The solar eclipse of August 11, 1999, presented good conditions for the stu
dy of associated geophysical effects. Ionospheric measurements clearly show
a decrease of electron density due to the reduced solar irradiation during
the eclipse. However, contrary to claims elsewhere, the decreased conducti
vity did not cause an obvious effect in the geomagnetic recordings at the E
arth's surface. Recordings of several European geomagnetic observatories an
d of a temporary variometer network, set up specially to observe an eclipse
effect in detail, have been studied directly and in terms of equivalent cu
rrents in the ionosphere. We present the results of these studies and discu
ss possible current configurations that might explain the lack of an eclips
e effect in geomagnetic recordings.