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

Sam Gillen (Van Damme) is a convict who gets sprung from Federal custody somewhere in the Midwest by his bank-robbing partner. In their last heist, Sam's partner killed a bank guard, and Sam took the rap for it. Sam's partner gets killed in the break, forcing Sam to go it alone in search of the loot, which is buried on the property of a farm inhabited by Clydie Anderson (Arquette), the widowed mother of two kids named Mike "Mookie" Anderson and Bree Anderson.Attempting to sneak into Clydie's house and "borrow" some salt for a campfire-broiled steak, Sam catches sight of Clydie taking a shower. The next morning, Sam is spotted bathing outdoors by Mookie. After saving Clydie, Mookie, and Bree from a trio of intruding thugs, Sam discovers that Clydie is holding out from selling her place to property developer Franklin Hale, who fears that he will be put out of business if he doesn't get Clydie's land so he can develop on it.Sam decides to hang around, sleeping first in Clydie's barn and then in her bed while repairing her late husband's Triumph motorcycle. And Hale hires an intimidation expert named Dunston, to force Clydie into selling her land. Secretly on Hale's payroll is corrupt sheriff Lonnie Cole, a sometime lover of Clydie.A jealous Lonnie discovers Sam's true identity and threatens to expose him if he doesn't leave. Not wanting to place Clydie in additional danger for helping a fugitive, Sam decides to leave, only to find that Hale has already blown the whistle on him in an attempt to get him out of the way. After evading police chasing him in cars, land rovers, helicopters, and on motorcycles and horseback, Sam returns to save Clydie from Dunston and Hale, who are planning to burn down her house.After fighting off the bad guys and getting Hale caught holding a gun to Clydie's head, he decides to turn himself in, rather than run away. He promises to be back to live with them.
Who spots Sam bathing outdoors ?

Many patients with restless legs syndrome (Willis-Ekbom disease) complain of burning sensations in their feet associated with the desire to move, such that they seek cooler environments. This pilot study aimed to characterise the microvascular skin changes in 12 patients with restless legs syndrome compared with 12 age- and sex-matched controls. Patients with moderate or severe restless legs syndrome and controls underwent detailed thermovascular assessment in a controlled temperature room at three different stages (normothermic phase 23C, hot phase 30C, cold phase 18C). Microvascular activity was recorded during all phases by bilateral great toe laser-Doppler flowmetry and also by whole-body thermography. Patient and control measurements were compared. The study protocol was well tolerated. Parameters extracted from the laser-Doppler flowmetry measurements were used to model a logistic function using binary logistic regression. This demonstrated a statistically significant difference between patients with restless legs syndrome and healthy controls (P<0.001). Visual inspection of the body thermography image sequences showed increased lower limb movement in patients with restless legs syndrome patients compared with controls. Thermography analysis also showed significant differences between foot temperatures in patients with restless legs syndrome compared with controls during the hot phase (P=0.011). Notably, patients with restless legs syndrome had more uniform foot temperatures, whereas controls had a wider variability in surface temperature across the feet. This novel study demonstrates impaired microvascular circulation in patients with restless legs syndrome in comparison to matched controls and a potential mechanism for the sensation of burning feet. The protocol also provides an experimental paradigm to test therapeutic interventions for the future.
Willis-Ekbom disease is also known as?

The study of rock strata is called stratigraphy. The laws of stratigraphy can help scientists understand Earths past. The laws of stratigraphy are usually credited to a geologist from Denmark named Nicolas Steno. He lived in the 1600s. The laws are illustrated in Figure 11.6. Refer to the figure as you read about the laws below. Superposition refers to the position of rock layers and their relative ages. Relative age means age in comparison with other rocks, either younger or older. The relative ages of rocks are important for understanding Earths history. New rock layers are always deposited on top of existing rock layers. Therefore, deeper layers must be older than layers closer to the surface. This is the law of superposition. You can see an example in Figure 11.7. Rock layers extend laterally, or out to the sides. They may cover very broad areas, especially if they formed at the bottom of ancient seas. Erosion may have worn away some of the rock, but layers on either side of eroded areas will still match up. Look at the Grand Canyon in Figure 11.8. Its a good example of lateral continuity. You can clearly see the same rock layers on opposite sides of the canyon. The matching rock layers were deposited at the same time, so they are the same age. Sediments were deposited in ancient seas in horizontal, or flat, layers. If sedimentary rock layers are tilted, they must have moved after they were deposited. Rock layers may have another rock cutting across them, like the igneous rock in Figure 11.9. Which rock is older? To determine this, we use the law of cross-cutting relationships. The cut rock layers are older than the rock that cuts across them. Geologists can learn a lot about Earths history by studying sedimentary rock layers. But in some places, theres a gap in time when no rock layers are present. A gap in the sequence of rock layers is called an unconformity. Look at the rock layers in Figure 11.10. They show a feature called Huttons unconformity. The unconformity was discovered by James Hutton in the 1700s. Hutton saw that the lower rock layers are very old. The upper layers are much younger. There are no layers in between the ancient and recent layers. Hutton thought that the intermediate rock layers eroded away before the more recent rock layers were deposited. Huttons discovery was a very important event in geology! Hutton determined that the rocks were deposited over time. Some were eroded away. Hutton knew that deposition and erosion are very slow. He realized that for both to occur would take an extremely long time. This made him realize that Earth must be much older than people thought. This was a really big discovery! It meant there was enough time for life to evolve gradually. When rock layers are in the same place, its easy to give them relative ages. But what if rock layers are far apart? What if they are on different continents? What evidence is used to match rock layers in different places? Some rock layers extend over a very wide area. They may be found on more than one continent or in more than one country. For example, the famous White Cliffs of Dover are on the coast of southeastern England. These distinctive rocks are matched by similar white cliffs in France, Belgium, Holland, Germany, and Denmark (see Figure 11.11). It is important that this chalk layer goes across the English Channel. The rock is so soft that the Channel Tunnel connecting England and France was carved into it! Like index fossils, key beds are used to match rock layers. A key bed is a thin layer of rock. The rock must be unique and widespread. For example, a key bed from around the time that the dinosaurs went extinct is very important. A thin layer of clay was deposited over much of Earths surface. The clay has large amount of the element iridium. Iridium is rare on Earth but common in asteroids. This unusual clay layer has been used to match rock up layers all over the world. It also led to the hypothesis that a giant asteroid struck Earth and caused the

A key bed of clay from around the time the dinosaurs went extinct led to the hypothesis that the extinction was caused by a