Mineral tests are several methods which can help identify the mineral type. This is used widely Hardness scale is Talc is 1, Gypsum is 2, Calcite is 3, Fluorite is 4, Apatite is 5, Orthoclase Feldspar is 6, Quartz is 7, Topaz is 8, Corundum is 9. Identify minerals based on their physical characteristics. Sort minerals . 6, apatite, 6 to hard steel file. 7, quartz. 8, topaz. 9, corundum. 10, diamond. With a Mohs scale, anyone can test an unknown mineral for its hardness. Imagine you . Describe how color, luster, and streak are used to identify minerals. You need to do simple tests to determine some properties, such as how hard the mineral is. . 3, Calcite. 4, Fluorite. 5, Apatite. 6, Orthoclase feldspar. 7, Quartz. 8, Topaz.
Rock Gallery. Take another look at Figure 3.
Mineral tests are several methods which can help identify the mineral type. This is used widely Hardness scale is Talc is 1, Gypsum is 2, Calcite is 3, Fluorite is 4, Apatite is 5, Orthoclase Feldspar is 6, Quartz is 7, Topaz is 8, Corundum is 9. Identify minerals based on their physical characteristics. Sort minerals . 6, apatite, 6 to hard steel file. 7, quartz. 8, topaz. 9, corundum. 10, diamond. With a Mohs scale, anyone can test an unknown mineral for its hardness. Imagine you .
The Physical properties of minerals are used by Mineralogists to help determine the identity of a specimen. Some of the tests can be performed easily in the field, while others require laboratory equipment. For the beginning student of geology, there are a number of simple tests that can be used with a good degree of accuracy.
The list of tests is in a suggested order, progressing from simple experimentation and observation to more complicated either in procedure or concept. Properties of Minerals The following physical properties of minerals can be easily used to identify a mineral:.
Most minerals have a distinctive color that can be used for identification. In opaque minerals, the color tends to be more consistent, so learning the colors associated with these minerals can be very helpful in identification.
Translucent to transparent minerals have a much more varied degree of color due to the presence of trace minerals. Therefore, color alone is not reliable as a single identifying characteristic. Streak is the color of the mineral in powdered form. Streak shows the true color of the mineral. In large solid form, trace minerals can change the color appearance of a mineral by reflecting the light in a certain way.
Trace minerals have little influence on the reflection of the small powdery particles of the streak. The streak of metallic minerals tends to appear dark because the small particles of the streak absorb the light hitting them. Non-metallic particles tend to reflect most of the light so they appear lighter in color or almost white.
Hardness is one of the better properties of minerals to use for identifying a mineral. The Mohs scale is a set of 10 minerals whose hardness is known. The softest mineral, talc, has a Mohs scale rating of one. Diamond is the hardest mineral and has a rating of ten. Softer minerals can be scratched by harder minerals because the forces that hold the crystals together are weaker and can be broken by the harder mineral.
Minerals tend to break along lines or smooth surfaces when hit sharply. Different minerals break in different ways showing different types of cleavage. Cleavage is defined using two sets of criteria. The first set of criteria describes how easily the cleavage is obtained. Cleavage is considered perfect if it is easily obtained and the cleavage planes are easily distinguished. It is considered good if the cleavage is produced with some difficulty but has obvious cleavage planes.
Finally it is considered imperfect if cleavage is obtained with difficulty and some of the planes are difficult to distinguish. The second set of criteria is the direction of the cleavage surfaces. The names correspond to the shape formed by the cleavage surfaces: Cubic, rhombohedral, octahedral, dodecahedral, basal or prismatic.
These criteria are defined specifically by the angles of the cleavage lines as indicated in the chart below:. Cubic Cleaves in three directions 90o to one anotherRhombohedral Cleaves in three directions but not 90o to one anotherOctahedral Cleaves in four directionsDodecahedral Cleaves in six directionsBasal Cleaves in one directionPrismatic Cleaves in two directions.
Fracture describes the quality of the cleavage surface. Most minerals display either uneven or grainy fracture, conchoidal curved, shell-like lines fracture, or hackly rough, jagged fracture. Mineral crystals occur in various shapes and sizes.
The particular shape is determined by the arrangement of the atoms, molecules or ions that make up the crystal and how they are joined. This is called the crystal lattice. There are degrees of crystalline structure, in which the fibers of the crystal become increasingly difficult or impossible to see with the naked eye or the use of a hand lens.
Microcrystalline and cryptocrystalline structures can only be viewed using high magnification. If there is no crystalline structure, it is called amorphous. However, there are very few amorphous crystals and these are only observed under extremely high magnification. The degree of transparency may also depend on the thickness of the mineral.
Tenacity is the characteristic that describes how the particles of a mineral hold together or resist separation. The chart below gives the list of terms used to describe tenacity and a description of each term. Magnetism is the characteristic that allows a mineral to attract or repel other magnetic materials. It can be difficult to determine the differences between the various types of magnetism, but it is worth knowing that there are distinctions made.
Luster is the property of minerals that indicates how much the surface of a mineral reflects light. The luster of a mineral is affected by the brilliance of the light used to observe the mineral surface. Luster of a mineral is described in the following terms:. Metallic The mineral is opaque and reflects light as a metal would. Submettalic The mineral is opaque and dull.
The mineral is dark colored. Nonmettalic The mineral does not reflect light like a metal. Waxy The mineral looks like paraffin or wax. Vitreous The mineral looks like broken glass. Pearly The mineral appears iridescent, like a pearl.
Silky The mineral looks fibrous, like silk. Greasy The mineral looks like oil on water. Resinous The mineral looks like hardened tree sap resin. Adamantine The mineral looks brilliant, like a diamond. Most minerals have no odor unless they are acted upon in one of the following ways: moistened, heated, breathed upon, or rubbed. Only soluble minerals have a taste, but it is very important that minerals not be placed in the mouth or on the tongue.
You should not test for this property in the classroom. Specific Gravity of a mineral is a comparison or ratio of the weight of the mineral to the weight of an equal amount of water. The weight of the equal amount of water is found by finding the difference between the weight of the mineral in air and the weight of the mineral in water.
Mineral Specimens For Sale. Wholesale Minerals. Complete Rock and Mineral Curriculum Lesson plans, activeities, and ready to use materials for the study of earth science.