AY Honors/Rocks & Minerals/Answer Key
Skill Level
2
Year
1937
Version
05.11.2024
Approval authority
General Conference
1
A mineral is a naturally occurring, inorganic solid with a definite chemical composition and a crystalline structure formed by geological processes. A rock is an aggregate of one or more minerals. (A rock may also include organic remains and mineraloids.) Some rocks are predominantly composed of just one mineral. For example, limestone is a sedimentary rock composed almost entirely of the mineral calcite. Other rocks contain many minerals, and the specific minerals in a rock can vary widely. Some minerals, like quartz, mica or feldspar are common, while others have been found in only one or two locations worldwide.
2
Identifying rocks and minerals is best done with a Field Guide. The following properties are very useful for identification purposes:
- Hardness
- Cleavage
- Specific gravity
- Luster
- Color
- Streak
- Texture
- Crystalline structure
These are described in detail in requirements 4 and 5.
You will need a few tools for measuring various aspects of rocks. Not all of them are required, but the more of them that are available to you, the more successful you will be in identifying specimens.
- Specific Gravity meter
- Ceramic tile for determining "scratch" color
- Magnifying glass
- Hardness kit (you can use the following as a hardness kit as explained in requirement 4)
- Fingernail
- Copper penny
- Knife blade
- Window glass
- Steel file
3
3a
- Igneous
- Igneous rock is formed when lava cools and solidifies.
Basalt
Granite
Obsidian
Gabbro
3b
- Sedimentary
- Sedimentary rock is formed when sediments carried by wind or water settle and turn to stone.
Chalk
Limestone
Sandstone
Shale
3c
- Metamorphic
- Metamorphic rock is formed when another type of rock is transformed by great heat and pressure.
Slate
Marble
Gneiss
Schist
4
The Mohs scale of mineral hardness characterizes the scratch resistance of various minerals through the ability of a harder material to scratch a softer material. It was created in 1812 by the German mineralogist Friedrich Mohs and is one of several definitions of hardness in materials science.
Mohs based the scale on ten minerals that are all readily available. As the hardest known naturally occurring substance, diamond is at the top of the scale. The hardness of a material is measured against the scale by finding the hardest material that the given material can scratch, and/or the softest material that can scratch the given material. For example, if some material is scratched by apatite but not by fluorite, its hardness on the Mohs scale is 4.5.
The Mohs scale is a purely ordinal scale. For example, corundum (9) is twice as hard as topaz (8), but diamond (10) almost four times as hard as corundum. The table below shows comparison with absolute hardness measured by a sclerometer.
| Hardness | Mineral | Absolute Hardness |
|---|---|---|
| 1 | Talc
(Mg3Si4O10(OH)2) |
1 |
| 2 | Gypsum (CaSO4·2H2O) | 2 |
| 3 | Calcite (CaCO3) | 9 |
| 4 | Fluorite (CaF2) | 21 |
| 5 | Apatite
(Ca5(PO4)3(OH-,Cl-,F-)) |
48 |
| 6 | Orthoclase Feldspar (KAlSi3O8) | 72 |
| 7 | Quartz (SiO2) | 100 |
| 8 | Topaz (Al2SiO4(OH-,F-)2) | 200 |
| 9 | Corundum (Al2O3) | 400 |
| 10 | Diamond (C) | 1500 |
On the Mohs scale, fingernail has hardness 2.5; copper penny, about 3.5; a knife blade, 5.5; window glass, 6.5; steel file, 6.5. Using these ordinary materials of known hardness can be a simple way to approximate the position of a mineral on the scale.
One mnemonic traditionally taught to geology students to remember this table is "To Get Candy From Aunt Fanny, Quit Teasing Cousin Danny".
An alternative table is shown below which has been modified to incorporate additional substances that may fall in between two levels.
Source: American Federation of Mineralogical Societies: Mohs Scale of Mineral Hardness
| Hardness | Substance or Mineral |
|---|---|
| 1 | Talc |
| 2 | Gypsum |
| 2.5 to 3 | pure Gold, Silver |
| 3 | Calcite, Copper penny |
| 4 | Fluorite |
| 4 to 4.5 | Platinum |
| 4 to 5 | Iron |
| 5 | Apatite |
| 6 | Orthoclase |
| 6.5 | Iron pyrite |
| 6 to 7 | Glass, Vitreous pure silica |
| 7 | Quartz |
| 7 to 7.5 | Garnet |
| 7 to 8 | Hardened steel |
| 8 | Topaz |
| 9 | Corundum |
| 10 | Diamond |
| 11.1 | Aggregated diamond nanorods |
5
The terms that follow have specific meaning in mineralogy, and are useful for identifying the type of a specimen of rock or mineral. To the uneducated eye, a rock is a rock is a rock. But if the following terms are understood, noted, and cross-checked against known values for various specimens, a positive identification can be made.
5a
Cleavage is the tendency of crystalline materials to split along definite planes, creating smooth surfaces, of which there are several named types:
- Basal cleavage: cleavage parallel to the base of a crystal, or to the plane of the lateral axes. This occurs quite easily in graphite, making the material feel slippery.
- Cubic cleavage: cleavage parallel to the faces of a cube. This is the source of the cubic shape seen in crystals of ground table salt.
- Diagonal cleavage: cleavage parallel to a diagonal plane.
- Lateral cleavage: cleavage parallel to the lateral planes.
- Octahedral, Dodecahedral, or Rhombohedral cleavage: cleavage parallel to the faces of an octahedron, dodecahedron, or rhombohedron (respectively). Octahedral cleavage is seen in common semiconductors used in electronics.
- Prismatic cleavage, cleavage parallel to a vertical prism.
Cleavage is of technical importance in the electronics industry and in the cutting of gemstones. While precious stones are generally cleaved by impact, man-made single crystals of semiconductor materials are generally sold as thin wafers which are much easier to cleave. Simply pressing a silicon wafer against a soft surface and scratching its edge with a diamond scribe is usually enough to cause cleavage.
5b
Specific gravity is the ratio of the density of a material relative to the density of water. Density is the ratio of an object's mass to its volume. For instance, we know that 1 cm^3 of water weighs 1 gram. Therefore, the density of water is:
- [math]\displaystyle{ density_{water} = \frac{1 gram}{1 cm^3} = 1g/cm^3 }[/math]
A cubic centimeter of diamond would weigh 3.52 grams, so we can calculate the density of diamond as:
- [math]\displaystyle{ density_{diamond} = \frac{3.52 grams}{1 cm^3} = 3.52g/cm^3 }[/math]
Finally, we can calculate the specific gravity (G) of diamond:
- [math]\displaystyle{ G = \frac{density_{specimen}}{density_{water}} = \frac{3.52g/cm^3}{1g/cm^3} = 3.52 }[/math]
Division by 1 is a lovely thing!
What this really boils down to is that any given volume of diamond will weigh 3.52 times more than an equal volume of water. If you know the specific gravity, [math]\displaystyle{ G }[/math] of any material, you will know that it weighs [math]\displaystyle{ G }[/math] times an equal volume of water.
But what use is specific gravity? It helps us identify a mineral. We can measure a sample's specific gravity and compare it to the specific gravities of known specimens. To do this, we will need to make two measurements: the weight of the specimen, and its volume. Weight is easy (assuming you have a scale or a balance that can measure grams), but how do you measure the volume of an irregularly shaped specimen? All you need is some water, a drop of dish soap, and a graduated cylinder marked in metric units (note that 1 milliliter equals 1 cubic centimeter). Put some water in the cylinder, adding enough until the level comes to a convenient, well-marked level (such as 100 ml). Add a drop of dish soap to break the surface tension (you won't need more than a tiny drop). Then drop the specimen into the water and note the new water level. Subtracting the new level from the old will give you the volume of the specimen. Now all you need to do is divide the weight in grams by the volume in milliliters.
5c
Luster is a description of the way light interacts with the surface of a crystal, rock, or mineral. For example, a diamond is said to have an adamantine luster and pyrite is said to have a metallic luster.
Other descriptive terms used for gems include vitreous, like glass; resinous, like amber; waxy, like jade; greasy, like soapstone; pearly; and silky.
5d
Color indicates the appearance of the mineral in reflected light (for opaque specimens) or transmitted light (for translucent specimens). In other words, it means just what you would think it means - what it looks like to the naked eye. Before noting the color of a specimen, it is important to clean it off.
5e
The streak (also called powder color) of a mineral is the color of the powder produced when it is dragged across an unweathered surface. Unlike the apparent color of a mineral, which for most minerals can vary considerably, the trail of finely ground powder generally has a more consistent characteristic color, and is thus an important diagnostic tool in mineral identification. If no streak seems to be made, the mineral's streak is said to be white or colorless. Streak is particularly important as a diagnostic for opaque and colored materials. It is less useful for silicates, most of which have a white streak and are too hard to powder easily.
The apparent color can vary widely because of trace impurities or a disturbed macroscopic crystal structure. Small amounts of an impurity that strongly absorbs a particular wavelength can radically change the wavelengths of light that are reflected by the specimen, and thus change the apparent color. However, when the specimen is dragged to produce a streak, it is broken into randomly oriented microscopic crystals, and small impurities do not greatly affect the absorption of light.
The surface across which the mineral is dragged is called a "streak plate," and is generally made of unglazed porcelain tile. In the absence of a streak plate, the underside of a porcelain bowl or vase, the surface of an electrical fuse, or the back of a glazed tile will work. Sometimes a streak is more easily or accurately described by comparing it with the "streak" made by another streak plate.
Because the trail left behind results from the mineral being crushed into powder, a streak can only be made of minerals softer than the streak plate, around 7 on the Mohs scale of mineral hardness. In this case, the color of the powder can be determined by filing or crushing with a hammer a small sample, which is then usually rubbed on a streak plate. Most minerals that are harder have an unhelpful white streak.
Some minerals leave a streak similar to their natural color, such as cinnabar and azurite. Other minerals leave surprising colors, such as fluorite, which always has a white streak, although it can appear in purple, blue, yellow, or green crystals. Hematite, which is black in appearance, leaves a red streak which accounts for its name, which comes from the Greek word "haima," meaning "blood." Galena, which can be similar in appearance to hematite, is easily distinguished by its gray streak.
5f
Texture in geology refers to the physical appearance or character of a rock, such as grain size, shape, and arrangement, both to the naked eye and under a microscope.
5g
A crystal is a solid whose atoms, molecules, or ions are packed in a regularly ordered, repeating pattern extending in all three spatial dimensions. Snowflakes, diamonds, and common salt are common examples of crystals.
6
Uses for Rock
- Building material
- Gravel
- Paving stones
- Grinding grain into meal (millstones)
- Sharpening blades (whetstones)
- Sculpture medium (marble, granite, others)
- Fill material
- Fuel (coal)
- Ores (most metals are extracted from ore)
Uses for Minerals
- Abrasives (diamond dust, garnet, others)
- Lasers (sapphire, ruby)
- Electronics (semiconductors)
- Lenses (quartz)
- Nutrition (your body needs many minerals)
- Traction (silica - also known as sand)
- Currency (gold, silver, copper)
- Pencil lead (graphite)
- Lubricant (graphite)
- Medicine (Kaopectate is made from the mineral kaolin)
7
- Exodus 24:16-18
- God carves the ten commandments in stone.
- Numbers 20:2-13
- God commands Moses to speak to the rock to provide water for the Israelites but Moses hits it instead.
- 1 Samuel 17
- David kills Goliath with a stone.
- Daniel 2:34
- A stone is cut without hands and destroys the image in Nebuchadnezzar's dream.
- John 11:38-44
- Jesus orders that the stone covering the tomb of Lazarus be removed.
- Matthew 7:24-29
- The parable of the wise and foolish builders.
- Acts 6-7
- The stoning of Stephen.
8
Revelation 21:19,20 describes the foundation stones of the New Jerusalem.
1. Jasper 
2. Sapphire 
3. Chalcedony (Carbuncle?) 
4. Emerald 
5. Sardonyx 
6. Sardus (Ruby?) 
7. Chrysolite 
8. Beryl 
9. Topaz 
10. Chrysophase 
11. Jacinth (Turquoise?) 
12. Amethyst (Chrystal?)
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The wall has twelve foundation stones, and on these are written the names of the Twelve Apostles. Revelation lacks a list of the names of the Twelve Apostles, and does not describe which name is inscribed on which foundation stone, or if all of the names are inscribed on all of the foundation stones, so that aspect of the arrangement is open to speculation. One scholar hold that Judas Iscariot's name is absent from the foundations, replaced by that of another Apostle.
These foundation stones are adorned with twelve types of precious stones. In modern times, the precise identification of all these precious stones is not certain, as several of the ancient names may refer to several different types of stones, or may no longer refer to the same kinds of stones that they did at the time of Revelation's writing. Also, the layout of the precious stones is contested. All of the precious stones could adorn each foundation stone, either in layers or mixed together some other way, or just one unique type of stone could adorn each separate foundation stone.
References
Wikipedia Articles
