Levallios Flake

After my second season at Grimes Graves, in 1974, the director G.de G Sieveking asked for volunteers to work a small excavation he had planned in North London.

The place was in Acton, at a school,  the Haberdashers Aske School. The property was changing hands and would become the Japanese School in the new term. 

Mr Sieveking had been given permission and support to excavate part of the grounds of the school as it was known that a knapping floor was present in the area yielding an unusual style of knapping technique,  the Levallois technique. 

The flints that we were hoping to find were large and sort of triangular.

The site of our excavation was just outside the window into the head teacher's office, and as we had not been told about the circumstances of the change of hands of the property it felt slightly sacriligeous to be cutting into turf that we as children, not that long ago, would have been forbidden to walk on.

The turf was tidily cut and carefully stacked for re-laying. When that was done we were told that the finds that we could expect to find would be in the material immediately beneath the turves, 

That material was called "loess", which, we were told was Dutch for loose.

The material that we were digging through was not loose, it was the hardest soil that any of us had had the misfortune to be required to excavate. It was as hard as solid chalk, but even then chalk would have been much easier to work than this. There were a few mattocks on site, but not many, so for the four weeks of the dig we stabbed the ground with our trowels, accepting the punishment that the work did to our hands, wrists, and arms.

One of the only people equipped with a mattock was Phil Harding,  and he used it to good effect, finding the only levallois flake of the entire excavation. 

Unfortunately his find received a direct hit from the matlock, breaking into a lot of shard-like pieces.

At the time it was not lost on me that while we were digging a material called "loose", what we were actually working was anything but loose.

It was not though until recently that, in researching geology I discovered the term "overconsolidated" which is material that has been subjected to a huge mass laid over it. Indeed the mass was so great that all the molecules of air and water that had been in the material when it was laid down were compressed out of it.

The actual material here was chalky white, and was probably of the same material as that I found under the Dorset Barrow. 

While the material under the Dorset Barrow was fluffy and loose, and indeed may have been wind blown, the stuff in Acton was nearly as hard as concrete, which I take to mean that at some stage in the last million years the ice sheets from at least one ice age were laid over parts of London. 

The weight of hundreds of metres of ice may well have been enough to overconsolidate the wind blown stuff.

Piece by piece, I begin to map out where the ice sheets over Britain were, and where they were not, or where they weren't very thick anyway. 

This in an effort to better understand what happened in the ice ages, and how they shaped Britain. 

Jeffery Nicholls 

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