SECOND LESSON Flashcards

(40 cards)

1
Q

This are naturally occurring, inorganic, solid element or
compound crystalline substance, has definite atomic structure and chemical composition.

A

MINERALS

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2
Q

8 PHYSICAL PROPERTIES OF MINERALS

A

COLOR
LUSTER
FRACTURE
HARDNESS
STREAK
CLEAVAGE
TENACITY
SPECIFIC GRAVITY

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2
Q

HOW CAN A MINERAL BE CLASSIFIED?

A

Geologists in the field often lack access to advanced lab techniques. Instead, they rely on properties that can be seen with the naked eye or measured using simple tools.

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3
Q

is that seen on its surface by
the naked eye. It may depend on the impurities
present in light-coloured minerals, and one mineral
specimen may even show gradation of color or
different colors.

A

color

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3
Q

color is usually
a _________rather than specific guide to which
mineral is present.

A

general

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4
Q

LIST OF SOME COLORING ELEMENTS AND THE COLOR THEY PRODUCE IN AT LEAST ONE MINERAL:

A

COBALT: Produces the violet-red color in
erythrite, (Cobalt arsenic sulfide)
COPPER: Produces the azure blue color of
azurite, (copper carbonate hydroxide)

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5
Q

Two general types of luster are designated as follows:

A

 METALLIC(SHINY)
 NONMETALLIC (DULL)

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5
Q

Light is reflected from the surface of a mineral, the amount of light depending on physical qualities of the surface (such as its smoothness and transparency).

A
  1. LUSTER
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6
Q

looks fibrous. Ex. gypsum, serpentine, malachite.

A
  1. Silky
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6
Q

Non metallic lusters are referred to as :

A
  1. Vitreous
  2. Resinous
  3. Pearly
  4. Greasy
  5. Silky
  6. Adamantine
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6
Q

looks resinous - examples: sphalerite, sulfur.

A
  1. Resinous
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6
Q

looks glassy - examples: clear quartz,
tourmaline

A
  1. Vitreous
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7
Q

iridescent pearl-like - example: apophyllite

A
  1. Pearly
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8
Q

appears to be covered with a thin layer of oil - example: nepheline.

A
  1. Greasy
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9
Q

brilliant luster like diamond

A
  1. Adamantine
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10
Q

If the mineral contains no planes of weakness, it will break along random directions called

A
  1. FRACTURE
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11
Q

KINDS OF FRACTURE

A
  1. Conchoidal
  2. Uneven or Irregular
  3. Splintery
  4. Hackly
  5. Earthy
  6. Subconchoidal
11
Q

defined as the appearance of its broken surface.

12
Q

mohs scale

A

Diamond, 10;
Corundum, 9;
Topaz, 8;
Quartz, 7;
Orthoclase, 6;
Apatite, 5;
Fluorite, 4;
Calcite, 3;
Gypsum, 2;
and Talc, 1.

12
Q

a smoothly curved fracture that is familiar to people who have examined broken glass. Sometimes described as a clam-shell fracture. Quartz has this fracture type and almost all specimens that have been broken, demonstrate this fracture type
very well.

13
Q

jagged fractures with sharp edges

13
Q

rough irregular surfaces

A
  1. Uneven or Irregular
14
Q

fracture type that occurs in fibrous or finely acicular minerals and in minerals that have a relatively stronger structure in one direction than the other two. Chrysotile serpentine is a typical mineral with splintery fracture and kyanite is an example of a non-fibrous mineral that has this fracture.

15
Q

describes the reaction of a mineral to stress such as crushing, bending, breaking, or tearing. Certain minerals react differently to each type of stress.

15
Similar to conchoidal, just not as curved, but still smooth. E.g. Andalusite
6. Subconchoidal
16
a fracture that produces a texture similar to broken children's clay. It is found in minerals that are generally massive and loosely consolidated such as limonite.
5. Earthy
17
is the characteristic that describes how the particles of a mineral hold together or resist separation
4. TENACITY
18
DIFFERENT FORMS OF TENACITY
1. Brittle 2. Ductile 3. Elastic 4. Malleable: 5. Sectile:
18
breaks or powders easily; for example, pyrite or marcasite.
1. Brittle
19
can be drawn into a wire; for example, copper.
2. Ductile:
20
bends and resumes its original position or shape when pressure is released; for example, biotite or muscovite.
3. Elastic
20
can be hammered into thin plates or sheets; for example, gold or copper
4. Malleable:
21
can be cut or shaved with a knife; for example, gypsum or galena.
5. Sectile:
21
------------ of a mineral can be measured by its resistance to scratching or abrasion. Mohs scale is a set of 10 common minerals chosen for comparative hardness.
hardness (scratchability
21
A mineral that naturally breaks into perfectly flat surfaces is exhibiting -----
Cleavage
22
of a mineral is the color of the powder produced when the mineral is rubbed against an unglazed porcelain plate or other fine-grained, hard, abrasive surface. The color of a particular mineral may vary, but the streak is generally constant
6. STREAK
22
is the tendency of a mineral to break along certain planes to make smooth surface
Cleavage
23
A ______ represents a direction of weakness in the crystal lattice
Cleavage
24
_____ surfaces can be distinguished by how they consistently reflect light, as if polished, smooth, and even
Cleavage
24
of a mineral is its weight compared to the weight of an equal volume of water; thus, a mineral with a specific gravity of 4 is four times heavier than water.
The specific gravity (relative density)