Given a question and a context passage, generate the answer having the word or phrase from the context passage. Here, the answer should be a shortest continous span from the passage.

Input: Consider Input: Context: On November 13, 1982, 15-year-old Scott Safran of Cherry Hill, New Jersey, set a world record of 41,336,440 points on the arcade game Asteroids, beating the 40,101,910 point score set by Leo Daniels of Carolina Beach on February 6, 1982. In 1998, to congratulate Safran on his accomplishment, the Twin Galaxies Intergalactic Scoreboard searched for him for four years until 2002, when it was discovered that he had died in an accident in 1989. In a ceremony in Philadelphia on April 27, 2002, Walter Day of Twin Galaxies presented an award to the surviving members of Safrans family, commemorating the Asteroid Champions achievement. On April 5, 2010, John McAllister broke Safrans record with a high score of 41,838,740 in a 58-hour Internet livestream.
Question: Who had the highest score second playing Asteroids, Safran, Daniels or Mc Allister?

Output: safran

Input: Consider Input: Context: Earth formed at the same time as the other planets. The history of Earth is part of the history of the Solar System. Earth came together (accreted) from the cloud of dust and gas known as the solar nebula nearly 4.6 billion years ago, the same time the Sun and the rest of the solar system formed. Gravity caused small bodies of rock and metal orbiting the proto-Sun to smash together to create larger bodies. Over time, the planetoids got larger and larger until they became planets. When Earth first came together it was really hot, hot enough to melt the metal elements that it contained. Earth was so hot for three reasons: Gravitational contraction: As small bodies of rock and metal accreted, the planet grew larger and more massive. Gravity within such an enormous body squeezes the material in its interior so hard that the pressure swells. As Earths internal pressure grew, its temperature also rose. Radioactive decay: Radioactive decay releases heat, and early in the planets history there were many ra- dioactive elements with short half lives. These elements long ago decayed into stable materials, but they were responsible for the release of enormous amounts of heat in the beginning. Bombardment: Ancient impact craters found on the Moon and inner planets indicate that asteroid impacts were common in the early solar system. Earth was struck so much in its first 500 million years that the heat was intense. Very few large objects have struck the planet in the past many hundreds of millions of year. When Earth was entirely molten, gravity drew denser elements to the center and lighter elements rose to the surface. The separation of Earth into layers based on density is known as differentiation. The densest material moved to the center to create the planets dense metallic core. Materials that are intermediate in density became part of the mantle (Figure 1.1). Lighter materials accumulated at the surface of the mantle to become the earliest crust. The first crust was probably basaltic, like the oceanic crust is today. Intense heat from the early core drove rapid and vigorous mantle convection so that crust quickly recycled into the mantle. The recycling of basaltic crust was so effective that no remnants of it are found today. There is not much material to let us know about the earliest days of our planet Earth. What there is comes from three sources: (1) zircon crystals, the oldest materials found on Earth, which show that the age of the earliest crust formed at least 4.4 billion years ago; (2) meteorites that date from the beginning of the solar system, to nearly 4.6 billion years ago (Figure 1.2); and (3) lunar rocks, which represent the early days of the Earth-Moon system as far back as 4.5 billion years ago.
Question: which is not a reason why earth was molten in its early days?

Output: the sun

Input: Consider Input: Context: Fun, and maybe more Nickname: tatoosun Email: tatoosun2003@yahoo.com When to travel: Jun 2007 - Aug 2007 Who am I: Slender African girl in her late 20's. Quite charming, loving, pretty, fun to be with. My travel plans: Nothing in mind for sure, just looking to come with you. Who am I looking for: Looking for a white male between 40-50 years, someone who is full of energy and lively. When was this ad published: Nov 11 2006, Sat. 20yr old aussie looking for travel companion Nickname: Aly Email: alyssia _ europe@hotmail.com When to travel: May 2007 Who am I: a lovely girl, with fun, honest, caring. My travel plans: I will be traveling to Europe cities, then the world!! Whom am I looking for: An extremely fun and entertaining male / female, middle-aged. Someone that I can enjoy every travel moment with. When was this ad published: Nov 12, 2006, Sun *Just for fun Nickname: Queen Email: qrutta@yahoo.co.uk When to travel: Jan 2007 - Dec 2007 Who am I: Young slender girl, looking to see Asia with anyone who wants to travel. My travel plans: I most prefer a white man in his late 30's to have fun with me as he travels either on business or leisure trips. Whom am I looking for: someone who is kind, loving, honest, friendly, good sense of humor, adventurous. When was this ad published: Nov 6, 2006, Mon By Road Around the World Nickname: H N Solanki Email: ragwani@hotmail.com When to travel: May 2007-Aug 2007 Who am I: I am 55. From my childhood, have this dream to go around the world by hitch hiking. However this is now changed and I want to go by Road. My travel plans: Going throughout the world and studying various people, culture and habits. Whom am I looking for: A female companion, and she must have similar interest as me. When was this ad published: Oct 3 2006, Tue
Question: How will H N Solanki travel this time?
Output: by road