More important, downtown NO is a very, very small area: less than 4 square miles. Most of which is 2-4 story buildings! (Very light weight, geologically speaking. There are only a few high-rises, and something like the Long Bridge weighs more than the buildings.)
Uh, that was my point. I noted out that the lithospheric bending was from the sediment column, not the local effects of building weight or groundwater pumping (which is a greater effect in clays than silts, anyway, and especially insidious with hysteresis).
Perhaps I wasn't clear enough in my post. Thank you for clarifying.