Problem: This article: Sir Osbert Lancaster, CBE (4 August 1908 27 July 1986) was an English cartoonist, architectural historian, stage designer and author. He was known for his cartoons in the British press, and for his lifelong work to inform the general public about good buildings and architectural heritage. The only child of a prosperous family, Lancaster was educated at Charterhouse School and Lincoln College, Oxford, at both of which he was an undistinguished scholar. From an early age he was determined to be a professional artist and designer, and studied at leading art colleges in Oxford and London. While working as a contributor to The Architectural Review in the mid-1930s, Lancaster published the first of a series of books on architecture, aiming to simultaneously amuse the general reader and demystify the subject. Several of the terms he coined as labels for architectural styles have gained common usage, including "Pont Street Dutch" and "Stockbrokers' Tudor", and his books have continued to be regarded as important works of reference on the subject. In 1938 Lancaster was invited to contribute topical cartoons to The Daily Express. He introduced the single column-width cartoon popular in the French press but not until then seen in British papers. Between 1939 and his retirement in 1981 he drew about 10,000 of these "pocket cartoons", which made him a nationally known figure. He developed a cast of regular characters, led by his best-known creation, Maudie Littlehampton, through whom he expressed his views on the fashions, fads and political events of the day. From his youth, Lancaster wanted to design for the theatre, and in 1951 he was commissioned to create costumes and scenery for a new ballet, Pineapple Poll. Between then and the early 1970s he designed new productions for the Royal Ballet, Glyndebourne, D'Oyly Carte, the Old Vic and the West End. His productivity declined in his later years, when his health began to fail. He died at his London home in Chelsea, aged 77. His diverse career, honoured by a ... contains an answer for the question: What is the last name of the person who studied at leading art colleges in Oxford and London?, what is it ?

A: Lancaster

Problem: Given the question: This article: The college presents a symmetrical front to New Road and the castle mound, with four small gables between a larger gable at either end. There are two quadrangles, with steps leading down from the upper quadrangle (to the east) to the lower quadrangle (to the west). Residential accommodation for students and fellows is located in the lower quadrangle, whilst the hall, library, and administrative offices are in the upper quadrangle. The buildings are two storeys high, with dormers above. There are pools in the centre of the quadrangles (the one in the lower quadrangle is the longer of the two); the writer Simon Jenkins said that these are "almost puddles", and saw them as relics of Harrison's Mediterranean plan. The writer Peter Sager, however, thought that the pond represents the canal basin that previously occupied the site. The main entrance leads into the upper quadrangle, which has the hall on its east side. The square-mullioned windows facing the quadrangles are arranged in close-set groups of three; at the east end of the upper quadrangle, the common room has a larger bay window. An abstract sculpture by Hubert Dalwood, from 1962, has been positioned on the lawn inside the college. Dalwood also designed the fountain in the pool in the upper quadrangle, although his plan for a spray of water was not implemented, "leaving the sculpture with no obvious purpose". The hall has a floor of black and white marble and arches made of concrete supporting an oak roof with red panels. The furniture in the hall was designed by, and the chairs were built by, Edward Barnsley. Lord Nuffield's coat of arms are displayed over the fireplace, carved from a single piece of stone, and his portrait, painted by Sir Arthur Cope, hangs in the hall. The chapel, on the south side of the college, can seat forty people. It has five abstract stained glass windows that were designed by John Piper and executed by Patrick Reyntiens, and a metal reredos with a bronze crucifix. The roofs are finished with Collyweston stone slates from... contains an answer for the question: What is the full name of the person whose portrait was painted by Sir Arthur Cope?, what is it ?
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The answer is:
Lord Nuffield

[Q]: This article: An unconformity of 15 to 20 million years separates the Supai Group from the previously deposited Redwall Formation. Supai Group was deposited in late Mississippian, through the Pennsylvanian and into the early Permian time, some 320 million to 270 million years ago. Both marine and non-marine deposits of mud, silt, sand and calcareous sediments were laid down on a broad coastal plain similar to the Texas Gulf Coast of today. Around this time, the Ancestral Rocky Mountains rose in Colorado and New Mexico and streams brought eroded sediment from them to the Grand Canyon area.Supai Group formations in the western part of the canyon contain limestone, indicative of a warm, shallow sea, while the eastern part was probably a muddy river delta. This formation consists of red siltstones and shale capped by tan-colored sandstone beds that together reach a thickness of 600 to 700 ft (around 200 m). Shale in the early Permian formations in this group were oxidized to a bright red color. Fossils of amphibian footprints, reptiles, and plentiful plant material are found in the eastern part and increasing numbers of marine fossils are found in the western part.Formations of the Supai Group are from oldest to youngest (an unconformity is present at the top of each): Watahomigi (see 5a in figure 1) is a slope-forming gray limestone with some red chert bands, sandstone, and purple siltstone that is 100 to 300 feet (30 to 90 m) thick. Manakacha (see 5b in figure 1) is a cliff- and slope-forming pale red sandstone and red shale that averages 300 feet (90 m) thick in Grand Canyon. Wescogame (see 5c in figure 1) is a ledge- and slope-forming pale red sandstone and siltstone that is 100 to 200 feet (30 to 60 m) thick. Esplanade (see 5d in figure 1) is a ledge- and cliff-forming pale red sandstone and siltstone that is 200 to 800 feet (60 to 200 m) thick. An unconformity marks the top of the Supai Group. contains an answer for the question: What time period of time did the Ancestral Rocky Mountains rise?, what is it ?
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[A]:
early Permian