zero at x = L at time t = t c remains fixed at this point for all times t > t c is actually a result of the linearization of the Boussinesq equation and not, as previously suggested [ Brutsaert, 1994 ; Verhoest and Troch, 2000 ], a result of the Dupuit assumption. Rather, by examination of the nonlinear Boussinesq equation the drying front, i.e., the point x f at which h is zero for times t ≥ t c , actually recedes downslope as physically expected. This points out that the linear Boussinesq equation should be used carefully when a zero depth is obtained as the concept of an “average” depth loses meaning at that time.