The Alum Shale is a black, organic rich shale formation exposed across parts of Sweden, spanning the Cambrian through Ordovician periods and locally more than five hundred million years old at its base, historically mined for alum and, more recently, for uranium and oil shale, while also preserving trilobites and other early marine fossils, including the well known Orsten-type deposits within it that preserve microscopic animals in exceptional three dimensional detail. The formation is one of the most extensively studied Paleozoic rock sequences in Scandinavia.
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Alum Shale Formation (Wikipedia)
In Discipline: Stratigraphy, Lead section (in-discipline Stratigraphy)
The Alum Shale Formation is a rock formation of black shale of Miaolingian (Middle Cambrian) to Tremadocian (Lower Ordovician) in age found predominantly in Scandinavia, but also some parts of Estonia and Finland.
Caused By: Sedimentation, Article text
Subsequently, Ordovician limestones and shales sequences were deposited until the Silurian.
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