Marble is formed by the metamorphosis of limestone by heat and pressure.
The parent rock of a marble is a.
Therefore limestone may be called the parent rock or more correctly the protolith of marble.
Marble is commonly used for sculpture and as a building material.
Parent rock also referred to as substratum refers to the original rock from which something else was formed it is mainly used in the context of soil formation where the parent rock or parent material normally has a large influence on the nature of the resulting soil for example clay soil is derived from shale while sandy soil comes from the weathering of sandstones.
It is composed primarily of the mineral calcite caco 3 and usually contains other minerals such as clay minerals micas quartz pyrite iron oxides and graphite under the conditions of metamorphism the calcite in the limestone recrystallizes to form a rock that is.
Slate is a foliated displaying layers or banding metamorphic rock and its parent rock was shale or mudstone.
Marble is a metamorphic rock that forms when limestone is subjected to the heat and pressure of metamorphism.
Start studying parent rocks of metamorphic rocks.
The two main influences are the kind of limestone that makes up the parent rock and the kind and degree of metamorphism.
Marble is a non foliated metamorphic rock no layers or bands and its parent rock.
There is a lot of variation in the color and texture of marble.
Marble is a metamorphic rock composed of recrystallized carbonate minerals most commonly calcite or dolomite marble is typically not foliated although there are exceptions in geology the term marble refers to metamorphosed limestone but its use in stonemasonry more broadly encompasses unmetamorphosed limestone.
Marble is a metamorphic rock formed when limestone is subjected to high pressure or heat.