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Yooperlite

Pronounced: YOO-per-lite

Yooperlite is a trade name for sodalite-bearing syenite that can glow vivid orange or yellow-orange under ultraviolet light due to fluorescent sodalite within the rock.

Formula: No single formula — multi-mineral rockMohs hardness: Approximately 5.5–6.5System: Not applicable — multi-mineral rock
YooperliteCW

Meet the crystal

About Yooperlite

Yooperlite is the popular trade name for a fluorescent sodalite-bearing syenite rock found especially along the shores of Lake Superior in Michigan’s Upper Peninsula. In normal daylight, Yooperlite can look like an ordinary grey, speckled or pale igneous rock. Under ultraviolet light, however, patches and veins containing fluorescent sodalite can glow vivid orange or yellow-orange. The name Yooperlite was popularised after rock hunter Erik Rintamaki discovered the fluorescent stones along the Lake Superior shoreline in 2017. The word combines “Yooper”, a nickname for people from Michigan’s Upper Peninsula, with “-lite”, giving the stone its distinctive commercial name. Yooperlite is not a separate mineral species. It is a multi-mineral syenitic rock containing fluorescent sodalite alongside feldspar and other minerals. The Lake Superior examples are believed to have originated farther north, most likely from the Coldwell Alkaline Complex in Ontario, Canada. Glacial activity transported pieces of the rock southward and deposited them around the Lake Superior region, where waves later rounded and polished many of the stones. The dramatic contrast between its plain daylight appearance and intense ultraviolet fluorescence has made Yooperlite especially popular with mineral collectors and UV rock hunters.

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Showing Science & Formation

Scientific passport

The mineral facts

Observable and measurable properties used to describe and identify this mineral.

Chemical formula
No single formula — multi-mineral rock
Mineral class
Igneous rock — syenite
Crystal system
Not applicable — multi-mineral rock
Mohs hardness
Approximately 5.5–6.5
Lustre
Dull to vitreous
Streak
Usually white to pale
Specific gravity
Approximately 2.5–2.8
Transparency
Opaque

Common colours

Grey, black, white, cream and pale blue-grey; bright orange under UV

Cleavage and fracture

Variable depending on the minerals present; generally uneven fracture.

From the Earth

How it forms

The geological processes that create this crystal over time.

Formation

Its geological story

Yooperlite begins as syenitic igneous rock formed when alkaline magma cools and crystallises. Sodalite develops within the rock alongside feldspar and other silicate minerals. The Lake Superior material was later transported by glacial ice from its original bedrock source and deposited as glacial erratics. Wave action along the shoreline then rounded and polished many of the loose stones found today.

A closer look

Scientific notes

Yooperlite is a commercial name rather than a recognised mineral species. The material is sodalite-bearing syenite. Its most famous property is bright orange to yellow-orange fluorescence under ultraviolet light. The fluorescence is caused by sodalite containing minor sulphur-related components within its crystal structure. Electron microprobe analysis has confirmed sodalite in Lake Superior Yooperlite material. The Michigan stones are thought to have originated from the Precambrian Coldwell Alkaline Complex in Ontario and were transported into the Lake Superior region by glaciation.

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