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Minerals Let’s Review Mineral Ide ntification

Minerals

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Let’s Review…. Minerals. Mineral Identification. Mineral Definition:. Naturally occurring Solid Orderly crystal structure Definite chemical composition 5. Inorganic. How Minerals Form (4 Major Processes). Crystallization of Magma. 2. Precipitation (evaporated H 2 O). - PowerPoint PPT Presentation

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Mineral Definition:

1.Naturally occurring2.Solid3.Orderly crystal structure4.Definite

chemical composition

5. Inorganic

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How Minerals Form(4 Major Processes)

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1.Crystallization of Magma

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2. Precipitation (evaporated H2O)

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3. High Pressure & Temperature

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4. Hydrothermal Solutions

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Rocks

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Rock Cycle DrawingDraw, label, and color a diagram of the rock cycle.

Make sure that you include all of the following terms…

Types of Rocks: Igneous, Sedimentary, MetamorphicIngredients: Magma, SedimentsProcesses: 1. Weathering & erosion 2. heat & pressure3. melting 4. cooling 5. compaction & cementation

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Weathering the breaking down of rocks at

Earth’s surface

Erosion – the transportation of weathered

material by wind, water, ice, or other agent.

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Rocks • Naturally occurring solid material

made of one or more minerals• Grouped into 3 main types, based

on the way it was formed• Types of Rocks Brain Pop

Igneous Sedimentary Metamorphic

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IGNEOUS ROCKS

•Formed from magma that cools and hardens

•“Fire Formed”

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Fact:

•75% of Earth’s surface is

sedimentary rock!

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How Sedimentary Rocks are made:

1. Weathering:Existing rocks are broken down by chemical or physical means to create sediments.

2. Erosion: sediments are removed by wind, water, ice, or gravity.

3. Deposition: erosion energy becomes too weak to carry the sediments and they are “dropped”.

4. Compaction: Pressure placed in sediment layers cause them to change to rocks.

5. Cementation: sediments are joined together (cemented) by minerals dissolved in water.

6. Strata :Layers of sediments go through the process and a rock forms over time.

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Metamorphic Rocks

Metamorphism:• Changing of one type of rock in to

another due to - 1. Tremendous heat2. Great pressure3. Chemical reactions ( a change in

composition of minerals)

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IGNEOUS ROCKS: 2 types

• Intrusive rocks:– formed deep within Earth

–Magma “intrudes” into existing rock

• Extrusive rocks:– formed from lava at Earth’s surface

–Lava cools quickly in air

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IGNEOUS ROCKS: texture1. Fine grained

2. Coarse grained

3. Glassy4. Porphyritic

Cools fast, small crystals

Cools slow, large crystals

Lava cools rapidly at surface

Minerals cool at different rates

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IGNEOUS ROCKS: porphyry(POR-fuh-ree)

• Igneous rock with a mixture of large and small crystals

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•Granitic: –Light-colored

–Rich in silica

–Less dense

•Basaltic:–Dark-colored

–Rich in iron–More dense

Igneous Rocks: Compostion

* Major rocks of the crust

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Scoria

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Igneous Intrusion

Granitic or Basaltic?

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Oldest layers on the bottom

Youngest layers on the top

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Sedimentary rocks usually form in water

•Ripple marks and mud cracks

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Sedimentary Rocks: Classified by

• Composition• Texture• Grain size

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Types:1.Clastic2.Organic3.Chemical

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1. Clastic Rocks

•Formed by broken pieces or fragments of rock

•Classified according to size and shape of fragments

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Clastic RocksConglomerates:• Made of rounded pebbles and

other rocks of different sizes and cemented together by clay, mud ,or sand

• Formed when rivers deposit large pieces of rock

• Pieces of rock rounded by water before deposited

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Conglomerate:

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Clastic Rocks

Breccia:•Similar to conglomerates, but fragments are sharp and angular

•Not carried far enough by water to round the edges

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Breccia:

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Clastic Rocks

Sandstone:•Made of small, sand-sized grains•Very common•Resistant to wear and decay•Used to make buildings

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Sandstone:

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Clastic Rocks

Mudrock: •Formed from small particles of clay•Example: shale

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shale

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shale

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2. Organic Rock

•Formed directly or indirectly from material that used to be living

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Fossils often preserved in sedimentary rocks

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Organic Rock

Fossilized Limestone:•Shells from dead animals (containing calcium carbonate) that sink to bottom of ocean floor

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Limestone:

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Organic Rock

Chalk:•Composed of animals and calcium carbonate that have been pressed together

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Chalk

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Organic Rock

Coal:•Rock formed from plants that lived millions of years ago

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3. Chemical Rock

•Formed by chemical means that do not involve any living organisms

•Can occur through evaporation or chemical action

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Chemical Rock

Limestone: •Formed directly from ocean water instead of organisms

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Chemical Limestone:

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Chemical Rock

Rock salt:•Natural form of common table salt •Ex: Halite

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Chemical Rock

Rock gypsum:

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Contact Metamorphism• Occurs when rocks are heated by contact

with magma or lava• Covers a small area

Types of Metamorphism:

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Types of Metamorphism:

2. Regional Metamorphism:• Occurs when rocks are buried

deep beneath Earth’s surface and changed by increase in temperature and pressure

• Covers a large area

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Metamorphic Rock: Classification

1. Foliated Texture:Mineral crystals arranged in parallel layers or bands (flatten under pressure)

Slate Shale

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Foliated Texture:

Gneiss

Granite

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Foliated Texture:

phyllite:

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Foliated Texture:

gneiss:

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Metamorphic Rock: Classification

2. Unfoliated Texture:• No bands of crystals • Don’t break in layers• Most contain only one mineral

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Unfoliated Texture:

Marble

Limestone

Calcite crystals

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quartzite

Unfoliated Texture:

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COOKIES ROCK!! LAB1. Vanilla

Wafer

2. Chocolate Chip

3. Fudge Stripe

4. Sugar Wafer

• Igneous• Sedimentary• Metamorphic

For Each Cookie:

1)Name of Cookie

2)Characteristics

3)Rock Type

4)Why did you choose this?