Observations of the varying orientations of comet tails led to the suggesti
on of the existence of the solar wind-a continuous outflow of ionized mater
ial from the Sun(1). It is now well established that gas from comets is ion
ized by several processes and joins the solar wind(2), forming an ion (plas
ma) tail that points away from the Sun. The plasma environments of three co
mets have been measured in situ, but only in the upstream direction or less
than 8,000 km downstream of the nucleus. Here we report a fortuitous cross
ing by a spacecraft of the plasma tail of comet Hyakutake (C/1996 B2), at a
distance of more than 3.8 astronomical units (550 million kilometres) from
its nucleus. This surpasses the tail length of 2 AU determined for the Gre
at March Comet of 1843 (C/1843 D1)(3). Our measurements reveal that, at thi
s distance, the tail of comet Hyakutake was a structured entity at least 7
million kilometres in diameter.