Origins of Goldfire Schist

(scroll to the bottom for picture highlights!)

Goldfire Schist was recovered from a large, exposed rock face that has stood behind my family’s cabin near Rollinsville, Colorado for as long as I can remember. For most of my life, it existed simply as part of the landscape—a constant presence passed daily without question.

It was only well into adulthood, through years of rockhounding and learning to read geological structure, that I began to recognize signs of something more complex. What appeared uniform at a distance revealed internal fracture, mineral migration, and iron-rich staining shaped by pressure and heat over immense spans of time. In my excitement, I had samples tested at a local geological research laboratory, where trace amounts of a naturally occurring gold–silver alloy known as electrum were confirmed running through the stone.

Schist is structurally unstable. Its layered planes separate easily, often failing under minimal handling. Many pieces fracture before their internal character is ever exposed. Working with this material required learning how to stabilize what had already been in the process of breaking apart.

I was drawn to Goldfire Schist because it reminded me that recognition often arrives late—and that what endures longest in our lives can still surprise us once we learn how to look.