geology - lincolnshire · pdf fileh erit age l incolnshire y o u r w o l d d o w n geology the...

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H ERITAGE L INCOLNSHIRE Y o u r W o l d D o w n Geology The geology of the west facing escarpment between Claxby and Neleton is reflected in the landscape. The relavely hard limestone and ironstone beds are separated by soſter, less durable mudstones, clays and sands. This is an unstable mix and there is much evidence of landslips along the boom of the slope. The iron ore was extracted from the Claxby Ironstone Formaon. The main rocks in the Neleton area – ironstone, sandstone, limestone, mudstone and chalk - were deposited during the Cretaceous era around 65 million to 135 million years ago. Overlying sands and gravels came later, during the ice ages of the Pleistocene era, around 1.8 million years ago. Deposits of ironstone were mined and quarried during the last century at three locaons near Neleton Top. The low grade ore (20-30% iron content) was transported by rail to Scunthorpe for smelng. A small outcrop of Claxby Ironstone close to a collapsed entrance to the Claxby mine. It is a coarse iron rich oolite (sedimentary rock formed from ny, spherical, fish-egg like grains), containing many fossil shells. The fossilised remains of squid like creatures called belemnites are common in the sediments of the Claxby and Tealby Formaons Claxby Ironstone was also used locally as a building material – Neleton Church is a fine example and demonstrates that whilst being pleasing to the eye, Claxby Ironstone is not parcularly resistant to the elements. Contains Brish Geological Survey materials © NERC Fossils in wall of Neleton Church Belemnite in Claxby Ironstone Geology map of Claxby- Neleton Area Geomorphology at Claxby Mine Claxby Ironstone outcrop at Claxby Mine Close up image of Claxby Ironstone showing ‘gunshot’ effect caused by ny, spherical ooliths The Down Your Wold volunteers would like to thank H Bourne & Sons, the Brant family and the Society for Lincolnshire History and Archaeology for their help and assistance. There is no public access to any of the above sites. All images are copyrighted. Mine buildings Nettleton top Ancholme Clay Spilsby Sandstone Claxby Ironstone Tealby Series Carstone Red Chalk Chalk Nettleton bottom Landslip Blown sand A e r i a l r o p e w a y Mine tunnels Mine tunnels Chalk quarry Caistor High Street

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Page 1: Geology - Lincolnshire · PDF fileH ERIT AGE L INCOLNSHIRE Y o u r W o l d D o w n Geology The geology of the west facing escarpment between Claxby and Nettleton is reflected in the

H E R I T A G E L I N C O L N S H I R E

Your

Wold

Down

Geology

The geology of the west facing escarpment between Claxby and Nettleton is reflected in the landscape. The relatively hard limestone and ironstone beds are separated by softer, less durable mudstones, clays and sands. This is an unstable mix and there is much evidence of landslips along the bottom of the slope.

The iron ore was extracted from the Claxby Ironstone Formation.

The main rocks in the Nettleton area – ironstone, sandstone, limestone, mudstone and chalk - were deposited during the Cretaceous era around 65 million to 135 million years ago. Overlying sands and gravels came later, during the ice ages of the Pleistocene era, around 1.8 million years ago. Deposits of ironstone were mined and quarried during the last century at three locations near Nettleton Top. The low grade ore (20-30% iron content) was transported by rail to Scunthorpe for smelting.

A small outcrop of Claxby Ironstone close to a collapsed entrance to the Claxby mine. It is a coarse iron rich oolite (sedimentary rock formed from tiny, spherical, fish-egg like grains), containing many fossil shells.

The fossilised remains of squid like creatures called belemnites are common in the sediments of the Claxby and Tealby Formations

Claxby Ironstone was also used locally as a building material – Nettleton Church is a fine example and demonstrates that whilst being pleasing to the eye, Claxby Ironstone is not particularly resistant to the elements.

Contains British Geological Survey materials © NERC

Fossils in wall of Nettleton Church

Belemnitein Claxby Ironstone

Geology map of Claxby-Nettleton Area

Geomorphology at Claxby Mine

Claxby Ironstone outcrop at Claxby Mine

Close up image of Claxby Ironstone showing ‘gunshot’ effect caused by tiny, spherical ooliths

The Down Your Wold volunteers would like to thank H Bourne & Sons, the Brant family and the Society for Lincolnshire History and Archaeology for their help and assistance. There is no public access to any of the above sites. All images are copyrighted.

Minebuildings

Nettletontop

Ancholme ClaySpilsby SandstoneClaxby IronstoneTealby SeriesCarstoneRed ChalkChalk

NettletonbottomLandslip

Blown sand

Aerial ropeway

Mine tunnels Mine tunnels

Chalkquarry

CaistorHigh Street