noun a rare type of granitic rock containing a high percentage of orthoclase feldspar
adjective relating to or characteristic of adamellite rock
Adamellite is a type of granitic rock characterized by its pink or reddish color and containing large crystals of feldspar and quartz. It is commonly found in mountain ranges and is associated with the formation of plutons.
In mineralogy, adamellite is a variety of granite that typically contains orthoclase feldspar, quartz, and plagioclase feldspar. It is often used in construction and as a decorative stone.
Adamellite is studied in petrology as a part of the larger field of igneous rocks. Its composition and texture provide valuable information about the geological processes that formed it.
Adamellite is a type of granitic rock that is commonly found in igneous intrusions. Geologists study adamellite to understand the geological history and formation of certain regions.
Mineralogists may analyze the mineral composition of adamellite samples to identify the specific minerals present and their proportions.
Civil engineers may encounter adamellite in construction projects where the rock is used as a building material or as a foundation for structures.
Archaeologists may come across adamellite artifacts or structures in their excavations, providing insights into past civilizations and their use of materials.
Environmental scientists may study the impact of adamellite mining or extraction on the surrounding ecosystem and work on strategies for sustainable resource management.