The general Basalt and Marl definition can be stated as: Basalt is a common extrusive igneous rock formed by the rapid cooling of basaltic lava exposed at or very near the surface of Earth. On the other hand, Marl is an unconsolidated sedimentary rock consisting of clay and lime. Along with definition of Basalt and Marl, get to know about Properties of Basalt and Marl. Get to know more information about Basalt and Marl origin and discoverer, etymology and class.
The history of Basalt and Marl 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.
Basalt and Marl definition gives us a brief idea about the two rocks. In some cases, the definition also gives summary about the Formation of Basalt and Marl. In this section, you will know about Basalt and Marl Origin and Discoverer. Origin of Basalt is Egypt whereas Origin of Marl is Unknown. It is interesting to know the name of Basalt and Marl discoverer. The Discoverer of Basalt is Georgius Agricola and the discoverer of Marl is Unknown.
Along with Basalt and Marl definition, know more about the etymology of Basalt and Marl. Etymology of Basalt and Marl gives information about origin and formation of a particular rock. Know more about Formation of Basalt and Formation of Marl. The etymology of Basalt is From Late Latin Basaltes (variant of basanites ), very hard stone, which was imported from Ancient Greek Basanites while that of Marl is From Late Latin Basaltes (variant of basanites ), very hard stone, which was imported from Ancient Greek Basanites. The process of formation of rocks defines the class of rock. All the rocks in a class are formed by similar processes. Basalt belongs to Igneous Rocks while Marl belongs to Sedimentary Rocks. The sub-class, group and other categories of Basalt and Marl are listed below.
For Basalt,
For Marl,