Final answer:
The water table can mimic topography by rising with hills and sinking with valleys. It spans valleys and higher elevations and is much higher in discharge areas. All the options are correct.
Step-by-step explanation:
The water table can mimic topography in several ways. It generally lies near the surface of the ground, but its elevation can vary with the local topography. The water table rises with hills and sinks with valleys. As a result, it can span valleys and higher elevations. Additionally, the water table is much higher in discharge areas, where it discharges into streams.