Camulodunum type 262, le type Besançon and Central Gaulish granite-tempered ware
||TF2 ’Standard fabric‘ /cf.B134
IF: plagioclase, orthoclase biotite mica feldspar
- shattered? crushed?
weathered rock not moved from where it was weathered.
Inclusion looks like glass (?obsidian)
Pyroxene, lava - fresh feld phenocryst (2 egs)
Volcanic rather than lava as such
Basically granitic, feldspars much fresher,
typical of volcanic feldspar - Massif Central
basic igneous rock and opaque inclusions