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∙ 15y agoOne example in particular comes to mind. Kimberlite pipes, former explosive conduits for volcanic material, are great sources of the mineral diamond, having ripped apart the mineral from their point of formation deep in the Earth and thrusting them toward the surface. Underground salt domes are virtually unlimited sources of the mineral halite (table salt). The mineral calcite is produced primarily from the sedimentary rock limestone. Sandstone is a primary source of the mineral quartz. Shale deposits are great sources for clay minerals used in ceramics and brick making.
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∙ 15y agoRock Bottom
Roles of microbes in geological processes can be identified in the geomicrobial processes. In these processes, microbes help in transformation of minerals and metals.
Schists are a group of minerals that are characterized by having plate-like crystal structures that slide easily over one another. Common examples are Mica and Graphite.
6 types of silicate minerals
Minerals that crystallize directly from seawater are examples of hydrogenous sediment.
Minerals are natural chemicals (in the geological sense).
which of the following minerals would be most concentrated
Maybe minerals is a type of structures of phosphates or carbonates
Geological surveying.
•Formation of minerals via biology
yes
Geological bioturbation is the process where organisms, such as burrowing animals or bottom-dwelling organisms, disturb and mix sediments in the Earth's crust. This activity can create structures and patterns in the sediment layers, influencing the distribution and composition of rocks and minerals. It plays an important role in sedimentary processes and can provide insights into past environmental conditions.
Rock Bottom
Ewan!
the geological changees are occuring in the fossil fuels rocks and other minerals
Roles of microbes in geological processes can be identified in the geomicrobial processes. In these processes, microbes help in transformation of minerals and metals.
Schists are a group of minerals that are characterized by having plate-like crystal structures that slide easily over one another. Common examples are Mica and Graphite.