
sedimentary
Small iron-oxide-rich rock fragment (possibly ferruginous sandstone)
Ferruginous sandstone or ironstone; likely quartz grains cemented by iron oxides such as hematite/goethite
AI-generated identification · may be incorrectSmall, rough, brown-red fragment with an earthy to dull luster and no visible crystal faces. Exact hardness, cleavage, and specific gravity cannot be determined from the photo; ferruginous sandstone is typically about 6–7 Mohs if quartz-rich.
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Physical properties
Small, rough, brown-red fragment with an earthy to dull luster and no visible crystal faces. Exact hardness, cleavage, and specific gravity cannot be determined from the photo; ferruginous sandstone is typically about 6–7 Mohs if quartz-rich.
Formation & geological history
Likely formed as sedimentary grains cemented or stained by iron oxides during weathering or groundwater circulation. The reported location in eastern Morocco makes iron-stained sedimentary material plausible, but the fragment is too small to establish its age or origin.
Uses & applications
Commonly has no commercial value at this size; ironstone and ferruginous sandstone can be used as construction stone or iron ore when sufficiently rich in iron.
Geological facts
Iron oxides produce the rusty red-brown color and may leave a reddish or ochre streak. The specimen’s grain texture and composition are not clear enough in this image for a definitive identification.
Field identification & locations
A rusty surface and gritty texture would support ferruginous sandstone; a red-brown streak suggests hematite, while a yellow-brown streak favors goethite. A fresh break and simple streak/magnet tests can help distinguish it; iron-rich rocks occur in many settings.
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