After a short historical introduction to the problem of the subsidence in t
he Po Valley, some results are shown of levelling campaigns carried out by
various authorities or agencies in recent years, mainly in the southeast pa
rt of the Po Valley. We also present the results obtained along the coastli
ne using the GPS technique both in a static and in fast-static modes. Atten
tion is focused on the problem of the homogeneity of data from different so
urces, different periods and using different reference benchmarks. To overc
ome these problems, we propose a general levelling network covering the who
le area of the valley, south of the Po river, connected with a GPS network
of more than 50 points. This network will represent a spatial and temporal
reference framework for all the measurements made in the past and for those
planned for the future. A data information system has been implemented in
order to organise and manage all available data in a well defined and homog
eneous framework. This system will make it possible to store other related
data, such as the pattern of the water table. geological evidences, land us
e, etc. (C) 2000 Elsevier Science Ltd. All rights reserved.