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WELCOME TO THE GLENDALE COMMUNITY
COLLEGE
presented by:
Susan Celestian - Curator of the Arizona Mining and Mineral Museum
Stan Celestian - Photographer
MINERAL IDENTIFICATIONPROGRAM
© copyright 2002
Crystals………………………………….…4 Isometric……………………………….…..6Hexagonal……………………………….…10Tetragonal………………………………….14Orthorhombic…………………………..….18Monoclinic………………………………...23Triclinic……………………………………26Resources………………………………….29
TABLE OF CONTENTS
This is the second part of Mineral Identification Program
Introduction to Mineral Identification Basics
Welcome to the fascinating world Welcome to the fascinating world of Minerals. The purpose of this of Minerals. The purpose of this
CD is to present you with some of CD is to present you with some of the basic techniques used to the basic techniques used to
identify minerals.identify minerals. This Power Point Presentation can also be viewed in the “edit” mode. Here you can view the many notes associated with the slides.
Mineral Identification Basics PHYSICAL PROPERTIES CRYSTALS
A CRYSTAL is the outward form of the internal structure of the mineral.
The 6 basic crystal systems are:
ISOMETRICHEXAGONAL
TETRAGONALORTHORHOMBIC
MONOCLINICTRICLINICDrusy Quartz on Barite
Mineral Identification Basics PHYSICAL PROPERTIES CRYSTALS
CRYSTAL SYSTEMS are divided into 6 main groups.
ISOMETRIC - Fluorite Crystals
The first group is the ISOMETRIC. This literally means “equal measure” and refers to the equal size of the crystal axes.
Mineral Identification Basics ISOMETRIC CRYSTALS
ISOMETRICIn this crystal system there are 3 axes. Each has the same length (as indicated by the same letter “a”).
They all meet at mutual 90o angles in the center of the crystal.
Crystals in this system are typically blocky or ball-like.ISOMETRIC
Basic Cube
a3
a2
a1
Mineral Identification Basics ISOMETRIC CRYSTALS
ISOMETRIC Crystal Model
Within this ISOMETRIC crystal model is the OCTAHEDRAL crystal form (yellow) and the TETRAHEDRAL crystal form (shown by the black lines).
Mineral Identification Basics ISOMETRIC CRYSTALS
ISOMETRIC - Basic Cube
a1
a3
a2
a3
a2
a1
Fluorite cube with crystal axes.
Mineral Identification Basics ISOMETRIC BASIC CRYSTAL SHAPES
Octahedron
Spinel
Cube
Fluorite Pyrite
Cube with Pyritohedron
Striations
TrapezohedronGarnetGarnet Garnet - Dodecahedron
Mineral Identification Basics HEXAGONAL CRYSTALS
HEXAGONAL - Three horizontal axes meeting at angles of 120o and one perpendicular axis.
a1
a2
a3
HEXAGONAL Crystal Axes
c
Mineral Identification Basics HEXAGONAL CRYSTALS
HEXAGONAL Crystal Model
HEXAGONAL
This model represents a hexagonal PRISM (the outside hexagon - six sided shape). The top and bottom faces are called PINACOIDS and are perpendicular to the vertical “c” axis.
Within this model is the SCALENOHEDRAL form. Each face is a scalenohedron. Calcite often crystallizes with this form.
Mineral Identification Basics HEXAGONAL CRYSTALS
These hexagonal CALCITE crystals nicely show the six sided prisms as well as the basal pinacoid.
Mineral Identification Basics HEXAGONAL CRYSTALS
RHOMBOHEDRON
Dolomite
SCALENOHEDRON
Rhodochrosite
QuartzHanksite
Pyramid Pyramid FaceFace
Prism Prism FacesFaces
Prism Prism FacesFaces
Pyramid Pyramid FacesFaces
Vanadinite
Mineral Identification Basics TETRAGONAL CRYSTALS
TETRAGONAL
Two equal, horizontal, mutually perpendicular axes (a1, a2)
Vertical axis (c) is perpendicular to the horizontal axes and is of a different length.
TETRAGONAL Crystal Axes
a1a2
c
c
a2a1
This is an Alternative Crystal Axes
Mineral Identification Basics TETRAGONAL CRYSTALS
TETRAGONAL Crystal Model
TETRAGONAL
This model shows a tetragonal PRISM enclosing a DIPYRAMID.
Mineral Identification Basics TETRAGONAL CRYSTALS
WULFENITE
Same crystal seen edge on.Same crystal seen edge on.
Mineral Identification Basics TETRAGONAL CRYSTALS
APOPHYLLITE on Stilbite
This is the same Apophyllite crystal looking down the “c” axis.
The red square shows the position of the pinacoid (perpendicular to the “c” axis).
Mineral Identification Basics ORTHORHOMBIC CRYSTALS
ORTHORHOMBIC
Three mutually perpendicular axes of different lengths.
ORTHORHMOBIC Crystal Axes
ab
c
a
c
b
An Alternative Crystal Axes Orientation
Mineral Identification Basics ORTHORHOMBIC CRYSTALS
ORTHORHMOBIC Crystal Model
ORTHORHOMBIC
This model shows the alternative axes where the vertical “c” axis is not the longest axis.
The model shows the outside “brick” shape of the PRISM and the inner shape is a DIPYRAMID. The top and bottom faces are called PINACOIDS and are perpendicular to the “c” axis.
Mineral Identification Basics ORTHORHOMBIC CRYSTALS
Topaz from Topaz Mountain, Utah.
Mineral Identification Basics ORTHORHOMBIC CRYSTALS
BARITE is also orthorhombic. The view above is looking down the “c” axis of the crystal.
Mineral Identification Basics ORTHORHOMBIC CRYSTALS
STAUROLITE
Prism View
Pinacoid
View
Mineral Identification Basics ORTHORHOMBIC CRYSTALS
This is a Staurolite TWIN with garnets attached.
Mineral Identification Basics MONOCLINIC CRYSTALS
MONOCLINIC
In this crystal form the axes are of unequal length.
Axes a and b are perpendicular.
Axes b and c are perpendicular.
But a and c make some oblique angle and with each other.
MONOCLINIC Crystal Axes
a
b
c
Mineral Identification Basics MONOCLINIC CRYSTALS
MONOCLINIC Crystal Model
MONOCLINIC
In this model the outside shape is the PRISM. It looks like a distorted brick - flattened out of shape.
Inside is the DIPYRAMID.
Mineral Identification Basics MONOCLINIC CRYSTALS
Gypsum Mica
Orthoclase
Top View
Mineral Identification Basics TRICLINIC CRYSTALS
TRICLINIC
In this system, all of the axes are of different lengths and none are perpendicular to any of the others.
TRICLINIC Crystal Axes
a b
c
Mineral Identification Basics TRICLINIC CRYSTALS
TRICLINIC Crystal Model
TRICLINIC
Again in this model the outside shape is the PRISM.
Located within the prism is the DIPYRAMID.
Mineral Identification Basics TRICLINIC CRYSTALS
Microcline, variety Amazonite
Mineral IdentificationMineral Identification RESOURCESRESOURCES
http://www.gc.maricopa.edu/earthsci/imagearchive/index.htm
For lots of useful images of minerals and more facts about minerals, check out this web site:
This copyrighted Power Point CD was produced strictly for educational purposes. Any attempt at using the images within this program for monetary gain is illegal. The authors have given permission to use the program or parts of it, provided credit is given to the Arizona Mining and Mineral Museum, its Curator - Susan Celestian and the photographer - Stan Celestian.
THE
END