Thank you Qshake and Wictor, I do appreciate your time and comments.
A relatively little-known fact in E North America (US and Canada) is that shallow rocks are under very, very high horizontal stresses (geological reasons are unimportant for engineering purposes); there are many measurements indicating that a range of 1500-2000psi is to be expected in the free field. In upstate NY and OH,concrete structures for power projects, poured directly against rock, have been destroyed by creeping rock. Horizontal displacements of several inches have been measured (NB: Wictor). Rock bursts are common in tunnels and other excavations which concentrate stresses. There are many examples of these horizontal stresses sneaking up on projects because we don't think about them.
When a valley is carved, the stress trajectories are deflected downward under the valley floor where stress concentrations factors can exceed 2. Sometimes compression folds (buckles) develop in the rock in the middle of the valley floors.
Let's assume a hypothetical single-span gird-bridge,simply supported on two piers, and two approach ramps, also supported by those piers; the bearings are high rocker type. The rocker bearings are found "frozen" as follows: the ones supporting the main span are badly over-extended (main span has dilated more than reasonable computations show); the ones supporting the approaches are badly over contracted. This behavior can be easily explained if one accepts movement of piers toward the valley center. In fact I think this is the case at the Albany bridge but pier movement is discarded outright in the forensic report. Problem is ground movements can be exceedingly difficult to identify and isolate in the field.
The often-cited cause for over-tilted, frozen rocker bearings: detritus, debris, soil, rust, on one side of the bearing
plate impeding rocking action and creating a ratcheting action does not cut mustard with me.
Happy end-of-year holidays
engeon