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crystallization

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What is hydrogenous sediments made of?

minerals that crystallize directly from ocean waters


Minerals that crystallize directly from seawater are examples of?

Minerals that crystallize directly from seawater are examples of evaporite minerals. These minerals form when seawater evaporates, leaving behind dissolved minerals that precipitate and crystallize into minerals like gypsum, halite, and calcite. Evaporite minerals are commonly found in areas with high rates of evaporation, such as salt flats and arid regions.


Where do minerals crystallize from evaporating water?

Minerals remain as a solid residue.


Can minerals crystallize out of magma when it melts?

Yes, minerals can crystalize when magma melts.


How does a chemical rock form?

Minerals crystallize from a solution.


Which ferromagnesian minerals and which of the feldspar's would be the first minerals to crystallize?

The first ferromagnesian mineral to crystallize is usually olivine, followed by pyroxene and amphibole. Among the feldspars, plagioclase feldspar is usually the first to crystallize, followed by potassium feldspar.


How does a chemical sedimentary rock form?

When minerals crystallize from a solution


What is cenmentation?

Cementation is when minerals crystallize and glue the sediments together


What type of the sediment forms from minerals that crystallize from seawater?

Chemical sedimentary rocks, such as limestone and chert, can form when minerals crystallize from seawater. These rocks are typically composed of minerals that precipitate out of solution in bodies of water, including oceans.


Do minerals form when hot water solution cools and the minerals crystallize?

This is one method of crystal formation.


Which forms when minerals dissolve in a water solution crystallize?

Chemical Rock


What process is required for minerals to crystallize to magma?

Minerals in magma crystallize through the process of cooling and solidification. As magma cools, atoms and ions within the molten rock arrange themselves into an ordered, repeating three-dimensional pattern, forming mineral crystals. The specific minerals that crystallize depend on factors such as temperature, pressure, and chemical composition of the magma.