Former Long Beach Executive Director Toby Rothschild, now a policy wonk in Iwasaki's outfit, agreed. "To some extent, I did look at it and say, 'We are the littlest kid on the block, and we don't want to get beat up so we need a bigger protector,'" Rothschild said. "Once we got past that, it became a real positive for the Long Beach program and Long Beach clients." But to the San Gabriel-Pomona Valley legal aid program, the positives of merging with Dudovitz's program, San Fernando Valley Neighborhood Legal Services, were never obvious. A meeting in late 1999 between Dudovitz and the San Gabriel-Pomona Valley program's board showed how little the two programs had in common and how difficult bridging the gap between their ideologies would be, Dudovitz recalled. Although no merger plans were discussed, board members at the smaller program knew of Dudovitz's preference for impact litigation over direct services. "We had a discussion about what our separate views were," Dudovitz said. "The message we got was that they wanted their program to stay as it was." Lauralea Saddick, former executive director of the San Gabriel-Pomona Valley program, said her board simply did not share Dudovitz's desire to spend money influencing social policy and participating in high-profile litigation over poverty-related issues. "Our board's philosophy was that the money given by the federal government was to help people with basic everyday needs," Saddick said. "It might take a little bit of humility to take those kinds of cases. Impact work is very important ... but what was the good of getting the law changed if no one is there to help the individual?" Before the San Gabriel program was subsumed by Dudovitz's group, it offered to merge with the Legal Aid Society of Orange County. The boards of both organizations eschewed impact litigation in favor of the 1960s model of providing direct client services. Supported by resolutions from the Pasadena, San Gabriel, Eastern and Foothill bar associations, the two programs drew up plans to merge and submitted them to the Legal Services Corp. Dudovitz won Iwasaki's backing to oppose the deal, and Legal Services Corp., the national funding source, overruled the proposed San Gabriel-Pomona Valley/Orange County merger. On Jan. 27, 2001, the federal agency awarded the San Gabriel-Pomona Valley service area to Dudovitz under the umbrella of an expanded San Fernando program, citing the location of both programs in Los Angeles, which would allow "better coordinated and more effective advocacy on county government policies." The San Gabriel-Pomona Valley program sued Legal Services Corp. to stop the takeover, claiming the federal program based the decision on favoritism for the politically active Dudovitz and the politically powerful Iwasaki. Though the federal suit accomplished little, it effectively suspended the end of the old program and the start of the new one for nearly a year.
What question would one ask from this paragraph?
Answer: A meeting in late 1999 showed that which two programs had very little in common?

Earthquakes seemed to outline a special feature of earth's crust. Earthquakes let scientists know where the crust was moving. This led to the discovery that the Earths crust was broken up into regions, or plates. Earthquakes happen most often along these plate boundaries. This was evidence that continents can move. The movements of the plates are called plate tectonics. The Earths crust is divided into plates. There are about a dozen large plates and several small ones. Each plate is named for the continent or ocean basin it contains. Scientists know he plates are in motion. They now know the direction and speed of this motion . Plates dont move very fast. They move only a few centimeters a year. This is about the same rate fingernails grow. So you might wonder, what could cause this motion? What supplies the energy to cause this change?
What question would one ask from this paragraph?
Answer: How fast do plates move?

(CNN) -- Japan's prime minister conceded defeat in parliamentary elections Sunday, signaling the return to power of the Liberal Democratic Party and ending the brief rule of the disappointing upstart Democratic Party of Japan. Prime Minister Yoshihiko Noda pledged to step down as party president after exit polls showed a smashing loss in lower house voting. The party, once seen as a breath of fresh air in Japanese politics, came to be regarded as increasingly ineffective. "We got a regrettable result," Noda said. "The result is everything in the politics. The biggest responsibility lies on me. I will quit as the partly leader of DPJ." The move clears the way for the return to power of former Prime Minister Shinzo Abe, the current leader of the conservative-leaning Liberal Democratic Party, or LDP. "The Japanese people will be keenly looking whether the LDP can meet with their expectations," Abe said in interviews after the polling. The LDP ruled the country almost continuously since its establishment in 1955 until it was forced from power three years ago by the DPJ. Public broadcaster NHK said the LDP and its coalition partner, the new Komei party, gained at least 302 seats in the 480-seat lower house. CNN's main affiliate, TV Asahi, reports the LDP/Komei coalition gained at least 312 seats. The official count is expected to be released Monday. The LDP is inheriting a struggling economy, regional tensions and questions over Japan's role in Asia. "The economy is at the bottom. It's our first mission to turn it around," Abe said.
What question would one ask from this paragraph?
Answer: What is the name of Japan's prime minister who conceded defeat in parlimentary elections?

Fossils can be used to match up rock layers. As organisms change over time, they look different. Older fossils will look different than younger fossils. Some organisms only survived for a short time before going extinct. Knowing what organisms looked like at certain times also helps date rock layers. Some fossils are better than others for this use. The fossils that are very distinct at certain times of Earths history are called index fossils. Index fossils are commonly used to match rock layers. You can see how this works in Figure 2.30. If two rock layers have the same index fossils, then they're probably about the same age.
What question would one ask from this paragraph?
Answer:
How can extinction help to date rock layers?