Metamorphic / Specimen 05

Marble.

How to identify it

Crystalline, sugary-looking texture when broken

Explore the metamorphic family ↗
White marble surface with crystalline texture
Zyance · CC BY-SA 2.5 · Image source ↗
01 / Origin story

How does marble form?

Marble is a non-foliated metamorphic rock formed when limestone (or chalk) is subjected to heat and pressure, causing its calcite crystals to recrystallize into a denser, interlocking crystalline structure.

02 / Read the clues

How can you identify marble?

Use several clues together.
One photograph shows one specimen, not every variation.

Enlarged crop of the Marble specimen
Texture study · enlarged crop of this specimen
  1. 01Crystalline, sugary-looking texture when broken
  2. 02Often shows swirling color patterns/veining from mineral impurities
  3. 03Still reacts with acid, just like its parent limestone (same mineral, calcite)
  4. 04Softer than most metamorphic rock — around 3 on the Mohs scale
  5. 05Prized for carving and construction — statues, buildings, countertops
03 / Commonly confused with

Similar at first glance.

Compare the materials side by side.
Photographs are not shown to the same scale.

Marble specimen for comparison

Marble ↗

Crystalline, sugary-looking texture when broken

Limestone specimen for comparison

Limestone ↗

Usually light-colored: white, gray, tan, sometimes yellowish

Limestonemarble's crystals are visibly interlocking and sugary once you look closely, while limestone often shows visible fossils or a duller, more granular texture. Both fizz with acid, so that test alone won't distinguish them.

04 / Out in the world

Where it’s found.

Regions of metamorphosed limestone — famously Carrara, Italy, and various deposits across the U.S. (Vermont, Georgia, Colorado).

Continue exploring

More from this family.