Puddingstone is a type of conglomerate sedimentary rock consisting of rounded, colorful pebbles embedded in a finer-grained matrix. It is highly valued by collectors for its resemblance to a pudding filled with fruit, often featuring contrasting colors between the clasts and the groundmass.
Is this puddingstone?
3-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Read the textureLook at a fresh break with a hand lens. Texture: Rounded gravel-sized clasts in a finer matrix. Grain size: Gravel-sized clasts.
- 2Pick out the mineralsComposition: Michigan puddingstone: white quartzite with pebbles of jasper and other dark inclusions. Identify the two or three most abundant grains.
- 3Match the color rangeCompare against the expected color range: multicolored, gray, red, white, brown.
Often confused with
Puddingstone vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside puddingstone
Minerals reported to co-occur with puddingstone. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Transparency
- Opaque
- Rarity
- Common
- Uses
- Decorative, Lapidary, Collector
- Host rock
- sedimentary basins
- Texture
- Rounded gravel-sized clasts in a finer matrix
- Grain size
- Gravel-sized clasts
- Composition
- Michigan puddingstone: white quartzite with pebbles of jasper and other dark inclusions
Where rockhounds find puddingstone
9 mapped spotsClassic worldwide localities
- Michigan, USA
- United Kingdom
- Ontario, Canada
- New England, USA
Field-hunting tip
Where it forms: sedimentary basins. If you start seeing quartz, calcite, iron oxides in float, you are in the right ground. In the U.S., the densest reported localities are in Michigan, Maryland. Start trip planning there.




