Thermals are winds driven by differences in air temperature. Warm air is lighter/thinner, hence rises (think of a hot-air balloon). Cooler air is denser/thicker, hence falls.
Thermals can occur in flat country. Bare ground absorbs heat much faster than forested or grassy areas. That bare ground also radiates more heat, warming the air just above the ground, which then rises. As that warmer air rises, surrounding air is drawn in from all directions to replace the rising air. Late in the morning, once the sun has had a chance to hit the ground for an hour or so, this differential heating process can produce light thermal winds being drawn into an open dirt field from the surrounding areas.
Although thermal winds will be produced anywhere differential heating of the surface occurs, thermals are most pronounced and obvious in hilly terrain. When the sun first peaks over the horizon, the suns rays hit the tops of ridge-lines first. The ground is warmed there, which warms the air just above it, and that air begins to rise. This rising air must be replaced, and air is drawn up out of the valleys, with air on the east (sunny-side) of the ridge rising most rapidly. This thermal wind rising up to and verically away from the top of the ridge aids both bucks near the rut and the hunter in the early morning hours. Bucks can walk the ridge-lines and scent-check for does in the valleys. Hunters hunting on ridge-lines can have their scent lifted vertically away from them producing a situation with literally no "downwind."
In hilly terrain, exactly the opposite occurs once the sun sets. Without the sun heating the ground, air begins to cool and settle. The coolest air settles the quickest, and begins to run downhill just like water. Imagine a "river" of the coolest air running down every drainage and concentrating in the bottoms of valleys. These evening thermal can become amazingly strong, often reaching 5-10 MPH, but can also be amazingly thin, only reaching 10-15 feet off the ground.
Of course, all of these thermal events can be heavily influenced by pressure system winds (winds driven by high and low pressures systems). Moderate to strong prevailing winds can over-power these thermals. Thermals are the most predictable under High pressure when prevailing winds are virtually nil. The mixture of thermals and prevailing winds are most confusing when prevailing winds are light.