The general Mylonite and Marble definition can be stated as: Mylonite is a metamorphic rock formed by ductile deformation during intense shearing encountered during folding and faulting, a process termed cataclastic or dynamic metamorphism. On the other hand, Marble is a non-foliated metamorphic rock which is composed of recrystallized carbonate which is formed when limestone is exposed to high temperatures and pressures over a long time. Along with definition of Mylonite and Marble, get to know about Properties of Mylonite and Marble. Get to know more information about Mylonite and Marble origin and discoverer, etymology and class.
The history of Mylonite and Marble gives information about where the rock was found and who was its discoverer. Almost each and every aspect of Earth's history is recorded in rocks be it the volcanoes which were erupted or the plants, animals and organisms which are now extinct, as rocks are present from millions of years.
Mylonite and Marble definition gives us a brief idea about the two rocks. In some cases, the definition also gives summary about the Formation of Mylonite and Marble. In this section, you will know about Mylonite and Marble Origin and Discoverer. Origin of Mylonite is New Zealand whereas Origin of Marble is Egypt. It is interesting to know the name of Mylonite and Marble discoverer. The discoverer of Mylonite and Marble are Unknown.
Along with Mylonite and Marble definition, know more about the etymology of Mylonite and Marble. Etymology of Mylonite and Marble gives information about origin and formation of a particular rock. Know more about Formation of Mylonite and Formation of Marble. The etymology of Mylonite is From Greek mulōn mill + -ite while that of Marble is From Greek mulōn mill + -ite. The process of formation of rocks defines the class of rock. All the rocks in a class are formed by similar processes. Mylonite and Marble belong to Metamorphic Rocks. The sub-class, group and other categories of Mylonite and Marble are listed below.
For Mylonite,
For Marble,