Matter and minerals Flashcards
Mineral
- Naturally occurring
- Solid within temperature range normally found at Earth’s Surface
- Orderly crystalline structure where atoms are arranged in an orderly, repetitive manner
- Well-defined chemical composition
- Generally inorganic, though some may contain carbon
Valence electrons
Electrons in the outermost shell.
Isotope
Atoms with differing proton and neutron counts.
Ion
Atom with differing proton and electron counts, causing an electrical charge.
Cation
Atom that with fewer electrons than protons and so has a positive charge.
Anion
Atom with more electrons than protons and so has a negative charge.
Compounds
Some combination of different elements
Elements form chemical bonds in order to?
Fill their outermost shells with electrons
Ionic bond
One element loses an electron and becomes positively charged. Another element gains an electron and becomes negatively charged. The oppositely charged ions are attracted and bond
Covalent bond
electron orbits (shells) can overlap with those of adjacent elements and so electrons are shared. e.g. Cl2 is the bond of two chlorine atoms sharing a single electron to fill their valence shell.
Metallic bond
Metallic atoms pack together as cations. Their electrons are mobile and move about freely to be shared among the cations. Occurs among a small number of minerals e.g. copper.
Diamond atomic structure
each carbon atom shares electrons with four adjacent carbon atoms in a tetrahedral arrangement.
Different minerals have different crystal forms due to differences in?
The internal arrangement of atoms.
What can we say about the faces and angles of a crystal?
Although some of the faces may grow larger than others, the angles between equivalent facer are constant for a given mineral.
Polymorphs
two minerals that have the same chemical composition but differ in crystal structure. e.g. graphite/diamond, calcite/aragonite
Silicates
Minerals comprised of silicon ions surround by four oxygen ions (SiO4)^-4. This is the basic building block is the Silicon-Oxygen Tetrahedron
General formula for silicates:
(SiO4)^-4 + cations.
Pyroxene group
Two planes at right angles. Single chains of Silicon-Oxygen Tetrahedrons. e.g. augite
Amphibole group
Two planes at 60 and 120 degrees. Double chains of silicon-oxygen tetrahedrons. e.g. hornblende
Micas are examples of?
Sheet silicates
Most common minerals in Earth’s crust?
Silicates
Carbonates
Basic unit is the (CO3)^-2 complex. There are different carbonate minerals depending on which cation is attached to the carbonate complex. The two most important carbonates are calcite (CaCO3) and dolomite (CaMg(CO3)2)
Oxides
Cations are bounded to oxygen: O^-2 + cations.
Two important oxides:
- Hematite (Fe2O3)
- Magnetite (Fe3O4)
Sulfates
Sulfur is present as the sulfate ion (SO4)^-2 (SO4)^-2 + cations Two important sulfates: - Anhydrite (CaSO4) - Gypsum (CaSO4 * 2H20)
Sulfides
Many important ore deposits exist as sulfides: S^-2 + cations Two important sulfides: - Pyrite (FeS2) - Galena (PbS)
Halides
Generally form ionic bonds. Some precipitate from salty water. Important Halides: - Halite (NaCl) - Sylvite (KCl) - Fluorite (CaF2)
Native Element Minerals
Composed of only one element
e.g. graphite (C), diamond (C), copper (Au), gold (Au), sulfur (S)
Streak
the color left behind when scratching a mineral on a tile of unglazed porcelain.
Hardness
the measure of the ease with which the surface of a mineral can be scratched.
Tenacity
describes a mineral’s toughness, or resistance to breaking or deforming
Cleavage
tendency of a crystal to break along flat planar surfaces.
- Covalent bonds are generally strong and have poor cleavage e.g. quartz
- Ionic bonds are relatively weak and yield good cleavage e.g. halite and calcite
Fracture
tendency of a mineral to break along irregular surfaces other than cleavage planes.
- Conchoidal (smooth, curved surfaces)
- Fibrous (similar to splitting wood)
- Irregular
Specific Gravity
a measure of the mass of a mineral divided by the mass of an equal volume of water.
Heavier minerals have higher specific gravity.
Luster
the way a mineral reflects light
- Metallic (strong reflections by opaque minerals)
- Vitreous (reflects like glass)
- Dull (earthy)
- Greasy (appearance of being coated with oil)
Adamantine (brilliant luster of diamond)
Form/Habit
the shape in which a crystal grows
- Bladed
- Prismatic
- Banded
- Botryoidal