Lab 2 Flashcards

(41 cards)

1
Q

What are minerals

A

Minerals are the basic building blocks of rocks, they are defined as a chemical element or compound that is a naturally occurring crystalline solid and is formed as a result of inorganic processes.

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2
Q

What are the 3 defining characteristics of minerals

A
  1. a mineral is homogeneous throughout
  2. A mineral has an ordered three-dimensional crystalline lattice. This gives the mineral its properties
  3. A mineral has a limited and definite chemical composition.
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3
Q

How do rocks differ from minerals

A

Rocks can be composed of a mixture of different minerals, pieces of organic material and fragments of other rocks. They do not have a crystalline nature, though the minerals within them do. And they can have a wide range of compositions based on component minerals.

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4
Q

how many minerals are there

A

There are over 3000 minerals discovered, but less than 30 make up the bulk of earth’s crust. These are called the rock-forming minerals

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5
Q

How are minerals classified

A

Minerals are classified based on the anion in their crystalline structures.
Groups of chemically related minerals are called classes. Many characteristics of minerals within a class have similar physical properties

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6
Q

What are the most common types of minerals

A

Silicates make up ~1/3 of all mineral types. They make up around 95% of earth’s crust.

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7
Q

What are Native element minerals

A

Minerals with no anions consisting of one element only. Ex: Sulphur, Graphite, Diamond, Gold

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8
Q

What are Sulphides

A

Minerals with Sulphur as the anion, ex: Pyrite, galena, Sphalerite, Pyrrhotite.

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9
Q

What are Oxides/hydroxides

A

Minerals with the anion of oxygen or hydroxyl.
ex: hematite, corundum, magnetite, bauxite

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10
Q

What are Halides

A

minerals with an Anion of fluorine or chlorine. Ex: Fluorite, halite, sylvite

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11
Q

What are Carbonates

A

Minerals with carbonate (CO3 2-) as the anion.
Ex: dolomite, calcite, siderite

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12
Q

What are Sulphates

A

minerals with sulphate (SO4 2-) as the anion. Ex: Gypsum, anhydrite, barite

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13
Q

What are Phosphates

A

Minerals with phosphate (PO4 3-) as the anion. Ex: apatite

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14
Q

What are Silicates

A

Minerals with the anion being Silicon-oxygen tetrahedral (SiO4 4-) in different linkages.
Ex (Phyllosilicate): mica, talc, chlorite, clay minerals
Ex (others): quartz, olivine, pyroxene, amphibole, feldspars.

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15
Q

what are a mineral’s diagnostic properties

A

the few characteristic physical properties that are most distinct and useful for accurate identification.

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16
Q

What are the most important properties

A

basic lustre, hardness, and cleavage. And some that are only applied to certain minerals such as streak, magnetism, acid reaction, detailed nonmetallic lustre, fracture and colour.

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17
Q

what are the steps for identifying minerals

A
  1. Determine the minerals basic lustre (metallic vs non metallic)
  2. Determine the minerals hardness range
  3. Look for cleavage planes and determine how many there are and the angle at which they intersect
  4. Make observations of other properties that may be of use:
    - Streak is useful with metallic minerals but rarely with non metallic
    - Colour is the easiest thing to observe, but most minerals occur in a variety of colour so its not always useful
    - The detailed lustre of nonmetallic minerals can sometimes be distinctive
    - only a couple metallic minerals are magnetic and a couple nonmetallic minerals react to acid
    - Exact specific gravity is not quick to determine, however it is worth noting if the mineral seems unusually heavy or light for its size.
  5. Finally use these observations to navigate the mineral identification tables which will allow to reach a final identification
18
Q

What is Lustre

A

the amount and quality of light reflected from the mineral surface. Basic lustre can be initially indentified as metallic or nonmetallic

19
Q

What is metallic lustre

A

a mineral that reflects light in a way similar to metal. can vary in reflectivity from bright and shiny like aluminium foil to dull like old coins.

20
Q

What is non-metallic lustre

A

Minerals that do not resemble metal and are further subdivided into different light reflective categories such as glassy, pearly, earthy, and waxy.

21
Q

What is hardness

A

a measure of the resistance of the specimen to abrasion or scratching and is determined by both mineral composition and its atomic structure

22
Q

how do you test hardness

A

by measuring its scratchability with reference to minerals of known hardness. These test minerals are arranged in a standard hardness scale known as Moh’s scale of hardness.

23
Q

what is Moh’s scale of hardness

A

a list of minerals from 1-10 in order of increasing hardness. Each mineral scratches minerals below but not above it.

24
Q

What are the 10 minerals on Moh’s hardness scale

A
  1. Talc
  2. Gypsum
    2.5 finger nail
  3. Calcite
    3.5 copper penny
  4. Fluorite
  5. Apatite
    5.5 Glass plate and metal scratcher/knife
  6. Feldspar
    6.5 streak plate
  7. Quartz
  8. Topaz
  9. Corundum
  10. Diamonds
25
How do you test hardness
1. Find the cleanest part of the specific and find a smooth surface on which to test. Press a sharp corner of the testing material against the specifimen and attempt to make a small scratch 2. check to see if you've made a scratch by cleaning the sample of any powder. Use hand lense 3. reverse the procedure and test the test material. If they scratch each other they have similar hardness
26
How should you test with glass or a scratch plate
hold it flat on the table, and draw the specimen firmly across it
27
What should you do when testing hardness with a mineral of small granular crystals (aggregates)
Aggregate will break apart easily. Use hand lens to determine just what scratching has done
28
Is hardness always the same for the same minerals
no, ex Hematite ranges from 1-6 depending on how well crystallized it is
29
How should you test hardness on a mineral with obvious cleavage
Perform the hardness on all cleavage planes, sometime one is harder than others
30
what is cleavage
the tendency of the mineral to break along well-defined planes which represent planes of weakness in the lattice.
31
What is the outer crystal face
represents the planes of growth of the minerals. Which is not always the same as cleavage. Quartz has a flat outer surface, but no cleavage planes
32
what is fracture
how a mineral breaks along non-cleavage plane. Most have an uneven fracture. However a few has more distinct fracture such as conchoidal where it is smooth and curved (mostly for glassy minerals)
33
What are some cleavage characteristic of common minerals
Quartz, garnet, and olivine have no cleavage Graphite, muscovite, biotite, and talc has one plane Pyroxene and feldspars have two at 90º Hornblende has two not at 90º Galene and halite have three at 90º Calcite and dolomite has three not at 90º (rhombic cleavage) fluorite has four planes Sphalerite has more than four (12)
34
35
what are some hints for determining cleavage
1. Look for flat shiny surfaces on mineral specific, not number of directions of those surfaces 2. Determine the approximate angle between cleavage planes 3. If you're having difficulty, check mineral tables to see what type of cleavage your mineral should have.
36
what is colour
Colour of a mineral results from absorption of certain wavelengths of light by the mineral. Many minerals occur in multiple colours, so colour isn't the most useful. Many minerals also display the same colour. Metallic minerals and native elements often has distinguishable colour.
37
How can reaction with acid help with mineral ID
Carbonate minerals can be distinguished from other minerals by the fact they react with acids. Note: go easy on acid, a small drop will do
38
How does magnetism help ID minerals
a few metallic minerals (magnetite and pyrrhotite) are strongly attracted by magnet
39
What is Odor
Kaolinite a clay mineral is the constituent of earth or soils which gives the earthy smell when moistened. Sphalerite gives a rotten egg smell when dilute HCl is on it
40
What is feel
some minerals have a greasy or soapy feel either due to basal cleavage (graphite, talc) or to dissolution of minerals by moisture on hand (halite)
41
What is streak
streak refers to colour of the mineral when a portion of it is crushed along a porcelain streak plate. Most minerals leave the same streak regardless of their colour. Non metallic minerals give a white or very pale streak.