Chapter 4 Flashcards
Atomic number
the number of protons in its nucleus
Atomic mass
the number of neutrons and protons in the nucleus
Isotopes
atoms of an element having the same atomic number but differing mass number
Ion
an atom with a positive or negative charge
Anion
atom gains electron that has a negative charge
Cation
atoms loses electron that has a positive charge
Ionic bond
two oppositely charge ions are attracted to form a bond
Covalent bond
elements “share” electrons to fulfill their outermost shells
Metallic bond
like covalent bonding except all the extra valence electrons of a large group of atoms are considered together in what is called an “electron sea” that is shared by all the atoms in the group
Silicates
silicon and oxygen formed a covalent bond to create the silicate compound
What structure does silicate have?
tetrahedron
Substitution
some cations can substitute for another because of the similar size and charge
Silicate structure of olivine
independent tetrahedron
Silicate structure of pyroxene
single chain
Silicate structure of amphibole
double chin
Silicate structure of micas
sheet
Silicate structure of feldspar and quartz
3D network (framework)
Olivine
Element and rock
Fe, Mg
olivine
Pyroxene group
Element and rock
Fe, Mg, Al, Ca, Na
augite
Amphibole group
Element and rock
Ca, Na, Fe, Mg, Al
hornblende
Micas group, Biotite
Element and rock
K, Fe, Mg
biotite, muscovite
Feldspar group
Element and rock
K, Na, Ca, Al, Si, O
orthoclase, plagioclase
Quartz
Element and rock
SiO(2)
quartz
Calcite
Element and rock
CaCO(3)
calcite
Sulfates
compounds of metallic cations bonded with sulfate anion
Sulfides
compounds of metallic cations bonded with sulfur
Oxides
compounds of metallic cations bonded to oxygen atoms
Carbonates
compounds of cations bonded with the carbonate ion
Cleavage
breakage along planes of weakness
Fracture
breakage not along cleavage plane
Hardness
resistance to scratching or abrasion
Luster
character of reflected light
Crystal form
geometric shape
Reaction to HCI
chemical interaction of weak hydrochloric acid (HCI) and calcium carbonate (CaCO[3])
Streak
color when powered
Mohs hardness scale
uses numerical values 1-10
Ex: diamond = 10, quartz = 7, talc = 1
How minerals form when magma cools
magma rises from mantle and from melted crust cools as it penetrates solid rock which allows igneous minerals to crystallize