by Gelogia Team | Jul 8, 2026 | Mineralogy
Evaporite minerals are sedimentary minerals that form when saline water evaporates, leaving dissolved minerals behind as crystalline deposits. They commonly develop in environments where evaporation exceeds precipitation, such as arid lakes, coastal lagoons, inland...
by Gelogia Team | Jul 8, 2026 | Mineralogy
Clay minerals are extremely fine-grained, sheet-like silicate minerals that form primarily through the chemical weathering and alteration of rocks and primary minerals. Although they are usually less than 2 micrometers (µm) in size, clay minerals have an enormous...
by Gelogia Team | Jul 8, 2026 | Mineralogy
Soil minerals are the inorganic components of soil formed through the weathering of rocks and minerals over thousands to millions of years. They provide the structural framework of soils, influence nutrient availability, control water retention, regulate soil...
by Gelogia Team | Jul 8, 2026 | Mineralogy
Metamorphism is the geological process in which existing rocks and minerals are transformed by increasing temperature, pressure, and chemically active fluids without completely melting. During metamorphism, minerals become unstable under new conditions and...
by Gelogia Team | Jul 8, 2026 | Mineralogy
The continental crust is the thick, buoyant outer layer that forms Earth’s continents and continental shelves. Unlike the denser oceanic crust, continental crust is composed mainly of silica-rich (felsic to intermediate) rocks, making it less dense and capable...
by Gelogia Team | Jul 6, 2026 | Mineralogy
Earth’s mantle is the thickest layer of the planet, extending from the base of the crust to the outer core at a depth of approximately 2,900 kilometers. It accounts for nearly 84% of Earth’s volume and about 67% of Earth’s mass. Although it is mostly...
