An intense solar energetic particle (SEP) event was detected in September 2004 by near‐Earth spacecraft and by Ulysses at 5.4 AU. Characteristics of the intensity and anisotropy time profiles at both heliospheric locations were determined by the presence of a corotating low‐density, low‐speed, and low‐proton‐beta βp solar wind stream. This low‐βp stream was followed by a faster and denser solar wind that formed a strong compression region. The bulk of energetic particles at 1 AU were observed downstream of this compression region. Only those particles either able to leak from behind the compression region, accelerated by the shock driven by the coronal mass ejection that generated the SEP event as it penetrated into the low‐βp region, or both were observed prior to the main component of the SEP event at 1 AU. Anisotropic ion intensity enhancements observed upstream of this shock resulted from both particle acceleration in a corrugated shock surface and particle propagation within the low‐βp region. The particle event at Ulysses had exceptionally large and long‐lasting (>4 days) field‐aligned anisotropies. These large anisotropies resulted from both leakage of energetic particles from behind the compression region and their propagation within the low‐βp region. We propose a scenario that explains the characteristics of the particle event at both 1 AU and Ulysses. The effects that large‐scale interplanetary structures have on the energetic particle transport determine the properties of the event at both spacecraft. These effects must be carefully considered by models of energetic particle transport in the heliosphere.