Minerals APSC 151 Study Notes
Course Information
Course Title: Minerals APSC 151: Earth Systems Engineering
Semester: Fall 2025
Instructors:
Dr. Jennifer Day, PhD, EMBA, PEng, PGeo
Dr. Dan Layton-Matthews, PhD (known as DL-M)
Dr. Chris Spencer, PhD, PGeo
Affiliation: Department of Geological Sciences and Geological Engineering
Housekeeping
Labs in APSC 151: Start on Wednesday, Sept 3rd, at 8:30 AM in Miller Hall (Room #20 on campus map).
There are 13 lab sections over the next two weeks. Check your scheduling.
Groups 08-A to 08-H will meet in Room 106.
Groups 08-I to 08-Q will meet in Room 102.
How to Check Group Number:
Log into onQ
Navigate to APSC 151 course page > Main Menu Bar > Communications > Groups
Bring a device/laptop to class.
Overview of Minerals
Earth Materials: The course focuses on the interesting earth materials surrounding us, with more than 6000 known minerals.
Annually, ~50-100 new minerals are discovered.
Mineralogy
Definition: The scientific and engineering study of minerals, which began in the 16th century.
Key Contributions:
1556: Georgius Agricola published De Re Metallica (On the Nature of Metals), providing the first descriptions of minerals.
1669: Nicholas Steno discovered geometric properties, initiating systematic description of minerals (e.g., Quartz: SiO2).
Mineral Names
Origins of Mineral Names:
Derived from various languages, properties, places, composition, and people:
Languages:
German: orthoclase (splits at right angles)
Latin: albite (white)
Properties:
Color: olivine is olive green
Places:
Skutterudite (Skutterud, Norway)
Illite (Illinois, USA)
Composition:
Chromite (chromium bearing)
Borax (contains boron)
Notable Individuals:
Jimthompsonite (James Thompson)
Schwertmannite (Udo Schwertmann)
Definitions
Mineral:
Naturally occurring
Inorganic
Solid
Ordered internal molecular structure
Definite chemical composition
Example: Garnet, Ca3Al2(SiO4)3
Rock:
A solid mass of minerals.
Biogenic Minerals
Definition: Minerals created by living organisms. Examples include:
Vertebrate bones (Apatite: Ca5(PO4)3(F,Cl,OH))
Oyster, mussel, clam shells (Aragonite: CaCO3)
Minerals created by bacteria (e.g., Fe Oxide, Aragonite)
Human teeth (Apatite)
Composition of Minerals
Elements: Basic building blocks of minerals.
There are 188 known elements, with 90 being naturally occurring.
Structure of Minerals
Crystalline Structure: Most solid materials are crystalline, with an ordered array of atoms bonded chemically.
Example: Halite (NaCl)
Polymorphism in Minerals
Definition: Polymorph refers to elements that can join in more than one geometric arrangement while maintaining the same chemical composition, leading to different physical properties.
Examples:
Graphite: Carbon atoms arranged in hexagonal structures.
Diamond: Carbon atoms arranged in tetrahedral structures.
Physical Properties of Minerals
Key properties include:
Crystal shape (habit)
Luster
Color
Streak
Hardness
Cleavage
Fracture
Specific gravity
Special properties.
Description Methods
Physical properties help in describing minerals by various characteristics:
Crystal Shape (Habit): Varies based on elements and arrangement.
Influenced by ion size and packing configurations.
Luster: Appearance in reflected light categorized into:
Metallic
Non-metallic: Descriptors include vitreous, milky, silky, earthy.
Examples: Quartz SiO2 (vitreous), Pyrite FeS2 (metallic).
Color: Varies and can help identify minerals when used cautiously.
Example: Cu2CO3(OH)2 can be green, yellow, pink, etc.
Impurities can cause color variations (e.g., Quartz: clear, white, rose, smoky, purple).
Streak: Color of a mineral in powdered form, obtained by rubbing on a streak plate.
Examples: Hematite Fe2O3, Magnetite Fe3O4 yield reddish-brown and black streaks.
Hardness: Measurement of mineral resistance to abrasion or scratching, compared to Mohs scale of hardness.
Cleavage: Tendency to break along planes of weak bonding, producing flat surfaces.
Fracture: Absence of cleavage when a mineral is broken, examples include conchoidal fractures that produce smooth, curved surfaces.
Specific Gravity: Ratio of mineral's weight to equivalent volume of water, ranging approximately between 2.5 and 3.
Special Properties: Includes magnetism, reaction to hydrochloric acid, malleability, double refraction, taste, smell, and elasticity (e.g., Calcite CaCO3).
Mineral Classes
Approximately 6000 identified minerals categorized mainly into:
Rock-Forming Minerals: Composed of the eight elements constituting over 98% of continental crust:
Order of Abundance: Oxygen, Silicon, Aluminum, Iron, Calcium, Sodium, Potassium, and Magnesium.
The Silicates: Most common mineral group characterized by the silicon-oxygen tetrahedron as the basic unit.
Examples:
Isolated: Olivine (Mg, Fe)2SiO4
Chains: Pyroxene (single), Amphibole (double).
Ferromagnesian Silicates: Containsions of iron and/or magnesium; examples include Olivine, Pyroxenes, Amphiboles, Biotite, and Garnet.
Nonferromagnesian Silicates: Contains aluminum, potassium, calcium, sodium; examples are Muscovite, K-feldspar (orthoclase), Plagioclase, and Quartz.
Non-silicate Mineral Groups: Include Oxides, Hydroxides, Sulphides, Sulphates, Native Elements (e.g., Gold), Halides, Carbonates, and Phosphates.
Applications and Implications
Engineering Connections: Discussion of career paths such as involvement with NASA and geological engineering applications impacting extraterrestrial materials, resource evaluation for lunar and Martian colonization requirements, etc.