
sedimentary
Glauconitic Sandstone
Glauconitic Sandstone (Quartz with Glauconite)
Hardness 6-7 (quartz matrix), dull to earthy luster, fine to medium grain size, distinctive greenish-gray to blue-green tint due to iron-rich glauconite mixed with tan/beige silica sand, clastic texture with faint bedding layers.
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Physical properties
Hardness 6-7 (quartz matrix), dull to earthy luster, fine to medium grain size, distinctive greenish-gray to blue-green tint due to iron-rich glauconite mixed with tan/beige silica sand, clastic texture with faint bedding layers.
Formation & geological history
Formed in shallow, oxygen-poor marine environments through the slow accumulation and diagenesis of quartz grains along with iron-potassium phyllosilicate minerals (glauconite). Common in Cretaceous and Paleogene sedimentary strata.
Uses & applications
Used historically as building stone, architectural flagstone, source of green pigment, soil conditioner (greensand), and geological study specimens.
Geological facts
Glauconite is often referred to as 'greensand' and indicates slow rates of accumulation in shallow sea environments. The greenish tinge is created by hydrous iron-rich potassium silicate minerals within the sandstone matrix.
Field identification & locations
Identified in the field by its sandy, abrasive texture combined with characteristic greenish-blue or sage-green patches amidst tan or gray sedimentary layers. Commonly found in coastal sedimentary exposures, river beds, and quarry outcrops worldwide.
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