Historical and modem high-precision leveling data are analyzed to meas
ure recent vertical movements in northeast Spain. The recent vertical
movements are deduced by comparing the original height differences (ta
ken from the original logbooks) measured in the field in two surveys c
arried out by the Institute Geografico Nacional in the periods 1871-19
22 and 1925-1974. An exhaustive study of the errors involved in the me
asurements indicates that some of the observed movements are significa
nt. We present the recent vertical movements along eight profiles with
significant uplift rates: a southern anomaly of about 1 mm/yr, observ
ed in two independent profiles, associated with the southern part of t
he Catalan Ranges frontal thrust; one anomaly between Caldetes and Are
nys with an average velocity of about 4 mm/yr, which can be related to
the seismic activity of this century; two anomalies of about of 2.5 m
m/yr in the noah and of about 4 mm/yr in the south associated with the
NW-SE striking Amer-Brugent fault system, which has been related to a
great seismic crisis in the fifteenth century, and one anomaly of abo
ut 0.8 mm/yr associated with the Emporda basin dynamics. Other observe
d recent vertical movements are mainly related to sediment compaction
masking possible tectonic deformations. All the northern anomalies are
associated with the NW-SE system of faults considered as a ''transfer
zone'' of the NE-SW striking faults which controlled the formation of
the Neogene European rifting. The former shows Plio-Quaternary tecton
ic activity: folds, faults, volcanism, hydrothermalism and historical
seismicity. The low seismicity of this century around the Amer-Brugent
fault system contrasts with both the high average velocities estimate
d here and with the fifteenth century seismic crisis, Therefore, if th
ese high uplift rates are tectonic in origin, they may represent an ac
cumulation of elastic strain which would be released in a future large
earthquake rather than in continual small ones. According to this hyp
othesis, a large part of the stress accumulated since the fifteenth ce
ntury has yet to be released. Further leveling and neotectonic surveys
are needed to test this hypothesis.