There are several common sources for gravity waves, including the oscillations of an intense updraft. The features in the pic that Sam posted are cloud streets / boundary layer rolls. If I'm not mistaken, gravity waves tend to have little preference for wind direction -- they spread out from a source in all directions (at least initially). BL rolls, on the other hand, are aligned in the same direction as the low-level flow. Looking at the surface map (and RUC analysis) across the Gulf region this morning, we see pretty strong north-northeast surface winds, which align very well with the north-northeast orientation of the cloud (streets). In addition, convective rolls/cloud streets tend to be rather stationary, since they are aligned with the boundary layer flow. If you loop that vis sat image, you'll see that the more prominent rolls are indeed quasi-stationary -- they do not propagate out as a gravity wave would.