chalk
Chalk
Chalk
Chalk.
Chalk
In outcrops and cliffs it is possible to see multiple layers of rock exposed in one place, which makes it easier to study a set of rocks.
Yes, coral beaches are a sedimentary deposit, much as a sand beach would be. Bits of shell also precipitate out of water to congeal into limestone formations, or the bodies of calcareous coccolithophores settle to form chalk deposits, as in the famous white cliffs of Dover. Limestone is regarded as a sedimentary rock.
There are MANY places. The types can also vary greatly. For examplelime stone is quarried in Iowa. It also makes the underlying strata in Mexico south of Cancun. The stone is soft and over MANY years holes form called cynotes and caves. In England, the white cliffs of Dover are white primarily because of the limestone content. Sandstone is also a relatively soft rock. Much sandstone is located in the desert area of the Southwest US. There are some interesting rock formations formed by the wind eroding the sandstone.
Sandstone and namurian shale.
It was formed by erosion around the cliffs, it is a harder rock so it is eroding more slowly
The white cliffs of Dover are composed of chalk.
Calcium carbonate, specifically chalk.
The material the cliffs are made from is CHALK
The White Cliffs of Dover are made of chalk which is a sedimentary rock.
A cliff face in the county of Dover (England) where the rock underneath the grass is shown on the coastline. The rock is limestone.
Yes, they are relatively strong but there are stronger types of rock such as quartzite.
The 'white Cliffs of Dover" are made of chalk and a little crumbly.
you are dum
The song is 'Cliffs of dover' by Eric Johnson.
That would depend on where the beach is located. Beaches are normally composed of loose sand or remains of animals living in the sea. Any rock found on a beach could have come from cliffs nearby, from under the sea or from some distance along the coast and could be any type of rock.
They're made of limestone (chalk).
In outcrops and cliffs it is possible to see multiple layers of rock exposed in one place, which makes it easier to study a set of rocks.