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13y ago

They use a microscope.

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Q: What do scientist use to study the crystal structure of mineral?
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Where do mineralogists study?

The study of chemistry, crystal structure, and physical properties of minerals


What do scientists use to study crystal structure?

x rays


Could you study the structure of DNA in a living specimen?

Yes. Scientist Wardisiani proved it


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A chemist could possibly study the structure of matter.


Is a cosmetologist a scientist?

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Are geology and crystallography closely related?

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Particle physicists. or Quantum Physicists or Atomic Physicists


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What branch of science involves the study of minerals?

There are many branches in science. Mineralogy the study of minerals. However, it is also the study of the chemistry, crystal structure, and physical properties of minerals


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Wheeler Pedlar Davey has written: 'Study of crystal structure [and] its application'


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Crystallography gives the geologist a basic knowledge of minerals. This helps them in their study of rocks. It helps him in the morphological and structural study of the crystal structure.


What are 5 facts about minerals?

A mineral is a naturally occurring solid formed throughgeological processes that has a characteristic chemical composition, a highly ordered atomic structure, and specific physical properties. Minerals in composition from pure elements and simple salts to very complex silicates with thousands of known forms The study of minerals is called mineralogy. A mineral is an element or chemical compound that is normally crystalline and that has been formed as a result of geological processes. Physical properties commonly used are: Crystal structure and habit: See the above discussion of crystal structure. A mineral may show good crystal habit or form, or it may be massive, granular or compact with only microscopically visible crystals. Hardness: the physical hardness of a mineral is usually measured according to the Mohs scale. This scale is relative and goes from 1 to 10. Minerals with a given Mohs hardness can scratch the surface of any mineral that has a lower hardness than itself.