Mineral physical properties

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Last updated 12:51 AM on 9/8/26
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74 Terms

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Color:

Caused by the complex ways in which light interacts with the mineral’s composition and internal structure (almost never diagnostic)

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Habit:

Refers to the shape in which a mineral often grows

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luster

Refers to how light bounces off a FRESH mineral surface (how shiny it is)

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Diaphaneity

How transparent or opaque a mineral is

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Density

technically specific gravity, but for us just eyeballed how heavy it is vs how heavy it looks like it should be

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Hardness

how easily a mineral’s surface is scratched

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Tenacity

The mineral’s resistance to breaking.

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Streak

the color of the trail of ground-up mineral bits if you scratch a mineral against a porcelain plate

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Luminescence

A minerals “glow” caused from electrons jumping to a higher energy state when you shine a light on it

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Flouresecne

A form of luminescence where the light you shine on it is UV.

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Phosphoresence

A form of luminescence where the electron gets trapped in a higher energy state for a while, so the glow sticks around even after you take away the light source.

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opalescence

minerals glinting different colors as the mineral is rotated

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magnetism

minerals being magnetic

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Effervescence

minerals fizzing when you drop HCL on them

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taste

sometimes minerals have a certain taste!

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Mohs hardness of talc

1

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Mohs hardness of gypsum

2

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Mohs hardness of calcite

3

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Mohs hardness of fluorite

4

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Mohs hardness of Apetite

5

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Mohs hardness of orthoclase feldspar

6

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Mohs hardness of quartz

7

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Mohs hardness of topaz

8

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Mohs hardness of corundum

9

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Mohs hardness of diamond

10

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Mohs hardness of pencil lead

1.5

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Mohs hardness of fingernail

2.5

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Mohs hardness of penny

3.5

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Mohs hardness of pocket knife blade

5.5

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glass

5.5

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steel file

6.5

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streak plate

7

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Metallic luster:

Like polished metal

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Sub-metallic luster:

looks like metal but not as shiny

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Non-metalic luster:

Not shiny like metal

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Vitreous luster:

like glass

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Resinous luster:

looks like resin or glass (mostly amber colored minerals)

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Greasy luster:

looks like it has grease on it

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waxy luster:

looks like its surface is made of wax paper

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silky luster:

like fine fibers

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Adamantine luster

brilliantly shiny, like a diamond

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Pearly luster

almost iridescent, like the inside of a seashell

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Dull luster

Not at all shiny

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Earthy luster

like dirt (leaves stuff on your hands!)

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Blocky habit

Having square-ish cross-sections

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Acicular habbit

Needle-like

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Tabular habbit

Like thick sheets stacked together

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Bladed

looks like a blade

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Columnar/prismatic

Elongated in one direction

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Micaceous

Easily split into sheets

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Massive

Solid mass of crystals, without real form

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dendritic

branching like a tree

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Botryoidal

like a bunch of grapes

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Drusy

Covered in fine crystals

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4 main variables that contribute top a minerals color:

composition, impurities, structure, habit

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Hematite color vs streak

usually black but red streak

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Galena appearance (lookalike mineral) vs streak

looks like hematite but has a grey streak

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Fluorite color vs streak

Usually blue or purple but has a white streak

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Most silicate minerals have a what streak color?

white

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3 types of fracture:

Uneven, chonchoidal, fiberous/spiny

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4 concepts to describe cleavage:

Quality, direction, angle, habit

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Basal cleavage habit:

1-direction, parallel to the mineral base.  Minerals look like they’re being peeled away, like biotite or muscovite

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Cubic cleavage habit:

Mineral ends up looking like a cube, like galena. 

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Octahedral cleavage habit:

Mineral ends up looking like two pyramids.  Pyramid-shaped wedges break off.  For example: fluorite.

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Rhombohedral cleavage habit:

Mineral ends up looking like a rhombohedron (a tilted cube), e.g., calcite.

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Indicators of a surface being a growth surface NOT a cleavage one:

Impurities (tiny pits or grooves in the surface), growth grooves / chatter marks, freshness of mineral surface (not fresh= might be a growth face)

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Striations are:

extremely thin, long, parallel grooves cut into the surface of a mineral (often caused by twinning)

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minerals in the Amphibole Group (Hornblende, Tremolite, Actinolite, Glaucophane, etc.) – all have what cleavage?

60˚/120˚

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Minerals in the Pyroxene Group (enstatite, diopside, augite, etc.) – all have what cleavage?

approx. 90˚

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Plagioclase will usually have what?

striations

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Calcite and dolomite have what cleavage?

Rhombohedral

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Quartz has what kind of fracture?

Conchoidal

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Mica minerals have what kind of cleavage?

1-directional, perfect basal

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The chrysotile form of serpentine by its has what kind of fracture?

Extremely fibrous