
igneous
Tumbled brown-and-black stone, likely basalt or andesite
Fine-grained mafic to intermediate volcanic rock; commonly plagioclase, pyroxene, and possibly olivine or iron oxides
AI-generated identification · may be incorrectDark gray-brown, mottled, and weakly lustrous with a fine-grained texture; estimated Mohs hardness 5–6.5, no visible cleavage, and likely specific gravity about 2.7–3.1.
Identified More igneous →
Explore Tumbled brown-and-black stone, likely basalt or andesite in the encyclopedia →Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Dark gray-brown, mottled, and weakly lustrous with a fine-grained texture; estimated Mohs hardness 5–6.5, no visible cleavage, and likely specific gravity about 2.7–3.1.
Formation & geological history
Likely formed from cooling lava, probably in the Cenozoic or older; subsequent weathering and tumbling produced the smooth rounded shape. Exact identification requires a fresh surface, streak, and mineralogical testing.
Uses & applications
Used as aggregate, road stone, landscaping material, and occasionally as a decorative tumbled stone; usually has little jewelry value.
Geological facts
The rusty brown areas likely reflect oxidation of iron-bearing minerals. Basalt and andesite can look similar in hand-sized, polished specimens.
Field identification & locations
Common in volcanic regions worldwide, including oceanic islands, western North America, Iceland, India, and Japan. A magnetism test, close inspection of grain size, and specific-gravity measurement can help distinguish basalt from andesite.