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Red |
| Terracotta probably cut from roof tile or brick. |
 |
Blue lias Dark blue grey to very
light grey/white |
| The tessera and stone tiles are identical
to the lower strata beds from the now worked–out Station
Quarry at Charlton Mackerell in Somerset. This would have
been formed from limy mud deposits in non-turbulent seas.
Blue lias can also be seen at Kilve on the coast in north
Somerset, and Lyme Regis on the Dorset coast. |
 |
Bright white |
| Possibly a very light Blue Lias or the
much harder geologically compressed chalk from the Purbeck
Ridge in Dorset. |
 |
Yellow-brown |
| Sandy limestone but with iron giving the
browner colour. Inferior Oolite (Jurassic,
appears to contain little egg shapes) as found at Seavington
St. Mary quarry, 3 kms to north west of the villa. |
 |
Sandy or pale yellow |
| Sandy limestone. Inferior Oolite
also found at Seavington St. Mary. |
|
Golden |
| Ham Hill Stone. Sandy limestone containing
shell fragments. Ham Hill by Stoke under Ham can be seen
to the east from the villa site. |
 |
Mortar |
| It contains smooth, well-rounded, very coarse
white, translucent sand grains probably derived from the
Upper Greensand. The mortar contains a lot of angular,
small flint chips. Possibly ‘sweepings’ or
sievings or broken with a hammer? |