Download presentation
Presentation is loading. Please wait.
1
Minerals What are minerals?
A naturally occuring, crystalline inorganic substance. What properties do we use to classify minerals? (7 properties) Color Luster Streak Crystal shape Hardness Cleavage Density
2
What is a Mineral? 1. Occurs naturally 2. Solid
3. Has a defined chemical composition 4. Atoms arranged in an orderly pattern 5. Was never alive- Inorganic
3
Mineral Identification
Approximately 4,000 known minerals About 30 are common These are the rock forming minerals (because they are the most common minerals in rocks!) Your ESRT helps you identify minerals
4
Formation From cooling of magma or lava Evaporites Precipitates
5
Distribution of elements within the lithosphere
6
Structure of Minerals
7
Types of minerals Native Silicates Silica tetrahedron Non-silicates
Composed of a single element Silicates Composed of Silicon and Oxygen Silica tetrahedron Non-silicates Oxides- Contains O+2 Sulfates- Contains Sulfur Carbonates- Contains Carbon
8
Minerals Minerals are identified by their physical characteristics. These include: Streak Color Luster Hardness Density (specific gravity) Crystal structure
9
Mineral ID What is the streak of hematite? (hint:use your ESRT)
The color of the powdered mineral Test by rubbing sample against unglazed porcelain What is the streak of hematite? (hint:use your ESRT)
10
Streak
11
Mineral ID Why is color not very reliable (ESRT)? Color
least reliable Why is color not very reliable (ESRT)?
12
Color “Don’t judge a mineral by its color”
13
Mineral ID Luster The way light reflects from a freshly broken surface
Metallic Nonmetallic
14
Luster
15
Hardness
16
Hardness
17
Arrangement of Atoms Influences Cleavage:
18
Cleavage Minerals that do not have cleavage tend to fracture
Look for flat or step like surfaces Minerals that do not have cleavage tend to fracture
19
Be careful: cleavage is not the same as crystal shape!
form when the mineral is allowed to cool and the molecules arrange themselves in a repeating pattern. Size and appearance of crystals depend on environment of formation Crystals need room to grow. Crystal form is the way a mineral GROWS Cleavage and fracture Planes along which the mineral tends to break Cleavage is the way a mineral BREAKS
20
Density Specific Gravity
Ex: Gold has a density of 19 g/cm3 , if we have a 2 gram sample, what would the samples volume be?
21
Mineral ID Density
22
Other Properties Bubbles “fizzzz”
23
Fluorescence
24
(ESRT) What is the hardness of olivine?
Does calcite exhibit cleavage when broken? What is one of the uses of biotite? Which minerals react to acid?
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.