Problem: What is the full name of the person whose joke makes them laugh to them self? Answer the above question based on the context below: In 1935 England, Briony Tallis is a 13-year-old from a wealthy family. She has just completed writing her first play to mark her brother's homecoming and plans to stage it later that day with her visiting cousins. Looking out of her bedroom window, she spies on her older sister, Cecilia, and the housekeeper's son, Robbie Turner, on whom Briony has a crush. Cecilia is undressing and dips into the fountain pool; a moment later, she climbs out, her undergarments wet, all while Robbie watches. Cecilia had gone to the pond to fill a vase, Robbie grabbed one of the handles, and it broke. A part fell into the pond, and Cecilia jumped in to retrieve it, but to Briony, it looked as if Robbie had ordered Cecilia to undress and go under the water. Robbie drafts a series of notes to Cecilia apologizing for the incident, namely breaking the vase and laughing about it. One contains an explicit expression of his sexual desire for her, including frequent and crude usage of the word "cunt": he writes it only as a joke, and it makes him laugh to himself. He writes another, more formal letter, and asks Briony to deliver it. Only after she has gone does he realise he has given her the explicit letter. Briony reads the letter before giving it to Cecilia. Later, she describes it to her older visiting cousin, Lola, who calls Robbie a "sex maniac". Paul Marshall, a visiting friend of Briony's older brother's and a chocolate magnate, introduces himself to the visiting cousins and appears to be attracted to Lola. Before dinner, Robbie apologises for the obscene letter, but Cecilia surprises him and confesses her secret love for him. They then proceed to make passionate love in the library when Briony walks in, and thinks that Cecilia is under attack. Cecilia and Robbie try to pass the incident off.

A: Robbie Turner

Problem: Who wrote Marutratcharitamu? Answer the above question based on the context below: The Kannada poets and scholars of the empire produced important writings supporting the Vaishnava Bhakti movement heralded by the Haridasas (devotees of Vishnu), Brahminical and Veerashaiva (Lingayatism) literature. The Haridasa poets celebrated their devotion through songs called Devaranama (lyrical poems) in the native meters of Sangatya (quatrain), Suladi (beat based), Ugabhoga (melody based) and Mundige (cryptic). Their inspirations were the teachings of Madhvacharya and Vyasatirtha. Purandaradasa and Kanakadasa are considered the foremost among many Dasas (devotees) by virtue of their immense contribution. Kumara Vyasa, the most notable of Brahmin scholars wrote Gadugina Bharata, a translation of the epic Mahabharata. This work marks a transition of Kannada literature from old Kannada to modern Kannada. Chamarasa was a famous Veerashaiva scholar and poet who had many debates with Vaishnava scholars in the court of Devaraya II. His Prabhulinga Leele, later translated into Telugu and Tamil, was a eulogy of Saint Allama Prabhu (the saint was considered an incarnation of Lord Ganapathi while Parvati took the form of a princess of Banavasi).At this peak of Telugu literature, the most famous writing in the Prabandha style was Manucharitamu. King Krishnadevaraya was an accomplished Telugu scholar and wrote the celebrated Amuktamalyada. Amuktamalyada ("One who wears and gives away garlands") narrates the story of the wedding of the god Vishnu to Andal, the Tamil Alvar saint poet and the daughter of Periyalvar at Srirangam. In his court were eight famous scholars regarded as the pillars (Ashtadiggajas) of the literary assembly. The most famous among them were Allasani Peddana who held the honorific Andhrakavitapitamaha (lit, "father of Telugu poetry") and Tenali Ramakrishna, the court jester who authored several notable works. The other six poets were Nandi Thimmana (Mukku Timmana), Ayyalaraju Ramabhadra, Madayyagari Mallana, Bhattu Murthi (Ramaraja Bhushana), Pingali Surana, and Dhurjati. This was the age of...

A: Srinatha

Problem: What forms when geothermally heated water is emitted from deep sea hydrothermal vents? Answer the above question based on the context below: The seabed contains enormous reserves of minerals which can be exploited by dredging. This has advantages over land-based mining in that equipment can be built at specialised shipyards and infrastructure costs are lower. Disadvantages include problems caused by waves and tides, the tendency for excavations to silt up and the washing away of spoil heaps. There is a risk of coastal erosion and environmental damage. Seafloor massive sulphide deposits are potential sources of silver, gold, copper, lead and zinc and trace metals since their discovery in the 1960s. They form when geothermally heated water is emitted from deep sea hydrothermal vents known as "black smokers". The ores are of high quality but prohibitively costly to extract. Small scale mining of the deep sea floor is being developed off the coast of Papua New Guinea using robotic techniques, but the obstacles are formidable.There are large deposits of petroleum, as oil and natural gas, in rocks beneath the seabed. Offshore platforms and drilling rigs extract the oil or gas and store it for transport to land. Offshore oil and gas production can be difficult due to the remote, harsh environment. Drilling for oil in the sea has environmental impacts. Animals may be disorientated by seismic waves used to locate deposits, probably causing the beaching of whales. Toxic substances such as mercury, lead and arsenic may be released. The infrastructure may cause damage, and oil may be spilt.Large quantities of methane clathrate exist on the seabed and in ocean sediment at a temperature of around 2 C (36 F) and these are of interest as a potential energy source. Some estimates put the amount available at between one and 5 million cubic kilometres (0.24 to 1.2 million cubic miles). Also on the seabed are manganese nodules formed of layers of iron, manganese and other hydroxides around a core. In the Pacific these may cover up to 30 percent of the deep ocean floor. The minerals precipitate from seawater and grow very slowly. Their commercial extraction for...

A:
Seafloor massive sulphide deposits