As I am typing this, I can see the Hogback out of my living room window. (Living here really rocks!) When you are looking at it from the flatlands east of the mountains, the name isn't doesn't seem as self-evident. It just looks like a jumble of low hills in front of the mountains. In fact, from where I live in Littleton, the Hogback is virtually all of the mountains that you can see.

I've tried to sort-out the natural history of the area so that I can share a bit of geological wisdom, but it's pretty much all Greek to me. I was embarrassed at how lost I was reading one article that promised to explain the process in "simple language." The main thing that you'll want to know is that the geological upheaval responsible for lifting the Rockies caused a break in the rock strata along the leading edge on the mountains to be tilted at a peculiar angle. This can be seen dramatically in the red sandstone outcroppings in places like Red Rocks Park in Metro Denver and Garden of the Gods in Colorado Springs. Glaciers and other forces of erosion carved out canyons and broke the single ridge into pieces. Much of the geography of central Colorado, including the locations of cities and roads, is dictated by the natural breaks in the Hogback.
It looks a lot more like "hogback" (or better yet "hogs' backs") from above. The picture below was taken from a trail at Mt Falcon Park.

Have fun!