THIRD LESSON Flashcards

(50 cards)

1
Q

QUARTZ FAMILY
- GERMAN “quarz” MEANING

A

UNCERTAIN ORIGIN

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2
Q

IS COMPOSED OF SILICON (Si) AND OXYGEN (O), THE TWO MOST ABUNDANT ELEMENTS IN THE CRUST OF THE EARTH.

A

QUARTZ OR SILICA

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2
Q

TRUE OR FALSE

WHEN QUARTZ IS PURE IN COMPOSITION, IT IS ENTIRELY DEVOID OF COLOR AND ALMOST WATER-CLEAN IN ITS LIMPIDITY.

A

TRUE

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2
Q

IT IS THIS KIND WHICH, WHEN FIRST TIME DISCOVERED IN ALPS, WAS BELIEVED TO BE A FORM OF FROZEN WATER AND THEREFORE CALLED ________

A

CRYSTAL

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2
Q

TWO CLASSIFICATIONS OF QUARTZ

A
  1. MACROCRYSTALLINE QUARTZ
  2. CRYPTOCRYSTALLINE QUARTZ
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2
Q

example of MACROCRYSTALLINE QUARTZ

A

 Rock crystal
 Milky quartz
 Brown quartz
 YELLOW QUARTZ
 AMETHYST
 ROSE QUARTZ

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3
Q

SIMPLY KNOWN AS QUARTZ

A
  1. MACROCRYSTALLINE QUARTZ
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3
Q

VARIETY THAT DEVELOP VISIBLE CRYSTALS OR ARE MADE OF LARGE INTERGROWN CRYSTALS (macro-large)
- EX: Rock, Crystal, Milky Quartz, Yellow Quartz, Amethyst

A
  1. MACROCRYSTALLINE QUARTZ
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3
Q

-_________ (krystallos in Greek meaning ice)
- Clear, transparent, colorless

A

Rock Crystal

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4
Q
  • The milkiness is due to myriad tiny cavities bubbles filled with CO2 or water
  • Vein quartz is often white and frequently contains gold
A

 Milky quartz

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4
Q

This variety called smoky quartz is pale beige, tan, brown, or deep brown in color

A

 Brown quartz

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4
Q

The name is from the old French citrin meaning yellow.
- Ranges in color from pale yellow through yellow-orange to rich golden orange, to very dark orange.

A

 YELLOW QUARTZ

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5
Q

_________ (in Greek atnethystos, meaning not drunken)
- Violet or purple quartz. The lightest color, a pale lilac shade, is known as Rose of France

A

Amethyst

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5
Q

The color of this variety is pink or (rarely) rose-red. This is due to presence of manganese.
- The material is nearly always cloudy or translucent, rarely transparent.

A

 ROSE QUARTZ

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6
Q
  • ALSO KNOWN AS MICROCRYSTALLINE QUARTZ.
A
  1. CRYPTOCRYSTALLINE QUARTZ
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7
Q

DENSE AND COMPACT VARIETIES (crypto-hidden)
- EX: Chalcedony, Onyx, Flint and Chert, Bloodstone, Agate, Jasper

A
  1. CRYPTOCRYSTALLINE QUARTZ
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7
Q

example of CRYPTOCRYSTALLINE QUARTZ

A

CHALCEDONY
ONYX
BLOODSTONE
FLINT AND CHERT
AGATE
JASPER

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7
Q

Unstained material often grayish blue, compact of silica.

A purple-colored ______ from Arizona has been marketed under the trade name damsonite.

A

chalcedony

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7
Q

Banded black and white chalcedony.

A

onyx

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8
Q

Banded onyx, with red and white layers.

A

Sardonyx:

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9
Q

Also known as heliotrope, consists of dark green plasma with blood-red and orange spots of iron oxides.

9
Q

Opaque, dull gray, or whitish chalcedony, very compact and hard.

A

FLINT AND CHERT

10
Q

Usually takes the form of colored layers or/ands, flat or concentric. Also, mossy or dendritic inclusions, sometimes creating the impression of landscapes, vegetation, and so forth.

11
Q

There are different agates such as banded agates, moss agates, scenic agates, lace agates, fire agates, shell agates, and turritella agate.

11
Usually, a mass of tiny silica crystals pigmented by impurities.
Jasper
11
The colors may be very stong, especially shades of brown, yellow, red, and green.______occurs worldwide.
Jasper
11
There are also different jaspers that are
orbicular and scenic
11
PHYSICAL PROPERTIES OF QUARTZ IN TERMS OF CRYSTAL SYSTEM, HABIT, CLEAVAGE, FRACTURE, COLOR
CRYSTAL SYSTEM: HEXAGONAL HABIT: CRYSTALLINE OR ARMOPHOUS CLEAVAGE: INDISTINCT FRACTURE: CONCHOIDAL COLOR: PURE - COLORLESS, COLORED - INDICATE IMPURITIES
11
PHYSICAL PROPERTIES OF QUARTZ IN TERMS OF LUSTER, HARDNESS, TENACITY, SPECIFIC GRAVITY, STREAK, TRANSPARENCY
LUSTER: VITREOUS HARDNESS: 7 TENACITY: BRITTLE SPECIFIC GRAVITY: 2.6 - 2.7 STREAK: WHITE TRANSPARENCY: TRANSPARENT/ SEMI-TRANSPARENT/ OPAQUE
11
PROCESS OF FORMATION OF QUARTZ
Forms when silica-rich magma cools and crystallizes. Develops in pegmatites during and after hot vapor-driven metamorphic processes. Grows in hot, water-rich environments (100°C to 450°C) under high pressure.
11
came from the word “feldspat” meaning a rock that does not contain a core
FELDSPAR
11
meaning a rock that does not contain a core
feldspat
11
is the name of a large group of rock-forming silicate minerals that make up over 50% of Earth's crust. They are found in igneous, metamorphic, and sedimentary rocks in all parts of the world
Feldspar
11
_______ minerals have very similar structures, chemical compositions, and physical properties
Feldspar
11
Common feldspars include
orthoclase(KAlSi3O8), albite (NaAlSi3O8), and anorthite (CaAl2Si2O8).
11
FELDSPAR CAN BE DIVIDED INTO TWO GROUPS:
- ALKALI FELDSPAR (k + Na) - PLAGIOCLASE FELDSPAR ( Na + Ca)
11
FAMOUS FELDSPAR FAMILY MEMBERS
1. MICROLINE 2. ORTHOCLASE 3. SANIDINE 4. PERTHITE 5. ALBITE 6. MOONSTONE 7. LABRADORITE 8.OLIGOCLASE, ANDESINE, BYTOWNITE, ANORTHITE
11
“small and inclined” because the cleavage is close to but not quite 90 degrees. Its color ranges from colorless, white, pink, yellow, red, gray or green to blue green
1. MICROLINE
11
“break straight” because the cleavages are at 90 degrees. Its color ranges from colorless, white, gray, yellow, reddish, and greenish. Orthoclase can have cats eye effect.
2. ORTHOCLASE
11
“Sanis”, meaning board, in reference to the tabular crystals. Its color ranges from colorless to pinkish or brownish. Sanidine is not a common mineral and is hardly ever seen as a gemstone.
3. SANIDINE
11
is an intergrowth of albite, oligoclase, plus orthoclase or microcline
4. PERTHITE
11
“Albus” meaning white, because the minerals is usually white. Other colors include, yellow, pink, gray, reddish, greenish, and colorless. Albite is sometimes intergrown with emerald.
5. ALBITE
12
is a sodium potassium aluminum silicate of the feldspar group that displays a pearly and opalescent schiller. An alternative name is hecatolite.
6. MOONSTONE
12
a feldspar mineral in the plagioclase series that is often valued as a gemstone and as ornamental material for its red, blue, or green iridescene.
7. LABRADORITE
12
These Feldspars are rarely encountered in gem form. Their occurrence is widespread throughout the world, in a great variety of rock types and environments. But in the most cases transparent crystals are rare.
OLIGOCLASE, ANDESINE, BYTOWNITE, ANORTHITE
12
PHYSICAL PROPERTIES OF ORTHOCLASE IN TERMS OF CRYSTAL SYSTEM, HABIT, CLEAVAGE, FRACTURE, COLOR
CRYSTAL SYSTEM: MONOCLINIC HABIT: ------ CLEAVAGE: PERFECT FRACTURE: UNEVEN, CONCHOIDAL COLOR: COLOURLESS, GREENISH, GREYISH YELLOW, WHITE, PINK
12
PHYSICAL PROPERTIES OF ORTHOCLASE IN TERMS OF LUSTER, HARDNESS, TENACITY, SPECIFIC GRAVITY, STREAK, TRANSPARENCY
LUSTER: VITREOUS, PEARLY HARDNESS: 6 TENACITY: BRITTLE SPECIFIC GRAVITY: 2.55 - 2.63 STREAK: WHITE TRANSPARENCY: TRANSLUCENT TO TRANSPARENT
12
PHYSICAL PROPERTIES OF PLAGIOCLASE IN TERMS OF CRYSTAL SHAPE, HABIT, CLEAVAGE, FRACTURE, COLOR
CRYSTAL SHAPE: TRICLINIC HABIT: TABULAR (CRYSTALLINE) CLEAVAGE: PERFECT-2DIRECTIONAL FRACTURE: CONCHOIDAL COLOR: WHITE TO DARK GRAY
12
PHYSICAL PROPERTIES OF PLAGIOCLASE IN TERMS OF LUSTER, HARDNESS, TENACITY, SPECIFIC GRAVITY, STREAK, TRANSPARENCY:
LUSTER: VITREOUS USUALLY PEARLY HARDNESS: 6 - 6.5 TENACITY: BRITTLE SPECIFIC GRAVITY: 2.6 - 2.8 STREAK: WHITE TRANSPARENCY: TRANSLUCENT TO TRANSPARENT
12
PROCESS OF FORMATION FELDSPAR
- MANY FELDSPAR ARE IGNEOUS AS THEY COMMONLY PRECIPITATE OUT IN MAGMA AS IT COOLS. - THEY MAY ALSO BE FORMED AS METAMORPHIC MINERALS IN VIENS OF OTHER ROCKS.