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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.


source


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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Chronicle entries

home page

what's new?

the geology of the Vale

the boundaries and rivers of the Vale

long, long ago

long ago

not that long ago

seems like yesterday


researching and writing local history

  • the Vale as a verb
  • getting started free advice from 2005
  • asking curious questions (YouTube video)


    local history groups in and around the Vale

  • Aslockton (Cranmer LHG)
  • Bingham Heritage Trails Association
  • Bottesford
  • Eastwell
  • Harby
  • Harlaxton
  • Hickling
  • Redmile archive
  • Belvoir Villages History and Memories Group
  • Belvoir Angel Society
  • Grantham Canal Society


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