Determining whether clean groundwater has become dirty and what caused any contamination is a complex pursuit. stephen osborn and three colleagues from duke university set out to learn whether drinking water was really being contaminated by nearby hydrofracking. osborn’s team focused on sites in northeastern pennsylvania and adjacent new york, where the marcellus shale formation overlies the utica shale formation. the sites they tested are indicated in the map below.

3. a worker pushes a 30.5 kg polished stone along a polished table with a force on bonin a straight line for 5.20 s after starting from rest. there is no friction between thestone and the table. at the end of the table. the stone is hooked to a cable with a lengthof 62.0 cm to rotate it to a rough table to store until they can be picked up. the roughtable has a coefficient of static friction 0.702 with the polished stone. remember that 8= 9.80 m/s2a) what is the speed of the stone when it is hooked to the cable? b) what is the tension in the cable while the stone is rotating? (there is still nofriction)c) how much force is needed to make the stone begin sliding from rest on therough table? ius = 0.70262.0 cm30.5 kg20.5 kg6= 0