Siegfried-I

Siegfried-I is a Vestan tectonic weapon developed and completed during the early phases of Operation Eurysian Storm, and subsequently used on the Scornstone Caldera, culminating in its eruption. Developed under Dr. Wolfgang Bloem in the late 1970s, Siegfried-I was first tested successfully in the Arctic Circle, recorded by western seismologists as the 1981 Arctic Circle Tectonic Disruption. Its development would continue with relative success until its full-scale deployment on December 31st, 1984, as part of Operation Endsieg.

The ensuing detonation of the Scornstone Caldera has solidified Siegfried-I's place as one of the most destructive weapons conceived in human history, posing an extreme threat to the Pacal Rim nations. Due to the scarce and expensive nature of the technology involved, however, only a handful of Siegfried-I tectonic weapons were ever built. In the current post-nuclear world, the Siegfried-I is of extreme interest to warlords and militaries alike, either due to the prospect of a tectonic weapon being alluring, or to ensure the destruction of such weapons.