Geol 101 - Mineral Identification

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23 Terms

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What is a mineral?

a naturally occurring inorganic substance that is solid at room temperature and has a distinct chemical composition + well-defined crystalline structure.

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How many common rock-forming minerals are there?

Less than 30. (95% of Earth’s Crust)

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Crystalline Structure

Arrangement of atoms that is repeated to form a mineral grain.

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Crystal Habit

Crystals that grow slowly in open space to develop a characteristic form.

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How many mineral groups are there?

8

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How are the mineral groups sorted by?

Chemical Composition

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Ferromagnesian Silicates

Iron/Magnesium that is dark colored; dense.

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Non-ferromagnesian Silicates

Calcium/Aluminum/Potassium that is light colored; light weight

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What are diagnostic physical properties?

Hardness, luster, streak, specific gravity, cleavage/fracture, tenacity and special properties.

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Hardness

ability of a solid substance to resist permanent deformation when subjected to a compressive force.

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Diaphaneity

Passage of light through a mineral.

  1. Transparent

  2. Translucent

  3. Opaque

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Color

Useful when looking at distinctive coloration that can be used for identification.

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Streak

a small sample is dragged across a sample of an unglazed ceramic plate, leaving a streak of powdered material. The streak reveals the actual color of a mineral.

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Tenacity

Toughness; how the mineral behaves in response to bending.

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Cleavage

How a mineral breaks along one or more weak planes within the crystalline structure.

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Fracture

Minerals breaking roughly; no flat surfaces.

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Crystal Shape/Habit

geometric form that displays how a crystal grew under unobstructed conditions.

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Luster

the way that light reflects, or doesn’t, from the surface of a material.

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How to identify an unknown mineral sample?

  1. Look at the mineral ID chart for luster

  2. Examine fractures/cleavage

  3. Estimate hardness

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<p>How many cleavages does this mineral have?</p>

How many cleavages does this mineral have?

One; Samples are split into thin sheets along that one plane.

<p>One; Samples are split into thin sheets along that <strong>one </strong>plane.</p>
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<p>How many cleavages does this mineral have? </p>

How many cleavages does this mineral have?

Two; Samples are split into thin sheets along two planes.

<p>Two; Samples are split into thin sheets along <strong>two</strong> planes. </p>
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<p>How many cleavages does this mineral have? </p>

How many cleavages does this mineral have?

Three; Right angles right to each other, breaks into cubes.

<p>Three; <strong>Right </strong>angles right to each other, breaks into cubes. </p>
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<p>How many cleavages does this mineral have?</p>

How many cleavages does this mineral have?

Three; Not right angles, breaks into rhombohedrons.

<p>Three; <strong>Not right</strong><em> </em>angles, breaks into rhombohedrons. </p>