Chapter 4 Minerals.

Slides:



Advertisements
Similar presentations
Chapter 3: Matter and Minerals (part II)
Advertisements

Chapter 4 Minerals.
Minerals. A Mineral is… Naturally Occurring – made by nature – not by man.
Minerals Unit 3 Notes. What is a mineral? A mineral must be all of the following: Naturally occurring Inorganic solid (not living) Definite structure.
Mineral Identification Identifying Minerals: Minerals have chemical and physical properties that are unique to each mineral Physical Properties Color.
MINERALS What are minerals used for? Have you ever put salt on your food? Chromoly bicycle frames Jewelry (silver, gold, precious stones) Computer chips.
Earth Science Notes MINERALS. Definition of a Mineral A mineral is a naturally occurring, inorganic, homogeneous solid with a definite chemical composition.
Minerals Chapter 4. What is a mineral Mineral- a naturally occurring, inorganic solid with a specific chemical composition and a definite crystalline.
MINERALS TYvye0CVbU0.
Minerals ***A mineral is a naturally occurring, inorganic, solid with a crystalline structure and a consistent chemical composition***.
Unit 5:.  Minerals are:  Solid  Formed in nature  Inorganic  Of a definite composition  Composed of a particular crystal structure.
Geology Mineral (definition) 1. naturally occurring, 2. inorganic solid 3. with a specific chemical composition 4. a definite crystalline structure  Minerals.
Minerals.
Minerals. A mineral:  Is a naturally occurring inorganic solid  Has a specific chemical makeup  A mineral has a specific crystalline structure.
MINERALS EARTH MATERIALS.
1. A mineral occurs naturally 2. A mineral is solid (definite shape & volume). It’s a crystalline structure.
Minerals UNIT 2 STANDARDS: STATE OBJECTIVES: NCES 2.1.1, 2.1.3, LESSON 2.
Minerals! What is a mineral? In order for a substance to be classified as a mineral it must maintain FIVE characteristics. 1. Naturally occurring 2.
Vocabulary Objectives mineral Luster Cleavage Hardness Gem crystal
What is a Mineral?  Naturally-formed solid substance with a crystal structure Pyromorphite.
Minerals Chapter 3. Minerals – naturally occurring, inorganic solid with a definite structure and composition Minerals – naturally occurring, inorganic.
Minerals. A Mineral is… 1. Naturally Occurring – made by nature – not by man Question: What are the 5 characteristics that all minerals share?
Minerals What are minerals? 7 th Grade Science. Minerals A mineral is defined as a naturally-occuring, inorganic solid with a definite chemical composition.
 Naturally occuring  Solid  Formed by inorganic processes  Have a crystal structure  Definite chemical composition  To be a mineral – MUST HAVE.
Minerals Mineral - A naturally occurring inorganic solid with specific chemical composition and a definite crystalline structure. Materials made in a lab.
Pg. 34 Use the following terms to construct a concept map of the six major crystal systems: Gypsum Topaz Pyrite Triclinic Cubic Hexagonal Tetragonal Crystal.
MINERALS CHAPTER 4. Minerals play important roles in forming rocks and in shaping Earth’s surface, and a select few have played a role in shaping civilization.
5.2 Structure and Composition of Minerals. A. What is a Mineral? Occurs Naturally Is a solid Has definite Chemical Composition Atoms are arranged in an.
Properties and Uses. Identify the physical properties that can be used to identify common minerals Identify major elements in the Earth’s crust Explain.
Minerals. Do Now 1. What is an atom? 2. What is a mineral? Provide 2 examples.
What Are Minerals? Minerals – a naturally occurring, inorganic solid that has a crystal structure and a definite chemical composition.
Topic 11 Rocks and Minerals. Minerals are economically important.
Chapter 30 Minerals and Their Formation. Background Rocks are made up of minerals like how atoms make up molecules Rocks are made up of minerals like.
-presents-. OBJECTIVES: Define a mineral. Describe how minerals form. Identify the most common elements in Earth’s crust. VOCABULARY mineral, crystal,
Minerals Aluminum Silicate minerals Calcium carbonate Iron pyrite.
Minerals Chapter 4 Section 1&2
Minerals.
Learning Target = Matter & Minerals
Minerals Section 4.1.
Minerals Ch. 4.
CHAPTER 4!.
Minerals Ms. Rudisill.
Minerals S6E5. Students will investigate the scientific view of how the earth’s surface is formed. B. Investigate the contribution of minerals to rock.
What is a mineral. Do Now: What do you know about minerals
Minerals.
Chapter 2.1 What Are Minerals?
Mineral Properties.
Bellringer #65: Why are minerals like gems so valuable?
Minerals.
Characteristics and Properties
Minerals.
Minerals S6E5. Students will investigate the scientific view of how the earth’s surface is formed. B. Investigate the contribution of minerals to rock.
Chapter 5.2 – 5.4 Minerals Earth Science 1.
Minerals Earth Science Ch. 2.
What are rocks made of? minerals.
Minerals Chapter 4 Section 1&2
Cleavage The physical property of some minerals that cause them to break along smooth, flat surfaces.
Minerals What are minerals?
Characteristics of Minerals
Minerals S6E5. Students will investigate the scientific view of how the earth’s surface is formed. B. Investigate the contribution of minerals to rock.
Minerals.
CHAPTER 4!.
Minerals.
Minerals Geology: Slides
Unit Introduction.
Earth Science Notes MINERALS.
Minerals.
Minerals of the Earth.
Earth Science Chapter 4 Section 1
Minerals of the Earth.
Presentation transcript:

Chapter 4 Minerals

Mineral: a naturally occurring, inorganic solid with a specific chemical composition and a definite crystalline structure. -Inorganic: Are not alive, nor were ever alive during any part of their existence. -Solids: Definite shape and definite volume Some minerals are elements like sulfur or copper but most are compounds like quartz.

Crystal: A solid in which the atoms are arranged in repeating patterns. -The longer the crystal has to grow, the larger it can get. -The deeper in the ground the magma is (warmer), therefore the slower the cooling rate and the larger the crystal.

Magma: Is molten rock beneath the Earth’s surface

Crystals have 6 basic crystal systems (structures) These are: Cubic, tetragonal, hexagonal, Orthorhombic, Monoclinic and Triclinic. The following slides are examples of these six systems and a mineral for each one.

This is an example of a cubic crystal such as pyrite.

This is an example of Wulfenite with a tetragonal shape This is an example of Wulfenite with a tetragonal shape. The Wulfenite is the yellow mineral.

Here is Pyromorphite and the hexagonal shaped crystal.

Here is Topaz with the Orthorhombic crystal shape.

This is gypsum with the Monoclinic shape.

Last but not least is Feldspar and it’s triclinic shape.

The two main ways in which minerals form. 1) From the cooling of magma 2) From a mineral saturated solution

There are 3000 minerals. There are four groups I want you to know. The Native elements, Silicates, Carbonates, and Oxides.

The native elements: are simply composed of one element such as Copper and Sulfur and are not compounds.

The Silicate group: Are made up of Oxygen and Silicon, the two most abundant elements in the Earth’s crust. It is no wonder then that they make up 96% of Earth’s elements. Quartz and Feldspar are two examples.

The Silicate group: Are made up of Oxygen and Silicon, the two most abundant elements in the Earth’s crust. It is no wonder then that they make up 96% of Earth’s minerals. Quartz and Feldspar are two examples. The shape that they form is called the silica tetrahedron. Oxygen is on the outside and silicon is on the inside

The next group is called the Carbonates. Carbonates are minerals composed of one or more metallic elements with the carbonate compound CO3 Examples are calcite and dolomite often found in limestone or marble. These are basically the only important non silicate rock forming minerals.

Oxides are compounds of oxygen and a metal. Examples are hematite (red streak) and magnetite.

Identifying Minerals Color: The least useful because many minerals have more than one color and many minerals share the same color.

Luster: The way that a mineral reflects light Luster: The way that a mineral reflects light. Your choices are metallic or nonmetallic. Texture: How a mineral feels to the touch. Talc feels greasy and olivine feels granular or “grainy.”

Streak: The powdered and non-weathered color of the mineral. Hardness: A minerals resistance to being scratched. Moh’s hardness scale 1-10 One (Talc) Is the softest and 10 (Diamond) is the hardest.

Cleavage Vs Fracture Cleavage: When a mineral splits relatively easily along one or more flat planes and has either layers or multiple flat surfaces or a geometric shape.

Fracture: When a mineral breaks unevenly due to tightly bonded atoms and have with rough or jagged edges.

Specific gravity: The ratio of weight of a substance to the weight of an equal volume of water at 4 degrees Celsius. For your lab simply put whether it feels light, medium or heavy for its size.

Special properties: Often a mineral will have some unusual characteristic. It may fizz in acid like calcite, smell like sulfur or glow under UV lights such as these minerals showing fluorescence.

Chapter 4 Quiz Describe why sugar is not a mineral. List the two main ways that minerals can form. What is the name of the atomic structure of the silicates and what is the composition of quartz? Why is color the least useful property for identifying minerals? How do you test a minerals hardness? Bonus: How can you tell the difference between the Calcite and Halite?