The "Bathonien" of some French geologists differs from the English Bathonian in that it includes at the base the zone of the ammonite Parkinsonia Parkinsoni, which in England is placed at the summit of the Inferior Oolite.
The white sandstone in the Clynelish quarry belongs to the Brora Formation, of the Callovian and Oxfordian stages (formerly Middle Oolite) of the Mid-Late Jurassic.
Dundry is notable for its stone: the yellow oolitic limestone from local quarries such as Dundry Main Road South Quarry and the Dundry Downs (to the west of the village) is found even at Cardiff Castle, a fort originally built by the Romans to defend against Anglo-Saxon invasions.
Dundry Main Road South Quarry is a 0.7 hectare geological Site of Special Scientific Interest near the village of East Dundry, because of the number of fossils in the inferior oolite.
The Inferior Oolite, capping the main north-west facing escarpment, comprises up to 100m of mainly oolitic limestones including the Cheltenham freestone - quarried most extensively at Leckhampton and used widely in the distinctive Regency architecture of Cheltenham.
Born in Oxford, Whiteaves was educated at private schools, and afterwards worked under John Phillips at Oxford (1858–1861); he was led to study the Oolitic rocks, and added largely to our knowledge of the fossils of the Great Oolite series, Cornbrash and Corallian.
The Pierre de Jaumont (lit. "stone of Jaumont") is an oolitic limestone of the Upper Jurassic, found in Malancourt-la-Montagne, part of the commune of Montois-la-Montagne, in Lorraine, France.
A Geodiversity audit of the site recorded pale to dark grey well bedded Carboniferous Limestone dipping consistently southwards with a small area of overlying horizontally bedded buff-coloured Jurassic oolitic limestone forming an angular unconformity.