Problem: Given the following context: Immediately southeast of Mount Cayley lies Mount Fee, an extensively eroded volcano containing a north-south trending ridge. It has an elevation of 2,162 m (7,093 ft) and is one of the older volcanic features in the Mount Cayley volcanic field. Its volcanics are undated, but its large amount of dissection and evidence of glacial ice overriding the volcano indicates that it formed more than 75,000 years ago before the Wisconsinan Glaciation. Therefore, volcanism at Mount Fee does not display evidence of interaction with glacial ice. The remaining products from Fee's earliest volcanic activity is a minor portion of pyroclastic rock. This is evidence of explosive volcanism from Fee's eruptive history, as well as its first volcanic event. The second volcanic event produced a sequence of lavas and breccias on the eastern flank of the main ridge. These volcanics were likely deposited when a sequence of lava flows and broken lava fragments erupted from a volcanic vent and moved down the flanks during the construction of a large volcano. Following extensive dissection, renewed volcanism produced a viscous series of lava flows forming its narrow, flat-topped, steep-sided northern limit and the northern end of the main ridge. The conduit for which these lava flows originated from was likely vertical in structure and intruded through older volcanics deposited during Fee's earlier volcanic events. This volcanic event was also followed by a period of erosion, and likely one or more glacial periods. Extensive erosion following the last volcanic event at Mount Fee has created the rugged north-south trending ridge that currently forms a prominent landmark.Pali Dome, located north and northeast of Mount Cayley, is an eroded volcano in the central Mount Cayley volcanic field. Like Cauldron Dome, it consists of two geological units. Pail Dome East is composed of a mass of andesite lava flows and small amounts of pyroclastic material. It lies on the eastern portion of the Powder Mountain Icefield. Much of the lava flows form... answer the following question: What is the full name of the eroded volcano in the central Mount Cayley volcanic field?

A: Pali Dome

Problem: Given the question: Given the following context: In Waters' absence, Gilmour had been recruiting musicians for a new project. Months previously, keyboardist Jon Carin had jammed with Gilmour at his Hookend studio, where he composed the chord progression that became "Learning to Fly", and so was invited onto the team. Gilmour invited Bob Ezrin (co-producer of 1979's The Wall) to help consolidate their material; Ezrin had turned down Waters' offer of a role on the development of his new solo album, Radio K.A.O.S., saying it was "far easier for Dave and I to do our version of a Floyd record". Ezrin arrived in England in mid-1986 for what Gilmour later described as "mucking about with a lot of demos".At this stage, there was no commitment to a new Pink Floyd release, and Gilmour maintained that the material might become his third solo album. CBS representative Stephen Ralbovsky hoped for a new Pink Floyd album, but in a meeting in November 1986, told Gilmour and Ezrin that the music "doesn't sound a fucking thing like Pink Floyd". Gilmour later said that the new project was difficult without Waters. He experimented with songwriters such as Eric Stewart and Roger McGough, but eventually settled on Anthony Moore, who was credited as co-writer of "Learning to Fly" and "On the Turning Away". Whereas many prior Pink Floyd albums are concept albums, Gilmour settled for the more conventional approach of a collection of songs without a thematic link. By the end of that year, he had decided to make the material into a Pink Floyd project. answer the following question: What is the name of the person that owned the Hookend studio?
++++++++++++++++++++++++++++++++
The answer is:
Gilmour

[Q]: Given the following context: The Rokeby Venus (; also known as The Toilet of Venus, Venus at her Mirror, Venus and Cupid, or La Venus del espejo) is a painting by Diego Velazquez, the leading artist of the Spanish Golden Age. Completed between 1647 and 1651, and probably painted during the artist's visit to Italy, the work depicts the goddess Venus in a sensual pose, lying on a bed and looking into a mirror held by the Roman god of physical love, her son Cupid. The painting is in the National Gallery, London. Numerous works, from the ancient to the baroque, have been cited as sources of inspiration for Velazquez. The nude Venuses of the Italian painters, such as Giorgione's Sleeping Venus (c. 1510) and Titian's Venus of Urbino (1538), were the main precedents. In this work, Velazquez combined two established poses for Venus: recumbent on a couch or a bed, and gazing at a mirror. She is often described as looking at herself on the mirror, although this is physically impossible since viewers can see her face reflected in their direction. This phenomenon is known as the Venus effect. In a number of ways the painting represents a pictorial departure, through its central use of a mirror, and because it shows the body of Venus turned away from the observer of the painting.The Rokeby Venus is the only surviving female nude by Velazquez. Nudes were extremely rare in seventeenth-century Spanish art, which was policed actively by members of the Spanish Inquisition. Despite this, nudes by foreign artists were keenly collected by the court circle, and this painting was hung in the houses of Spanish courtiers until 1813, when it was brought to England to hang in Rokeby Park, Yorkshire. In 1906, the painting was purchased by National Art Collections Fund for the National Gallery, London. Although it was attacked and badly damaged in 1914 by the suffragette Mary Richardson, it soon was fully restored and returned to display. answer the following question: What is the first name of the person who combined two established poses for Venus: recumbent on a couch or a bed, and gazing at a mirror?
****
[A]:
Diego