Noun:

डेवनशायर का (निवासी),

senonian's Usage Examples:

The Senonian chalk, or " White Limestone," is hard, with numerous bands of flint, and suffered from denudation in early Eocene times.

The Senonian limestone itself, which rests in the extreme north on Trias or even on the schists, is often conglomeratic and glauconitic at the base, the pebbles being worn from the old metamorphic series.

The Turonian is also sandy, but in most areas was not deposited, or has been denuded away during a local uplift that preceded Senonian times.

In the last-named year a Senonian named Drappes threatened the Provincia, but was captured and starved himself to death.

Only the higher divisions (Senonian and Danian) of the system are represented.

There is a continuous transition between the Senonian and Danian, proving that the Algerian region did not participate in the immersion which occurred in Provence and in the Corbieres of southern France during the Danian epoch.

The Senonian series is represented by the White Limestone, a hardened chalk with flints, which is often glauconitic and conglomeratic at the base.

The Senonian consists of a central facies with Micraster peini; a meridional facies with Ostrea; and a northern facies developed round Tunisia with large forms of Inoceramus and echinoids.

Limestones and marls represent the stages Cenomanian to Upper Senonian.

Beginning with the Aptian and Albian the sea again gradually spread over the country and attained its maximum in the early part of the Senonian epoch, when once more the ancient massifs of the Central Plateau, Brittany and the Ardennes, alone rose above the waves.