Presentation is loading. Please wait.

Presentation is loading. Please wait.

Vocabulary Objectives mineral Luster Cleavage Hardness Gem crystal

Similar presentations


Presentation on theme: "Vocabulary Objectives mineral Luster Cleavage Hardness Gem crystal"— Presentation transcript:

1 Vocabulary Objectives mineral Luster Cleavage Hardness Gem crystal
Streak Cleavage Gem Ore Objectives Define a mineral Characterize how minerals are identified What are the different types of metals, non-metals, ores, and gems Vocabulary mineral Luster Hardness Streak Cleavage Gem Ore crystal Silicates

2 Mineral Characteristics
What is a mineral? Mineral Characteristics A mineral is naturally occurring formed by natural processes Inorganic Never living, never will be Solid Specific chemical composition Definite crystalline structure. Earth’s crust is composed of about 3000 minerals.

3 Mineral Characteristics
What is a mineral? Mineral Characteristics Definite Crystalline Structure Atoms in minerals are arranged in geometric patterns that are repeated again and again. A crystal is a solid in which the atoms are arranged in repeating patterns. Triclinic Tetragonal Orthorhombic Monoclinic Hexagonal Cubic

4 Minerals form in 2 ways 1. From Magma
What is a mineral? Minerals form in 2 ways 1. From Magma Small crystals form from rapidly cooling magma. Large crystals form from slowly cooling magma.

5 Minerals form in 2 ways 2. From Solution
What is a mineral? Minerals form in 2 ways 2. From Solution If a solution becomes supersaturated, or overfilled, with another substance, mineral crystals may begin to precipitate, or drop out of solution. When liquid evaporates the element remains and begins crystallize.

6 Mineral Groups About 30 minerals are common in Earth’s crust.
What is a mineral? Mineral Groups About 30 minerals are common in Earth’s crust. Called “rock-forming minerals” because they make up most of the crust. The vast majority of minerals are made up of the eight most common elements.

7 What is a mineral? Mineral Groups Most minerals are formed from the eight most common elements in Earth’s crust.

8 Mineral Groups 1. Silicates
What is a mineral? Mineral Groups 1. Silicates Silicates contain silicon, oxygen, and one or more other elements. make up 96 percent of minerals in Earth’s crust. Most common: feldspar and quartz

9 Mineral Groups 2. Carbonates
What is a mineral? Mineral Groups 2. Carbonates composed of one or more metallic elements with the carbonate compound CO3. the primary mineral found in rocks such as limestone and marble.

10 Mineral Groups 3. Oxides compounds of oxygen and a metal.
What is a mineral? Mineral Groups 3. Oxides compounds of oxygen and a metal. Hematite (Fe2O3) and magnetite (Fe3O4) are common iron oxides and good sources of iron.

11 Mineral Identification
Identifying Minerals Mineral Identification Geologists use several simple tests to identify minerals. Tests are based upon a mineral’s physical and chemical properties.

12 Six Mineral Identification Tests
Identifying Minerals Six Mineral Identification Tests Color is one of the least reliable clues to a mineral’s identity trace elements or compounds within a mineral can change its color. 2. Luster is the way that a mineral reflects light is described as either metallic or nonmetallic. 3. Texture describes how a mineral feels. Texture can be described as smooth, rough, ragged, greasy, soapy, or glassy.

13 Six Mineral Identification Tests
Identifying Minerals Six Mineral Identification Tests Streak is the color of the fine powder of a mineral obtained by scratching or rubbing against a hard white surface. Sometimes, a mineral’s streak does not match the mineral’s external color 5. Hardness is a measure of how easily a mineral can be scratched. one of the most useful and reliable tests for identifying minerals.

14 Mineral Identification
Identifying Minerals Mineral Identification Hardness

15 Six Mineral Identification Tests
6. Cleavage & Fracture - Minerals break along planes where atomic bonding is weak. Cleavage some minerals split easily and evenly along one or more flat planes. Fracture is the ability of minerals to break with arclike, rough, or jagged edges.

16 Identifying Minerals Special Properties Special properties of minerals also can be used for identification purposes. A type of calcite called Iceland spar causes light to be bent in two directions, a process known as double refraction, when it passes through the mineral. Calcite (CaCO3) fizzes when it comes into contact with hydrochloric acid (HCl). Magnetite, an iron ore, is naturally magnetic. The mineral sphalerite produces a distinctive rotten-egg odor when it is rubbed vigorously across a streak plate.

17 Identifying Minerals Mineral Uses Ores An ore is a mineral that contains a useful substance that can be mined at a profit. - If the cost of separating waste material from ore becomes higher than the value of the ore itself, then the mineral is no longer considered to be an ore. The classification of a mineral as an ore may also change if the supply of or demand for that mineral changes.

18 Identifying Minerals Gems Gems are valuable minerals that are prized for their rarity and beauty. Gems such as rubies, emeralds, and diamonds are cut, polished, and used for jewelry. In some cases, the presence of trace elements can make one variety of a mineral more colorful and thus more prized than other varieties of the same mineral.


Download ppt "Vocabulary Objectives mineral Luster Cleavage Hardness Gem crystal"

Similar presentations


Ads by Google