Detailed autobiography of a chalk in 400 words.
Answers
Chalk is a soft sedimentary carbonate rock, a form of limestone composed of the mineral calcite. Calcite is an ionic salt called calcium carbonate or CaCO3.
It forms under reasonably deep marine conditions from the gradual accumulation of minute calcite shells shed from micro-organisms called coccolithophores.
Flint is very common as bands parallel to the bedding or as nodules embedded in chalk.
It is probably derived from sponge spicules or other siliceous organisms as water is expelled upwards during compaction.
Flint is often deposited around larger fossils such as Echinoidea which may be silicified
Chalk as seen in Cretaceous deposits of Western Europe is unusual among sedimentary limestones in the thickness of the beds.
Most cliffs of chalk have very few obvious bedding planes unlike most thick sequences of limestone such as the Carboniferous Limestone or the Jurassic oolitic limestones.
This presumably indicates very stable conditions over tens of millions of years.
Chalk has greater resistance to weathering and slumping than the clays with which it is usually associated, thus forming tall steep cliffs where chalk ridges meet the sea.
Chalk hills, known as chalk downland, usually form where bands of chalk reach the surface at an angle, so forming a scarp slope.
Because chalk is well jointed it can hold a large volume of ground water, providing a natural reservoir that releases water slowly through dry .
Chalk is mined from chalk deposits both above ground and underground.
Chalk mining boomed during the Industrial Revolution, due to the need for chalk products such as quicklime and bricks.
Some abandoned chalk mines remain tourist destinations due to their massive expanse and natural beauty
The Chalk Group is a European stratigraphic unit deposited during the late Cretaceous Period.
Chalk may also be used as a house construction material instead of brick or wattle and daub: quarried chalk was cut into blocks and used as ashlar, or loose chalk was rammed into blocks and laid in mortar.
There are still houses standing which have been constructed using chalk as the main building material. Most are pre-Victorian though a few are more recent.