instruction:
In this task, you're expected to write answers to questions involving multiple references to the same entity. The answer to the question should be unambiguous and a phrase in the paragraph. Most questions can have only one correct answer.
question:
Passage: Much of the court martial testimony was critical of Bligh's conduct—by the time of his return to England in August 1793, following his successful conveyance of breadfruit to the West Indies aboard Providence, professional and public opinion had turned against him. He was snubbed at the Admiralty when he went to present his report, and was left on half pay for 19 months before receiving his next appointment. In late 1794 the jurist Edward Christian, brother of Fletcher, published his Appendix to the court martial proceedings, which was said by the press to "palliate the behaviour of Christian and the Mutineers, and to criminate Captain Bligh". Bligh's position was further undermined when the loyalist gunner Peckover confirmed that much of what was alleged in the Appendix was true.Bligh commanded HMS Director at the Battle of Camperdown in October 1797 and HMS Glatton in the Battle of Copenhagen in April 1801. In 1805 while commanding HMS Warrior, he was court-martialled for using bad language to his officers, and reprimanded. In 1806, he was appointed Governor of New South Wales in Australia; after two years a group of army officers arrested and deposed him in the Rum Rebellion. After his return to England, Bligh was promoted to rear-admiral in 1811 and vice-admiral in 1814, but was not offered further naval appointments. He died, aged 63, in December 1817.Of the pardoned mutineers, Heywood and Morrison returned to naval duty. Heywood acquired the patronage of Hood and, by 1803 at the age of 31, had achieved the rank of captain. After a distinguished career, he died in 1831. Morrison became a master gunner, and was eventually lost in 1807 when HMS Blenheim foundered in the Indian Ocean. Muspratt is believed to have worked as a naval steward before his death, in or before 1798. The other principal participants in the court martial—Fryer, Peckover, Coleman, McIntosh and others—generally vanished from the public eye after the closing of the procedures. 
Question: What is the last name of the person who died at 63?
answer:
Bligh.


question:
Passage: Wheeler spent three months in the Dominion of Pakistan during early 1949, where he was engaged in organising the fledgling Pakistani Archaeological Department with the aid of former members of the Archaeological Survey and new students whom he recruited. The Minister of Education, Fazlur Rahman, was sympathetic to Wheeler's plans, and the government agreed to establish a National Museum of Pakistan in Karachi, which opened in April 1950. Wheeler himself was appointed the first President of the Pakistani Museums Association, and found himself as a mediator in the arguments between India and Pakistan over the redistribution of archaeological and historic artefacts following the partition. He also wrote a work of archaeological propaganda for the newly formed state, Five Thousand Years of Pakistan (1950).To instruct new Pakistani students in the methods of archaeology, in early 1950 Wheeler ran a training excavation at Mohenjo-daro; there, he was joined by the British student Leslie Alcock, who spoke both Punjabi and Urdu and who was appointed a site supervisor by Wheeler. This excavation proved to be the only one for which Wheeler would not write and publish a full excavation report. Instead, he made reference to its findings in his book The Indus Civilization, published as part of the series The Cambridge History of India. His relationship with the Pakistani government had become strained, and so he declined to return to work for them for a third year.Wheeler had been keen to return to excavation in Britain. Based on the one he had organised in India, Wheeler developed an archaeological training course, which he ran at Verulamium in the summer of 1949 to instruct British students in the methodologies of excavation. In summer 1950, he was invited by the Royal Commission on Historical Monuments to direct a trial excavation at Bindon Hill in Dorset. It was a leisurely project which he treated as a seaside holiday. He was invited by the Ancient Monuments Department of the Ministry of Works to excavate the Stanwick Iron Age Fortifications in North Riding, Yorkshire, which he proceeded to do over the summers of 1951 and 1952. Aided by many old friends and colleagues from within the British archaeological scene, he was joined by Alcock and Alcock's wife, among others. Wheeler published his report on the site in 1954.In 1949 Wheeler was appointed Honorary Secretary of the British Academy after Frederic G. Kenyon stepped down from the position. According to Piggott, the institution had "unhappily drifted into senility without the excuse of being venerable", and Wheeler devoted much time attempting to revitalise the organisation and ensured that Charles Webster was appointed President. Together, Wheeler and Webster sought to increase the number of younger members of the Academy, increasing the number of Fellows who were permitted to join and proposing that those over 75 years of age not be permitted to serve on the organisation's council; this latter measure was highly controversial, and though defeated in 1951, Wheeler and Webster were able to push it through in 1952. In doing so, Piggott stated, Wheeler helped rid the society of its "self-perpetuating gerontocracy". To aid him in these projects, Wheeler employed a personal assistant, Molly Myers, who remained with him for the rest of his life. 
Question: Which excavation did Wheeler make reference to in his book The Indus Civilization?
answer:
Mohenjo-daro.


question:
Passage: To have reached its enormous size within its relatively short (geologically speaking) 600,000 to 1,000,000 years of life, Mauna Loa would logically have had to have grown extremely rapidly through its developmental history, and extensive charcoal-based radiocarbon dating (perhaps the most extensive such prehistorical eruptive dating on Earth) has amassed a record of almost two hundred reliably dated extant flows confirming this hypothesis.The oldest exposed flows on Mauna Loa are thought to be the Ninole Hills on its southern flank, subaerial basalt rock dating back approximately 100 to 200 thousand years. They form a terrace against which younger flows have since banked, heavily eroded and incised against its slope in terms of direction; this is believed to be the result of a period of erosion because of a change in the direction of lava flow caused by the volcano's prehistoric slump. These are followed by two units of lava flows separated by an intervening ash layer known as the Pāhala ash layer: the older Kahuka basalt, sparsely exposed on the lower southwest rift, and the younger and far more widespread Kaʻu basalt, which appear more widely on the volcano. The Pāhala ashes themselves were produced over a long period of time circa 13 to 30 thousand years ago, although heavy vitrification and interactions with post and pre- creation flows has hindered exact dating. Their age roughly corresponding with the glaciation of Mauna Loa during the last ice age, raising the distinct possibility that it is the product of phreatomagmatic interaction between the long-gone glaciers and Mauna Loa's eruptive activities.Studies have shown that a cycle occurs in which volcanic activity at the summit is dominant for several hundred years, after which activity shifts to the rift zones for several more centuries, and then back to the summit again. Two cycles have been clearly identified, each lasting 1,500–2,000 years. This cyclical behavior is unique to Mauna Loa among the Hawaiian volcanoes. Between about 7,000 and 6,000 years ago Mauna Loa was largely inactive. The cause of this cessation in activity is not known, and no known similar hiatus has been found at other Hawaiian volcanoes except for those currently in the post-shield stage. Between 11,000 and 8,000 years ago, activity was more intense than it is today. However, Mauna Loa's overall rate of growth has probably begun to slow over the last 100,000 years, and the volcano may in fact be nearing the end of its tholeiitic basalt shield-building phase. 
Question: What is the name of the volcano whose prehistoric slump caused a change in the direction of lava flow resulting in a period of erosion?
answer:

Mauna Loa.