Letteratura scientifica selezionata sul tema "Guildford Cathedral, Guildford, Eng"

Philip Moore (b. 1943) has had a distinguished career as a cathedral musician, organist and, increasingly in recent years, as a composer. He began his career as a music master at Eton College and subsequently held a number of important positions, firstly at Canterbury and Guildford Cathedrals and latterly as Master of the Music at York Minster (1983–2008). His impressive catalogue of 400 works contains a substantial body of church music, but he has also written instrumental music and some larger works with orchestra including an organ concerto. His music draws on a wide sphere of influences with a strong tilt towards Vaughan Williams, Howells and Britten, plainchant and Duruflé and those whom he regards as the great classical architects of music: Bach, Brahms, Mozart and Hindemith amongst many others. On 20 November 2010 his new cantata Ode to St Cecilia was premièred in Guildford Cathedral. The composer has said that the genesis and design of the work derives from Britten's St Nicholas to which he hopes it will be seen as complementary. This interview took place in October 2009 before a recital devoted entirely to Moore's organ music at St Paul's Cathedral in London.

AbstractThe University of Surrey is situated on the northern slopes of Stag Hill, below Guildford Cathedral, which occupies the summit. During the investigation for the design of the University, it became apparent that the site was underlain by a large landslip, 500 m wide from east to west and extending 160 m from rear scarp to toe. Considerable effort was made to establish its geometry and extent (Skempton & Petley (1967), and Morgenstern & Tchalenko (1967)).In recent years it was realised that because the construction of the Cathedral extended over a long period of time, the likelihood of Stag Hill being covered by oblique aerial photography would be high. Some forty oblique aerial photographs, spanning the period 1949 to 1982, were collected and analysed together with vertical aerial photographs and topographic maps.Although the landslip is visible on vertical aerial photographs, individual elements are not easily identified. Using oblique photography, in particular that in which recognition of subdued topography has been enhanced by low sun angles, up to six phases of landslipping were identified.This paper uses this example to demonstrate the usefulness of aerial photography in site investigation and in particular the value of oblique photography, a topic which receives little attention in BS 5930:1981 considering how cost effective this tool can be.