Mineral

Chondrite Meteorite

Ordinary Chondrite (L or H Type)

Hardness: 5-6 (variable based on metallic content); Color: Mottled brown, orange, and gray due to oxidation; Luster: Sub-metallic to dull; Crystal structure: Contains spherical chondrules; Specific gravity: 3.0 to 3.8

Hardness: 5-6 (variable based on metallic content)
Color: Mottled brown, orange, and gray due to oxidation
Luster: Sub-metallic to dull

Identified April 8, 2026More mineral →

Identify your own rocks.

Get a report just like this from any photo, free.

App Store Google Play

Physical properties

Formation & geological history

Formed in the early solar system roughly 4.5 billion years ago from solar nebula dust and grains. Found as terrestrial falls typically in arid desert regions or Antarctica.

Uses & applications

Primarily used for scientific research, education, and private collection. Can be used in 'out of this world' jewelry when sliced and polished.

Geological facts

Chondrites are the most common type of meteorite falling to Earth, accounting for about 86% of all falls. They contain the oldest solid materials in our solar system.

Field identification & locations

Identify by looking for a fusion crust (exterior), magnetic attraction (due to iron-nickel flakes), and the presence of tiny spherical chondrules inside when cut.

Other mineral specimens

See all

Sandstone (with potential mineral staining/concretions)

Arenite (SiO2 based)

sedimentary

Epidote

Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)

metamorphic

Nephrite Jade

Nephrite

Mineral/Rock

Banded Gneiss (River Rock/Pebble)

Gneiss (specifically a banded variety often found as a river rock)

Metamorphic Rock

Green Apatite on Albite

Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]

mineral

Epidote

Epidote - Ca2(Al2,Fe3+)3(SiO4)3(OH)

mineral