SOLAR flares are closely associated with magnetic activity on the surf
ace of the Sun. They typically occur1 in complex sunspot groups, where
the vertical magnetic fields reverse abruptly, and the horizontal (tr
ansverse) fields connecting the vertical poles are both sheared and st
rong. A single field inversion line may be the site of many flares1. H
ere we report observations of a large, active sunspot group which reve
al a series of oppositely directed vertical-field inversions separated
by extremely narrow elongated channels of intense horizontal fields.
In a minimum-energy configuration, lines of force connecting oppositel
y directed vertical fields simply arch across the inversion line; but
when newly emerged sunspots move through older magnetic-field configur
ations, the poles are pushed together and the field lines turn sharply
along the inversion line to reconnect with the vertical field some di
stance away. These multiple channels of horizontal field imply a large
curl term (del x B), and hence a substantial electric current. Our ob
servations show that almost all of the larger flares in this region oc
cur in these highly convoluted fields.