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What is a mineral

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3- Solid w/ specific composition- Most often a combination of elements ... Examples: Quartz, feldspar, olivine, topaz, Mica. Carbonates and Oxides. Carbonates: ... – PowerPoint PPT presentation

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Title: What is a mineral


1
What is a mineral
  • Four requirements to be a mineral
  • 1- Naturally occurring
  • 2- Inorganic solid
  • 3- Specific chemical composition
  • 4- Definite crystalline structure
  • __________________________________
  • Each mineral has unique characteristics,
  • About 3000 minerals on Earth, but only about 10
    make 90 of the rocks in Earths crust (0.003
    of total of minerals)

2
Mineral characteristics
  • 1- Naturally occurring- No synthetic or
    manufactured material fits this condition
  • 2- Inorganic solid- No material (even naturally
    occurring) that is made by biotic means.
  • 3- Solid w/ specific composition- Most often a
    combination of elements (compounds), but a few
    are single elements. Minerals may have the same
    elements, but their proportion and arrangement
    are unique.
  • 4- Definite crystalline structure- A repeated
    pattern of crystal arrangement (one of 6 crystal
    systems)

3
What is not a mineral -Mineraloids and Rocks
  • Mineraloids - Some materials, even naturally
    occurring fit the conditions, except for the
    orderly internal (crystalline) structure (Ex.
    Opal)
  • Rocks Any solid mass of mineral, or
    mineral-like matter that occurs naturally as part
    of our planet. Some types
  • - Composed almost entirely of one mineral (ex.
    Limestone)
  • - Aggregates of several minerals (most rocks,
    ex. Granite, which is a combination of quartz,
    feldspar, hornblende)
  • - Composed of non-mineral matter
  • non-crystalline, glassy volcanic rocks
    (obsidian, pumice) solid organic debris (coal)

4
Crystals and Crystal Systems
  • Definition of Crystal - Regular polyhedral form,
    bounded by smooth faces, assumed by a chemical
    compound, due to the action of its inter-atomic
    forces, when passing, under suitable conditions,
    from liquid or gas to a solid.
  • 1- Polyhedral solid bounded by flat planes
    (Crystal Faces)
  • 2- Change from liquid or gas to solid Liquids
    and gases dont have definite shape (take shape
    of container), solids take on one of several
    regular geometric forms. These forms may be
    subdivided, using geometry, into six systems
  • 1- Cubic
  • 2- Tetragonal
  • 3- Hexagonal
  • 4- Orthorhombic
  • 5- Monoclinic
  • 6- Triclinic

5
Basis for Crystal Systems
  • Some geometry
  • CRYSTALLOGRAPHIC AXES.
  • - We have 3 dimensions, so we must have 3 axes.
  • - For a moment, let's make them all equal and at
    right angles to each other. This is the simplest
    case. The axes pass through the center of the
    crystal and, by using them, we can describe the
    intersection of any given face with these 3 axes.

6
Basis for Crystal Systems
  • Axes
  • Number Length angles
  • ____________________________
  • 1- Cubic 3 equal 90
  • 2- Tetragonal 3 2 equal 90
  • 3- Hexagonal 4 3 equal variable
  • 4- Orthorhombic 3 all diff. 90
  • 5- Monoclinic 3 all diff. variable
  • 6- Triclinic 3 unequal all different

7
But not all crystals are ideal !!(Most are not.)
  • Your mineral crystal that does not match the
    pictures books.
  • You may have is a distorted crystal form where
    some faces may be subordinate or missing.
    Distorted crystals are common and result from
    less-than-ideal growth conditions or even
    breakage and recrystallization of the mineral.
    However, remember that we must also be comparing
    the angles between similar faces. If the faces
    are not present, then you cannot compare them.
    With many crystals we are dealing with a final
    shape determined by forces other than those of
    the interatomic bonding.
  • During the process of crystallization in the
    proper environment, crystals assume various
    geometric shapes dependent on the ordering of
    their atomic structure and the physical and
    chemical conditions under which they grow. If
    there is a predominant direction or plane in
    which the mineral forms, different habits
    prevail. Thus, galena often forms equate shapes
    (cubes or octahedrons), quartz typically is
    prismatic, and barite tabular.

8
Mineral and Crystal formation
  • From Magma (molten matter from beneath Earths
    surface)
  • - Elements and proportion in magna Type of
    minerals formed
  • - Rate of cooling Size of crystals formed
    (slow-large crystals, fast-small)
  • From solutions.
  • - By precipitation In saturated solutions,
    mineral crystals precipitate.
  • - By evaporation Only water leaves, minerals
    stay behind

9
Common Mineral and Elements
  • Of the 4000 minerals on Earth, about 30 are
    common Rock forming minerals.
  • About 90 elements occur naturally on Earths
    crust. The great majority of minerals are made of
    8 common elements
  • Oxygen Aluminum Calcium Potassium
  • Silicon Iron Sodium Magnesium
  • All other elements combined make 1.7
  • Oxygen (46.6) and Silicon (27.7) are the most
    common.
  • In contrast, 6 elements are most common within
    living organisms (Carbon, Oxygen, Nitrogen,
    Hydrogen, Phosphorous and Sulfur).

10
Mineral Groups
  • 1- Silicates
  • 2- Carbonates
  • 3- Oxides and hydroxides
  • 4- Halides
  • 5- Sulfates
  • 6- Sulfides
  • 7- Native elements

11
SILICATES
  • - 96 of minerals in Earths crust
  • - Contain O, Si and 1 or more elements.
  • - Form Silica tetrahedron molecules, each made
    of 1 Si atom attached to 4 Oxygen atoms. This
    arrangement allows sharing Oxygen atoms among
    tetrahedron molecules and determines the great
    variety of silicates.
  • - Various arrangements of tetrahedron molecules
    are common Single chain, double, Sheet.
  • - The bonds between the other atoms in the
    silicate determine properties, particularly how
    they split.
  • - Examples Quartz, feldspar, olivine, topaz,
    Mica

12
Carbonates and Oxides
  • Carbonates
  • - One or more metallic elements, with a
    carbonate group (CO3).
  • - Examples Limestone (used commercially for
    road paving, building stone and cement), Marble
    (used decoratively)
  • Oxides
  • - Oxygen and a metal.
  • - Examples Hematite and Magnetite (Ore of Iron
    source of iron), Uraninite (source of uranium)

13
Sulfides, Sulfates, Halides Native Elements
  • Sulfides
  • - Sulfur and one more element (pyrite FeS2)
  • Sulfates
  • - Include the sulfate compound SO4 (anhydrate
    Ca SO4)
  • Halides
  • - Chloride or Fluoride, along with Ca, Na or K
    (Salt NaCl)
  • Native elements
  • - Silver (Ag), Copper (Cu) occur naturally alone.
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