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mineralogists want to see how the mineral is different from its appearance

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Why do mineralogists use senses while examining?

they use their senses because they are supposed to see the Mohs scale of the rocks. They test it out, they put stuff like oil on them, and they smell, touch what it feels like and they hear the noise of the rock by banging it and when their done they write their feelings on an expiriment paper. Thank you :)


What are the four main characteristics in minerals that mineralogists look for while examining them?

The color left on a streak plate when the mineral is scratched on the surface of the plate. Different minerals have different streak colors. The mineral is tested for hardness to see where it lies on the Mohs scale. The crystal structure (othorhombic, tetragonal, triclinic, isometric, monoclinic, or trigonal), will help identify the mineral. Different minerals have different densities and weights.


What are the key differences between a mineral and a rock, and how can one distinguish between the two?

Minerals are naturally occurring substances with a specific chemical composition and crystal structure, while rocks are made up of one or more minerals. One can distinguish between the two by examining their composition, texture, and formation process. Minerals have a defined chemical makeup and crystal structure, while rocks are aggregates of minerals or other materials. Rocks also have a variety of textures, such as coarse-grained or fine-grained, depending on how they were formed.


Relative cooling rates of igneous intrusive rocks can be estimated by comparing rocks?

The relative cooling rates of igneous intrusive rocks can be estimated by comparing the crystal sizes of the minerals within the rocks. In general, rocks that cool more slowly will have larger crystals, while rocks that cool more rapidly will have smaller crystals. Therefore, by examining the crystal sizes of minerals in intrusive rocks, we can infer their cooling rates.


Are rocks the same as minerals?

No, rocks are made up of one or more minerals, while minerals are naturally occurring inorganic substances that have a specific chemical composition and crystal structure. Rocks are composed of minerals, but not all minerals are rocks.

Related Questions

Why do mineralogists use senses while examining?

they use their senses because they are supposed to see the Mohs scale of the rocks. They test it out, they put stuff like oil on them, and they smell, touch what it feels like and they hear the noise of the rock by banging it and when their done they write their feelings on an expiriment paper. Thank you :)


What are the four main characteristics in minerals that mineralogists look for while examining them?

The color left on a streak plate when the mineral is scratched on the surface of the plate. Different minerals have different streak colors. The mineral is tested for hardness to see where it lies on the Mohs scale. The crystal structure (othorhombic, tetragonal, triclinic, isometric, monoclinic, or trigonal), will help identify the mineral. Different minerals have different densities and weights.


What are the key differences between a mineral and a rock, and how can one distinguish between the two?

Minerals are naturally occurring substances with a specific chemical composition and crystal structure, while rocks are made up of one or more minerals. One can distinguish between the two by examining their composition, texture, and formation process. Minerals have a defined chemical makeup and crystal structure, while rocks are aggregates of minerals or other materials. Rocks also have a variety of textures, such as coarse-grained or fine-grained, depending on how they were formed.


What are the remaining steps while examining patient except auscultation palpation?

The appropriate steps to take when examining a patient are inspection, auscultation, palpation and percussion.


What are the four main characteristics in minerals that mineralogists look for while examining?

The color left on a streak plate when the mineral is scratched on the surface of the plate. Different minerals have different streak colors. The mineral is tested for hardness to see where it lies on the Mohs scale. The crystal structure (othorhombic, tetragonal, triclinic, isometric, monoclinic, or trigonal), will help identify the mineral. Different minerals have different densities and weights.


What are four main characteristics in minerals that mineralogists look for while examining them?

The color left on a streak plate when the mineral is scratched on the surface of the plate. Different minerals have different streak colors. The mineral is tested for hardness to see where it lies on the Mohs scale. The crystal structure (othorhombic, tetragonal, triclinic, isometric, monoclinic, or trigonal), will help identify the mineral. Different minerals have different densities and weights.


Why are rocks identified in a different way from minerals?

Rocks and minerals are identified differently because they have distinct characteristics. Minerals are naturally occurring, inorganic solids with a specific chemical composition and crystal structure, whereas rocks are composed of one or more minerals or mineraloids and can also include organic materials. Identification of minerals focuses on their physical and chemical properties, such as hardness and cleavage, while rock identification involves examining the composition, texture, and formation processes of the rock as a whole. This differentiation reflects their unique roles in geology and earth sciences.


How many senses are used while watching TV?

3 senses: Ears for hearing, Eyes for watching, Hand for feeling.


Frank dance model of communication?

"If communication is viewed as a process, we are forced to adapt our examinations and our examining instruments to the challenge of something in motion, something that is changing while we are in the very act of examining it."


What is difference between ferrous and non-ferrous minerals?

Ferrous minerals contain iron, while non-ferrous minerals do not contain iron. Examples of ferrous minerals include magnetite and hematite, while examples of non-ferrous minerals include copper and aluminum. Ferrous minerals are often used in the production of steel, while non-ferrous minerals are used in a variety of industries including electronics and construction.


Burmese python sense its prey by?

it senses by its eyes and listens for it while it camofaluges


Relative cooling rates of igneous intrusive rocks can be estimated by comparing rocks?

The relative cooling rates of igneous intrusive rocks can be estimated by comparing the crystal sizes of the minerals within the rocks. In general, rocks that cool more slowly will have larger crystals, while rocks that cool more rapidly will have smaller crystals. Therefore, by examining the crystal sizes of minerals in intrusive rocks, we can infer their cooling rates.