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Geology of the Vale
The geology of the Vale of Belvoir consists of Triassic mudstones in the north leading into Lower Jurassic marine mudstones and limestones, which are heavily mantled by Quaternary glacial deposits.
Its prominent southern escarpment, where Belvoir Castle sits, is capped by the erosion-resistant Marlstone Rock Formation.
The landscape and bedrock structure are organized into a tiered, north-to-south sequence of sedimentary rocks that dip gently to the east.
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Bedrock Geology
Triassic (Mercia Mudstone and Penarth Group): Found at the northern fringe of the vale, these ancient red and green mudstones underlie the low-lying, gently undulating agricultural plains.
Lower Jurassic (Lias Group): The bulk of the vale is formed from thick sequences of dark-grey marine shales and mudstones (including the Charmouth Mudstone and Whitby Mudstone Formations). These layers are famously fossiliferous, frequently yielding ammonites and Gryphaea (often called "Devil's toenails").
Marlstone Rock Formation: This prominent ironstone bed caps the southern ridge of the vale, creating an abrupt 100 metre (330 feet) scarp slope. This rock is significantly more resistant to erosion than the surrounding clays, protecting the ridge and providing the foundation for Belvoir Castle.
Superficial (Quaternary) Deposits
Much of the solid geology is hidden by deposits left during the last two million years of the Ice Age and ancient river systems.
Glacial Till: Anglian-era glacial till (boulder clay) blankets much of the higher ground.
River sands and gravels: The vale was historically occupied by the ancient 'Proto-Trent' and Bytham rivers, which left behind rich, terrace sand and gravel deposits.
Alluvium and landslips: Modern river floodplains (like that of the River Devon) are lined with alluvium. Land-slipped ground is also common along the steeper Jurassic escarpments due to unstable mudstone.
Economic Significance
The interaction of mudstones and river gravels creates rich Grade 2 and Grade 3 agricultural soils.
Historically extraction of gypsum and gravels was important. Ironstone extraction was of national significance between the 1870s and 1970s. Very small amounts of ironstone are currently extracted when needed for heritage building repairs.
In addition the Lower Jurassic Lias mudstones are exploited for amateur and scientific fossil hunting, mostly by walking ploughed fields (with the landowners' consent).
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