1/73
reading 1
Name | Mastery | Learn | Test | Matching | Spaced | Call with Kai | Chat |
|---|
No analytics yet
Send a link to your students to track their progress
Color:
Caused by the complex ways in which light interacts with the mineral’s composition and internal structure (almost never diagnostic)
Habit:
Refers to the shape in which a mineral often grows
luster
Refers to how light bounces off a FRESH mineral surface (how shiny it is)
Diaphaneity
How transparent or opaque a mineral is
Density
technically specific gravity, but for us just eyeballed how heavy it is vs how heavy it looks like it should be
Hardness
how easily a mineral’s surface is scratched
Tenacity
The mineral’s resistance to breaking.
Streak
the color of the trail of ground-up mineral bits if you scratch a mineral against a porcelain plate
Luminescence
A minerals “glow” caused from electrons jumping to a higher energy state when you shine a light on it
Flouresecne
A form of luminescence where the light you shine on it is UV.
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.
opalescence
minerals glinting different colors as the mineral is rotated
magnetism
minerals being magnetic
Effervescence
minerals fizzing when you drop HCL on them
taste
sometimes minerals have a certain taste!
Mohs hardness of talc
1
Mohs hardness of gypsum
2
Mohs hardness of calcite
3
Mohs hardness of fluorite
4
Mohs hardness of Apetite
5
Mohs hardness of orthoclase feldspar
6
Mohs hardness of quartz
7
Mohs hardness of topaz
8
Mohs hardness of corundum
9
Mohs hardness of diamond
10
Mohs hardness of pencil lead
1.5
Mohs hardness of fingernail
2.5
Mohs hardness of penny
3.5
Mohs hardness of pocket knife blade
5.5
glass
5.5
steel file
6.5
streak plate
7
Metallic luster:
Like polished metal
Sub-metallic luster:
looks like metal but not as shiny
Non-metalic luster:
Not shiny like metal
Vitreous luster:
like glass
Resinous luster:
looks like resin or glass (mostly amber colored minerals)
Greasy luster:
looks like it has grease on it
waxy luster:
looks like its surface is made of wax paper
silky luster:
like fine fibers
Adamantine luster
brilliantly shiny, like a diamond
Pearly luster
almost iridescent, like the inside of a seashell
Dull luster
Not at all shiny
Earthy luster
like dirt (leaves stuff on your hands!)
Blocky habit
Having square-ish cross-sections
Acicular habbit
Needle-like
Tabular habbit
Like thick sheets stacked together
Bladed
looks like a blade
Columnar/prismatic
Elongated in one direction
Micaceous
Easily split into sheets
Massive
Solid mass of crystals, without real form
dendritic
branching like a tree
Botryoidal
like a bunch of grapes
Drusy
Covered in fine crystals
4 main variables that contribute top a minerals color:
composition, impurities, structure, habit
Hematite color vs streak
usually black but red streak
Galena appearance (lookalike mineral) vs streak
looks like hematite but has a grey streak
Fluorite color vs streak
Usually blue or purple but has a white streak
Most silicate minerals have a what streak color?
white
3 types of fracture:
Uneven, chonchoidal, fiberous/spiny
4 concepts to describe cleavage:
Quality, direction, angle, habit
Basal cleavage habit:
1-direction, parallel to the mineral base. Minerals look like they’re being peeled away, like biotite or muscovite
Cubic cleavage habit:
Mineral ends up looking like a cube, like galena.
Octahedral cleavage habit:
Mineral ends up looking like two pyramids. Pyramid-shaped wedges break off. For example: fluorite.
Rhombohedral cleavage habit:
Mineral ends up looking like a rhombohedron (a tilted cube), e.g., calcite.
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)
Striations are:
extremely thin, long, parallel grooves cut into the surface of a mineral (often caused by twinning)
minerals in the Amphibole Group (Hornblende, Tremolite, Actinolite, Glaucophane, etc.) – all have what cleavage?
60˚/120˚
Minerals in the Pyroxene Group (enstatite, diopside, augite, etc.) – all have what cleavage?
approx. 90˚
Plagioclase will usually have what?
striations
Calcite and dolomite have what cleavage?
Rhombohedral
Quartz has what kind of fracture?
Conchoidal
Mica minerals have what kind of cleavage?
1-directional, perfect basal
The chrysotile form of serpentine by its has what kind of fracture?
Extremely fibrous