Physical properties of minerals

JeromeJerome1 22,303 views 32 slides Jul 11, 2018
Slide 1
Slide 1 of 32
Slide 1
1
Slide 2
2
Slide 3
3
Slide 4
4
Slide 5
5
Slide 6
6
Slide 7
7
Slide 8
8
Slide 9
9
Slide 10
10
Slide 11
11
Slide 12
12
Slide 13
13
Slide 14
14
Slide 15
15
Slide 16
16
Slide 17
17
Slide 18
18
Slide 19
19
Slide 20
20
Slide 21
21
Slide 22
22
Slide 23
23
Slide 24
24
Slide 25
25
Slide 26
26
Slide 27
27
Slide 28
28
Slide 29
29
Slide 30
30
Slide 31
31
Slide 32
32

About This Presentation

Physical properties of minerals such as luster, cleavage, color, streak, hardness, fracture, transparency, magnetism, and tenacity.


Slide Content

Physical Properties of Minerals Prepared by: Jerome A. Bigael , Leyte Progressive High School

To classify a mineral resource, the minerals in the rock should first be identified. Minerals can be identified through their physical properties. In some cases, some minerals may be found in different places and in different forms but their fundamental physical properties remain the same.

1.Color The most evident characteristic of and is usually the first property used to identify minerals. It is a result of the way minerals absorb light. When a mineral absorbs all the color of spectrum except that of a certain color , the mineral will appear in that color

However, this property may not be used in identifying translucent to transparent minerals due to the presence of other trace minerals or impurities.

Mineral Mineral Color Augite Brown, green ,black ,purple Biotite Black, brown, green Calcite Pearlescent and pale colors Dolomite Colorless , pink, pale brown Feldspar Yellow, white, pink, green, gray Hematite Metallic gray or black Hornblende Green, yellow, brown, black Limonite Black, brown, yellow Sulphur Pale gold

Augite = Brown , green ,black ,purple

Biotite = Black , brown, green

Calcite = Pearlescent and pale colors

Dolomite = Colorless , pink, pale brown

Feldspar = Yellow, white, pink, green, gray

Hematite = Metallic gray or black

Hornblende = Green, yellow, brown, black

Limonite = Black, brown, yellow

Sulphur = Pale gold

2.Streak The color of mineral in powder form. Usually the mineral is rubbed on a streak plate to determine its color .

3.Hardness The measure of the mineral’s resistance to scratching. To quantify the hardness of a mineral, the Mohs Scale is used. The harder the mineral, the less prone to scratches.

Mohs Relative Hardness Mineral Common Objects 1 Talc powder 2 Gypsum fingernails 3 Calcite tooth 4 Fluorite Iron nail 5 Apatite Window glass 6 Feldspar Steel file 7 Quartz porcelain 8 Topaz Hardened steel 9 Corundum Sapphire and ruby 10 Diamond none

4.Cleavage and Fracture Cleavage and fracture are used to describe how minerals break into pieces.

5.Crystalline structure/crystal lattice The periodic array of atoms This is a unique arrangement of atoms in a crystal. A hand lens is used for checking the crystalline structure. Non crystalline structure minerals are called “ amorphous ”; special lenses are needed to validate this.

6.Transparency/Diaphaneity Indicate the extent of light that can pass through the mineral. The degree of transparency may depend on the thickness of mineral.

7.Magnetism Indicates the ability of the mineral to attract or repel other materials.

8.Tenacity the mineral’s ability to hold its particles together or the mineral’s level of resistance to stress such as bending, breaking, crushing, or tearing . It indicate if the material is brittle, elastic, malleable, etc.

9.Luster Shows how much light is reflected in a mineral. This depends on the brilliance of light used to observe the surface of the mineral.

Classifications of Luster : Metallic, mineral is opaque and behaves like metal when reflecting light. Submetallic, mineral is opaque, dull, and dark colored . Nonmetallic , mineral does not reflect light like a metal. Waxy, mineral looks like paraffin. Vitreous, mineral looks like a broken glass.

10.Odor The distinct smell of a mineral that is usually released from a chemical reaction manifested when the mineral is subjected to water, heat, air and friction. Sulfur , for example smells like what is emitted when lighting a match. The strength of this smell increases when heated or stuck, giving off an odor similar to rotten eggs.

11.Specific Gravity It is the measure of the density of the mineral. It determines how heavy the mineral is by its weight to water. Specific gravity is used especially when two minerals have the same size and color .

Other Properties: Taste – some minerals have a characteristic taste. For example Halite tastes like salt.

Acid Reaction Some minerals that contain carbonate (CO 3 ) will react with diluted hydrochloric acid ( HCl ), forming carbon dioxide(CO 2 ) gas bubbles. Calcite (CaCO 3 ) will react with HCl

Feel Some minerals such as talc, feel soapy or greasy.

Presence of Striations Some minerals, such as pyrite, have closely spaced fine grooves on their crystal faces.  the state of being marked with stripes or lines.