New location and new 4th BPR for use at Axial. Data recorded are unusual because they show steady apparent deflation the whole year, amounting to ~40 cm! This is the first record from up on the western rim of the caldera, which probably has heavy sediment. The apparent deflation could be due to site instability - perhaps the instrument was slowly settling into the sediment all year? Or else the drift rate could be relatively high and positive, but unfortunately we have no way to constrain it.