Chapter 5 Outline/Study Guide
Minerals of Earth’s Crust
Mineral – a natural inorganic solid that has a characteristic chemical compositionand physical properties.
Characteristics of Minerals
In order to determine if a substance is a mineral a scientist will ask the following questions
- Is the substance inorganic?
- Inorganic - not made up of living things or the remains of living things
- Does the substance occur naturally?
- minerals form and exist in nature, they are not manufactured (man made)
- Is the substance in crystalline form?
- atoms need to be arranged in a regularly repeating crystalline structure
- Does the substance have a consistent chemical formula?
- The ratio of the substances does not vary
- Is the substance a solid?
Therefore, a substance is not a mineral if it does not meet the above information. (ex. granite is not a mineral)
Kinds of Minerals
The two main groups of minerals are silicate and nonsilicate. The chemical composition of a mineral helps determine what group it belongs in.
Silicate minerals–(96% of Earth’s crust) a mineral that contains a combination of silicon and oxygen and may also contain one or more metals. (Examples – quartz, feldspars, orthoclase, plagioclase, ferromagnesian)
Silicates are the most common group of minerals.
Nonsilicate minerals - (4% of Earth’s crust) minerals that do not contain compounds of silicon and oxygen
Please answer the following questions on your own
What do you use to measure the hardness of a mineral?
What hardness does each item represent?
What is reclamation?
Make sure you are able to determine if an item is a mineral or not based on the characteristics of minerals.
Identifying Minerals (7 characteristics)
Process if identifying minerals
- color – most easily observed, but it is not a good identifier since color may change.
- luster – the way that a mineral reflects right(metallic, non-metallic, dull, vitreous, glassy, pearly, waxy)
- streak – the color of a mineral in powder form (you use a streak plate to help determine this)
- hardness – ability of a mineral to resist scratching. (Moh’s hardness scale)
- fracture – tendency of a mineral to break and form uneven, irregular surfaces.
- cleavage – tendency of a mineral to split and form flat, smooth surfaces.
- specific gravity – the ratio of the weight of the mineral to the weight of an equal volume of water – how heavy the mineral feels. (similar to density)
density – ratio of a substances mass to its volume.
Moh’s Hardness Scale
1 – talc(softest)
2 – gypsum
3 – calcite
4 – fluorite
5 – apatite
6 – feldspar
7 – quartz (hardest common mineral)
8 – topaz
9 – corundum
10 – diamond (hardest)
Special Properties of Minerals
Radioactive- when unstable atomic nuclei decay over time into stable nuclei.
If a mineral is fluorescentit shines under UV light.
Magnetism – the presence of iron-ore in mineral. This can be tested with a magnet. So if iron is in the mineral it will be magnetic.
Double refraction – when a clear mineral displays two images placed on top, found in calcite.