The general Marl and Cataclasite definition can be stated as: Marl is an unconsolidated sedimentary rock consisting of clay and lime. On the other hand, Cataclasite is a type of cataclastic rock that is formed by fracturing and comminution during faulting. It is normally cohesive and non-foliated, consisting of angular clasts in a finer-grained matrix. Along with definition of Marl and Cataclasite, get to know about Properties of Marl and Cataclasite. Get to know more information about Marl and Cataclasite origin and discoverer, etymology and class.
The history of Marl and Cataclasite 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.
Marl and Cataclasite definition gives us a brief idea about the two rocks. In some cases, the definition also gives summary about the Formation of Marl and Cataclasite. In this section, you will know about Marl and Cataclasite Origin and Discoverer. Origin of Marl is whereas Origin of Cataclasite is Swiss Alps, Europe. It is interesting to know the name of Marl and Cataclasite discoverer. The Discoverer of Marl is William Smith and the discoverer of Cataclasite is Michael Tellinger.
Along with Marl and Cataclasite definition, know more about the etymology of Marl and Cataclasite. Etymology of Marl and Cataclasite gives information about origin and formation of a particular rock. Know more about Formation of Marl and Formation of Cataclasite. The etymology of Marl is From Old French marle, from Late Latin marglia while that of Cataclasite is From Old French marle, from Late Latin marglia. The process of formation of rocks defines the class of rock. All the rocks in a class are formed by similar processes. Marl belongs to Sedimentary Rocks while Cataclasite belongs to Metamorphic Rocks. The sub-class, group and other categories of Marl and Cataclasite are listed below.
For Marl,
For Cataclasite,
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