The general Diatomite and Hornfels definition can be stated as: Diatomite is a fine-grained sedimentary rock which is formed from consolidated diatomaceous earth. On the other hand, Hornfels is a metamorphic rock formed by the contact between mudstone or other clay rich rock, and a hot igneous body, and represents a heat altered equivalent of the original rock. Along with definition of Diatomite and Hornfels, get to know about Properties of Diatomite and Hornfels. Get to know more information about Diatomite and Hornfels origin and discoverer, etymology and class.
The history of Diatomite and Hornfels 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.
Diatomite and Hornfels definition gives us a brief idea about the two rocks. In some cases, the definition also gives summary about the Formation of Diatomite and Hornfels. In this section, you will know about Diatomite and Hornfels Origin and Discoverer. Origin of Diatomite is Germany whereas Origin of Hornfels is New Zealand. It is interesting to know the name of Diatomite and Hornfels discoverer. The discoverer of Diatomite and Hornfels are Unknown.
Along with Diatomite and Hornfels definition, know more about the etymology of Diatomite and Hornfels. Etymology of Diatomite and Hornfels gives information about origin and formation of a particular rock. Know more about Formation of Diatomite and Formation of Hornfels. The etymology of Diatomite is From diatom + -ite1 while that of Hornfels is From diatom + -ite1. The process of formation of rocks defines the class of rock. All the rocks in a class are formed by similar processes. Diatomite belongs to Sedimentary Rocks while Hornfels belongs to Metamorphic Rocks. The sub-class, group and other categories of Diatomite and Hornfels are listed below.
For Diatomite,
For Hornfels,
|
||
|
||
|