These are called veins
Mineral deposits beneath Earth's surface that differ from the surrounding rocks are called "ore deposits." These deposits often contain valuable minerals or metals that can be economically extracted. They can form through various geological processes, such as igneous, sedimentary, or metamorphic activities. The specific composition and concentration of minerals in these deposits make them significant for mining and resource extraction.
what mineral deposit do we have in the country
what mineral deposits do we have in the phillipines ? where are they located and why only in those places
sulfur rock
You can remove mineral deposits from your teapot with a mild vinegar solution.
what mineral deposits do we have in the country? where are they located?
Ores are deposits of economically valuable minerals, usually - but not necessarily metallic minerals.
Vein
The northern most regions of new hampshire have an extrermely abundant amount of mineral deposits. Searching through the mountains for mineral deposits will only further distribute the minerals amongst the lands.
what mineral deposits do we have in the phillipines ? where are they located and why only in those places
John Drew Ridge has written: 'Annotated bibliographies of mineral deposits in the Western Hemisphere' -- subject(s): Bibliography, Ore deposits 'Selected bibliographies of hydrothermal and magnetic mineral deposits' -- subject(s): Bibliography, Mines and mineral resources 'Annotated Bibliographies of Mineral Deposits in Europe' -- subject(s): Bibliography of bibliographies, Ore deposits
Mineral deposits are often found around the perimeter of igneous intrusions due to the process of hydrothermal alteration, where hot, mineral-rich fluids generated by the cooling magma migrate through fractures in the surrounding rock. As these fluids cool and react with the surrounding rocks, they can precipitate valuable minerals. Additionally, the temperature and pressure conditions around the intrusion create a favorable environment for the concentration of certain minerals, leading to the formation of ore deposits. This spatial relationship is commonly observed in various mining districts worldwide.