Given a context passage, generate a question from the passage such that its answer is shortest continous span from the passage.

Q: The Rose Experience is the fourth studio album by multi-platinum R&B singer Case.

A: What is the name of the artist or group which originally performed The Rose Experience?
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Q: After tough losses at home, the Raiders traveled to Cleveland to take on the Browns. The Browns scored 9 straight points leading into the 2nd quarter when Billy Cundiff kicked 3 field goals from: 52 (in the 1st quarter), 33, and 26 yards out (in the 2nd quarter) for leads of 3-0, 6-0, and 9-0. The Raiders got on the board when Sebastian Janikowski kicked 2 field goals before halftime from 46 and 38 yards out for a 9-3 and then 9-6 game at halftime. After a scoreless 3rd quarter, the Browns got back to work in the 4th when Brian Hoyer found Andrew Hawkins on a 4-yard touchdown pass for a 16-6 lead followed by Ben Tate running in the end zone for a 5-yard touchdown for a 23-6 game. The Raiders wrapped up the scoring of the game later on when Derek Carr found Andre Holmes 10-yard touchdown pass for the final score: 23-13.

A: Which kicker had more total yards, Cundiff or Janikowski?
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Q: The Cold War helped scientists to learn more about our planet. They set up seismograph networks during the 1950s and early 1960s. The purpose was to see if other nations were testing atomic bombs. Of course, at the same time, the seismographs were recording earthquakes. The scientists realized that the earthquakes were most common in certain areas. In the oceans, they were found along mid-ocean ridges and deep sea trenches. Earthquakes and volcanoes were common all around the Pacific Ocean. They named this region the Pacific Ring of Fire (Figure 6.13). Earthquakes are also common in the worlds highest mountains, the Himalaya Mountains of Asia. The Mediterranean Sea also has many earthquakes. Earthquakes are used to identify plate boundaries (Figure 6.14). When earthquake locations are put on a map, they outline the plates. The movements of the plates are called plate tectonics. The lithosphere is divided into a dozen major and several minor plates. Each plate is named for the continent or ocean basin it contains. Some plates are made of all oceanic lithosphere. A few are all continental lithosphere. But Convection within the Earths mantle causes the plates to move. Mantle material is heated above the core. The hot mantle rises up towards the surface (Figure 6.16). As the mantle rises it cools. At the surface the material moves horizontally away from a mid-ocean ridge crest. The material continues to cool. It sinks back down into the mantle at a deep sea trench. The material sinks back down to the core. It moves horizontally again, completing a convection cell. Plate boundaries are where two plates meet. Most geologic activity takes place at plate boundaries. This activity includes volcanoes, earthquakes, and mountain building. The activity occurs as plates interact. How can plates interact? Plates can move away from each other. They can move toward each other. Finally, they can slide past each other. These are the three types of plate boundaries: Divergent plate boundaries: the two plates move away from each other. Convergent plate boundaries: the two plates move towards each other. Transform plate boundaries: the two plates slip past each other. The features that form at a plate boundary are determined by the direction of plate motion and by the type of crust at the boundary. Plates move apart at divergent plate boundaries. This can occur in the oceans or on land. Plates move apart at mid-ocean ridges. Lava rises upward, erupts, and cools. Later, more lava erupts and pushes the original seafloor outward. This is seafloor spreading. Seafloor spreading forms new oceanic crust. The rising magma causes earthquakes. Most mid-ocean ridges are located deep below the sea. The island of Iceland sits right on the Mid-Atlantic ridge (Figure 6.17). A divergent plate boundary can also occur within a continent. This is called continental rifting (Figure 6.18). Magma rises beneath the continent. The crust thins, breaks, and then splits apart. This first produces a rift valley. The East African Rift is a rift valley. Eastern Africa is splitting away from the African continent. Eventually, as the continental crust breaks apart, oceanic crust will form. This is how the Atlantic Ocean formed when Pangaea broke up. A convergent plate boundary forms where two plates collide. That collision can happen between a continent and oceanic crust, between two oceanic plates, or between two continents. Oceanic crust is always destroyed in these collisions. Oceanic crust may collide with a continent. The oceanic plate is denser, so it undergoes subduction. This means that the oceanic plate sinks beneath the continent. This occurs at an ocean trench (Figure 6.19). Subduction zones are where subduction takes place. As you would expect, where plates collide there are lots of intense earthquakes and volcanic eruptions. The subducting oceanic plate melts as it reenters the mantle. The magma rises and erupts. This creates a volcanic mountain range near the coast of the continent. This range is called a volcanic arc. The Andes Mountains, along the western edge of South America, are a volcanic arc (Figure 6.20). Two

A:
where two plates move away from each other
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