The Parent Rock Of Marble Is

Slate phyllite schist gneiss.

The parent rock of marble is.

Thus it can be one of several rock types often limestone though it can conceivably also be dolomite or travertine etc. In its pure form marble is a white stone with a crystalline and sugary appearance consisting of calcium carbonate caco3. See full answer below. The parent rock of marble is.

Shale granite hornblende garnet muscovite schist. The two main influences are the kind of limestone that makes up the parent rock and the kind and degree of metamorphism. Which of the following is a granular non foliated metamorphic rock. Both marble and quartzite.

What is the parent rock of the metamorphic rock marble. The parent rock of marble can be composed of calcite or dolomite. The parent rock of slate garnet muscovite schist and phyllite is. The parent rock of hornblende schist is.

Limestone is the parent rock of marble. 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. Marble is a metamorphic rock that forms when limestone is subjected to the heat and pressure of metamorphism. The parent rock of quartzite is.

Usually marble contains other minerals including quartz graphite pyrite and iron oxides. The parent rock of marble is. 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. Depending on the composition of the marble rock it can be one or both of the parent rocks that.

The parent rocks of marble are dolomite and calcite. Which series of rocks is in order of increasing metamorphism. The name of the rock which has resulted from partial melting is. It can be most any color including white black reds greens and more.