Skiddaw Group, Rock formation in Cumbria, England
The Skiddaw Group is a major rock formation spanning the northern Lake District, composed of mudstones, siltstones, and wacke-type sandstones. It comprises five distinct units that each display different geological characteristics and mineral compositions.
The formation developed during the Ordovician period, with some of its oldest beds possibly extending back to Cambrian times. It represents a significant chapter in the geological history of northern England.
Research on the Skiddaw Group has influenced geological studies since the 19th century, contributing to understanding regional low-grade metamorphic processes.
The rock formation spreads across a wide area within the Lake District and can be accessed through various routes and trails. Weather conditions can change quickly in this region, so visitors should prepare accordingly.
One distinctive unit within this formation is the Buttermere Formation, which represents an olistostrome structure. Fossils of Dichograptus octobrachiatus can be found in specific layers, providing evidence of ancient marine life from this period.
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