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Northamptonshire Stone EarthCache

Hidden : 4/13/2010
Difficulty:
1.5 out of 5
Terrain:
1 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

Drive through almost any Northamptonshire village and you can't fail to notice the mellow golden browns of the stone-built buildings - which give a clear indication of the underlying sandstone and ironstone of the local geology.



The geology of Northamptonshire consists largely of sedimentary strata laid down during the Jurassic period (195 to 145 million years ago). During this period, the current Nene valley formed a narrow channel between the high grounds of the southern Pennines and the north-western shore of the Anglo-Belgian land mass. Rivers from the uplands carried sand and shells which were deposited near the coast in the slower moving waters. Over time the sediments were compacted and cemented together with calcite, silica or limonite to form the limestones, sandstones and ironstones that today form the "Northampton Sand Formation".

These rocks have been quarried for hundreds of years, and a few buildings (such as the Church of the Holy Sepulchre in Sheep Street) still remain from the 12th century. Many of the original pits are long gone, but there are still some working quarries - for example at Pitsford, Harlestone and Pury End.

The coordinates for this cache take you to the site of the former New Duston Quarry, which dates from as far back as the sixteenth century, and maybe much longer. Much of this quarry has now been infilled, and it has been incorporated into a housing estate; but the exposed face is still visible in a number of places. A thick layer of dark brown ironstone can be clearly seen at the base, above which lies a 1.2m layer of sandy limestone (also known as "Pendle"). The upper layer of more yellow sandstone is unfortunately less clear due to downwash from the soil above.

Unusually, this quarry also produced Duston "slates". This is not true slate, but calcerous sandy rock that happens to split suitably along bedding planes - thus producing good quality roofing material.

To log this cache, please email your answers to the following questions via my profile:


  1. Approach the rock face closest to the given coordinates. Which is the harder of the two layers of rock - the upper limestone layer, or the sandstone beneath? Describe at least one feature which supports your answer.
  2. What evidence can you see to show that this stone might be useful for slate roofing?
  3. Photos are optional - but it would be good to see a photo of you at the quarry, or maybe a picture of a stone building from your local village?

Many thanks to Northants Borough Council for their permission and support for this Earthcache (the first in Northamptonshire!)

Additional Hints (No hints available.)