Blue Pearl Granite Identification Guide
Identify Blue Pearl 'granite' as a larvikite monzonite by its blue-flashing feldspar (schiller), coarse interlocking crystals, and hardness near 6.
Read the full Blue Pearl Granite encyclopedia entry →
What Blue Pearl Granite Looks Like
Blue Pearl is a famous commercial 'granite' that is geologically a larvikite (a syenite/monzonite, not a true granite). It is a coarse-grained igneous rock dominated by large blocky feldspar crystals that flash silvery-blue (schiller/labradorescence) when light hits them at the right angle. The background is gray to blue-gray, speckled with dark minerals. The defining feature is the shimmering blue iridescence of the feldspar grains.
Step-by-Step Field ID Checklist
- Look for the blue flash: Tilt the slab — the feldspar crystals flash blue/silver (schiller). This is the signature of larvikite.
- Grain size: Coarse, interlocking feldspar crystals (often 1–3 cm) visible to the eye.
- Mineral mix: Light feldspar dominant, with scattered dark grains (pyroxene, amphibole, biotite); little or no visible quartz (unlike true granite).
- Luster: Feldspar shows a pearly-to-metallic sheen on cleavage faces.
- Hardness test: Feldspar scratches glass (~6); a knife will not scratch it easily.
Key Diagnostic Tests
- Hardness: Feldspar grains ~6 (scratch glass); overall a hard rock.
- Schiller/labradorescence: Blue-to-silver iridescence within feldspar — the diagnostic optical effect.
- Cleavage: Feldspar shows two cleavage directions at ~90° with flat reflective faces.
- Texture: Holocrystalline, coarse, interlocking (phaneritic igneous), not banded like gneiss.
- Acid reaction: None on the silicate minerals.
- Low quartz content: Helps separate larvikite from true granite.
Common Look-Alikes and How to Tell Them Apart
- True granite: Granite contains abundant glassy quartz and often pink/white feldspar without the strong blue schiller; Blue Pearl's flash and lack of quartz distinguish it.
- Labradorite slabs: Labradorite is a single feldspar showing similar flash, but Blue Pearl is a whole rock (larvikite) with feldspar crystals set in a coarse igneous matrix.
- Gneiss/migmatite: These are foliated/banded metamorphic rocks; larvikite is unfoliated igneous with random crystal orientation.
- Gabbro/anorthosite: Darker or more plagioclase-rich; lack the pervasive blue feldspar schiller of larvikite.
Where Blue Pearl Granite Is Found
Blue Pearl larvikite is quarried in the Larvik area of southern Norway, the type locality of larvikite (Norway's national stone). The rock formed from slowly cooled alkaline magma in the Oslo Rift around 290 million years ago, allowing the large feldspar crystals to develop. It is shipped worldwide as dimension stone for countertops, facades, and tiles.
Quick Confidence Check
A coarse, quartz-poor igneous rock whose blocky feldspar crystals flash silvery-blue when tilted, with feldspar that scratches glass, is Blue Pearl larvikite (sold as Blue Pearl granite).
Frequently asked questions
Is Blue Pearl granite really granite?
No. Geologically it is larvikite, a coarse-grained syenite/monzonite low in quartz. It is sold as 'granite' in the stone trade, but true granite contains abundant quartz and lacks larvikite's strong blue feldspar schiller.
What causes the blue flash in Blue Pearl granite?
The blue-to-silver shimmer is schiller (labradorescence), caused by light interference from microscopic lamellae within the feldspar crystals. Tilting the stone makes the flash appear and disappear.
How can you tell if it's real Blue Pearl granite (larvikite)?
Look for coarse blocky feldspar crystals that flash blue when tilted, set in a quartz-poor igneous matrix with scattered dark minerals. The feldspar scratches glass (hardness ~6) and the rock is unbanded.
Blue Pearl granite vs labradorite — what's the difference?
Labradorite is a single feldspar mineral showing blue flash, while Blue Pearl is a whole rock (larvikite) in which feldspar crystals showing that flash are set within a coarse igneous matrix.
Where does Blue Pearl granite come from?
It is quarried from larvikite deposits in the Larvik region of southern Norway, where it formed from slowly cooled alkaline magma about 290 million years ago.