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

Ex Input:
Freshwater below Earths surface is called groundwater. The water infiltrates, or seeps down into, the ground from the surface. How does this happen? And where does the water go? Water infiltrates the ground because soil and rock are porous. Between the grains are pores, or tiny holes. Since water can move through this rock it is permeable. Eventually, the water reaches a layer of rock that is not porous and so is impermeable. Water stops moving downward when it reaches this layer of rock. Look at the diagram in Figure 13.11. It shows two layers of porous rock. The top layer is not saturated; it is not full of water. The next layer is saturated. The water in this layer has nowhere else to go. It cannot seep any deeper into the ground because the rock below it is impermeable. The top of the saturated rock layer in Figure 13.11 is called the water table. The water table isnt like a real table. It doesnt remain firmly in one place. Instead, it rises or falls, depending on how much water seeps down from the surface. The water table is higher when there is a lot of rain and lower when the weather is dry. An underground layer of rock that is saturated with groundwater is called an aquifer. A diagram of an aquifer is shown in Figure 13.12. Aquifers are generally found in porous rock, such as sandstone. Water infiltrates the aquifer from the surface. The water that enters the aquifer is called recharge. Most land areas have aquifers beneath them. Many aquifers are used by people for freshwater. The closer to the surface an aquifer is, the easier it is to get the water. However, an aquifer close to the surface is also more likely to become polluted. Pollutants can seep down through porous rock in recharge water. An aquifer that is used by people may not be recharged as quickly as its water is removed. The water table may lower and the aquifer may even run dry. If this happens, the ground above the aquifer may sink. This is likely to damage any homes or other structures built above the aquifer. One of the biggest aquifers in the world is the Ogallala aquifer. As you can see from Figure 13.13, this aquifer lies beneath parts of eight U.S. states. It covers a total area of 451,000 square kilometers (174,000 square miles). In some places, it is less than a meter deep. In other places, it is hundreds of meters deep. The Ogallala aquifer is an important source of freshwater in the American Midwest. This is a major farming area, and much of the water is used to irrigate crops. The water in this aquifer is being used up ten times faster than it is recharged. If this continues, what might happen to the Ogallala aquifer? The top of an aquifer may be high enough in some places to meet the surface of the ground. This often happens on a slope. The water flows out of the ground and creates a spring. A spring may be just a tiny trickle, or it may be a big gush of water. One of the largest springs in the world is Big Spring in Missouri, seen in Figure 13.14. Water flowing out of the ground at a spring may flow downhill and enter a stream. Thats what happens to the water that flows out of Big Spring in Missouri. If the water from a spring cant flow downhill, it may spread out to form a pond or lake instead. Lake George in New York State, which is pictured in Figure 13.15, is a spring-fed lake. The lake basin was carved by a glacier. Some springs have water that contains minerals. Groundwater dissolves minerals out of the rock as it seeps through the pores. The water in some springs is hot because it is heated by hot magma. Many hot springs are also mineral springs. Thats because hot water can dissolve more minerals than cold water. Grand Prismatic Spring, shown in Figure 13.16, is a hot mineral spring. Dissolved minerals give its water a bright blue color. The edge of the spring is

Ex Output:
top of an underground rock layer that is saturated with water


Ex Input:
In 1997 the Kymi Province was merged with the Uusimaa Province and the southern parts of the Hame Province into the new Southern Finland Province.

Ex Output:
What was replaced Kymi Province?


Ex Input:
Mowat-Wilson syndrome is a genetic condition characterized by a recognizable facial phenotype in addition to moderate to severe cognitive disability with severe speech impairment and variable multiple congenital anomalies. The anomalies may include Hirschsprung disease, heart defects, structural eye anomalies including microphthalmia, agenesis of the corpus callosum, and urogenital anomalies. Microcephaly, seizure disorder and constipation are common. All typical cases result from haploinsufficiency of the ZEB2 (also known as ZFHX1B or SIP-1) gene, with over 100 distinct mutations now described. Approximately 80% of patients have a nonsense or frameshift mutation detectable by sequencing, with the rest having gross deletions necessitating a dosage sensitive assay. Here we report on the results of comprehensive molecular testing for 27 patients testing positive for MWS. Twenty-one patients had a nonsense, frameshift, or splice site mutation identified by sequencing; 14 of which localized to exon 8 and 17 of which are novel. Six patients had deletions in the ZEB2 gene, including two novel partial gene deletions. This report, the first such analysis in North American patients, adds to the growing list of both novel pathogenic mutations associated with MWS, as well as other variants in the ZEB2 gene. In addition, we suggest an economical testing strategy.

Ex Output:

Which gene is responsible for the development of the Mowat-Wilson syndrome?