Record ID: LVPL-AFEB44
Object type: LITHIC IMPLEMENT
Broad period: PALAEOLITHIC
County: North Yorkshire
Workflow stage: Awaiting validation
Cream coloured flint flake,- possible scraper. There is some possible re-touching along one edge although this is just as likely to have occurred once in the ground, i.e. plough damage. It is not really possible to date a single flake more precisely than to the prehistoric period.
Created on: Wednesday 14th November 2007
Last updated: Thursday 24th February 2011
Spatial data recorded. This findspot is known as 'NORTH YORKSHIRE', grid reference and parish protected.

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Record ID: LVPL-AFE2E0
Object type: LITHIC IMPLEMENT
Broad period: PALAEOLITHIC
County: North Yorkshire
Workflow stage: Awaiting validation
Cream coloured flint tool- possible scraper. It is drop shaped with a ridge running all the awy down, just off-centre. It is a flake which has been re-touched along one side. It is not possible to date this more precisely than to the prehistoric period.
Created on: Wednesday 14th November 2007
Last updated: Thursday 24th February 2011
Spatial data recorded. This findspot is known as 'NORTH YORKSHIRE', grid reference and parish protected.

Record ID: LVPL-C99AE1
Object type: LITHIC IMPLEMENT
Broad period: PALAEOLITHIC
County: Cheshire East
Workflow stage: Awaiting validation
Flake of a mottled grey flint which cannot be dated more closely than to the general prehistoric period. The flake is an irregular shape and quite thin in section.
Created on: Monday 22nd October 2007
Last updated: Thursday 24th February 2011
Spatial data recorded.

Record ID: LVPL-426334
Object type: FLAKE
Broad period: PALAEOLITHIC
County: Cheshire East
Workflow stage: Awaiting validation
Edge damaged flint flake from the the prehistoric period. It is roughly triangular in section and in plan. It is made from a grey flint. The dorsal face has a central ridge which is broken where the flint is notched. The ventral face is smooth although slight cnchoidal ripples can be seen. One long side of the flint has been broken and chipped, probably when it has been in the ground. This is likely to be a bi-polar flake which would explain the different fracture lines.
Created on: Monday 4th June 2007
Last updated: Thursday 24th February 2011
Spatial data recorded.