Term
| The scientific study of the Earth |
|
Definition
|
|
Term
| the study of Earth's materials |
|
Definition
|
|
Term
| the building blocks of rocks |
|
Definition
|
|
Term
| naturally occurring, inorganic, crystalline solid, physically and chemically ditinctive |
|
Definition
|
|
Term
|
Definition
|
|
Term
| not synthesized in the laboratory |
|
Definition
|
|
Term
| no animal or vegetable matter |
|
Definition
|
|
Term
| regular internal structure; 3D framework |
|
Definition
|
|
Term
| a substance that can not be broken down into others by ordinary chemical reactions |
|
Definition
|
|
Term
| the smallest unit of a stubstance that retains the properties of that element |
|
Definition
|
|
Term
|
Definition
|
|
Term
|
Definition
|
|
Term
|
Definition
|
|
Term
| represents a tiny fraction of the volume at the center of an atom, but nearly all mass |
|
Definition
|
|
Term
|
Definition
|
|
Term
| electrons orbit the nucleus in discrete ___ or energy levels |
|
Definition
|
|
Term
| represent nearly all of the volume of an atom, but only a tiny fraction of the mass |
|
Definition
|
|
Term
| number of protons in the nucleus |
|
Definition
|
|
Term
| number of protons and neutrons in the nucleus |
|
Definition
|
|
Term
| atoms of an element with different numbers of neutrons |
|
Definition
|
|
Term
| retain all of their protons and neutrons through time |
|
Definition
|
|
Term
| spontaneously lose subatomic particles from their nuclei over time |
|
Definition
|
|
Term
| controlled by outermost shell (valence) electrons |
|
Definition
|
|
Term
| typically react unless their valence shell is full |
|
Definition
|
|
Term
| atoms or groups of atoms with unequal numbers of protons and electrons, thus having a non-zero charge |
|
Definition
|
|
Term
| the smallest unit of a compound that retains the properties of that substance |
|
Definition
|
|
Term
| atoms of 2 or more different elements bonded together |
|
Definition
|
|
Term
| NaCI (salt), H2O (water), and SiO2 is an example of: |
|
Definition
|
|
Term
| involves transfer of valence electrons from one agom to another |
|
Definition
|
|
Term
| involves sharing of valence electrons among adjacent atoms |
|
Definition
|
|
Term
| electrons flow freely throughout metals; results in high electrical conductivity |
|
Definition
|
|
Term
| residual forces remaining after atoms have bonded |
|
Definition
|
|
Term
| may not be consistent for all minerals |
|
Definition
|
|
Term
| color of mineral in powder form |
|
Definition
|
|
Term
| the way a mineral's surface reflects light |
|
Definition
|
|
Term
| Vitreous (shiny like glass), Earthy - (has the irridescence of a pearl), Waxy - (like wax), and Resinous - (like resin) are all examples of: |
|
Definition
| nonmetallic physcial properties of minerals |
|
|
Term
|
Definition
|
|
Term
| the tendency of a mineral to break along a definite plane |
|
Definition
|
|
Term
| irregular break in a mineral |
|
Definition
|
|
Term
|
Definition
|
|
Term
| Physical Properties of Minerals are: |
|
Definition
Specific Gravity
Double Refraction
Magnetism
Smell
Taste
Striations
|
|
|
Term
| atoms or groups of atoms with unequal numbers of protons and electrons, thus having a non-zero charge |
|
Definition
|
|
Term
| positive and negative ioins are attracted to one another and may stick or ___. |
|
Definition
|
|
Term
| density relative to that of water |
|
Definition
|
|
Term
|
Definition
|
|
Term
| because of weak bonds, ___ splits easily between "sandwiches" |
|
Definition
|
|
Term
| positive ions, sandwiched between tow sheet silicate layers |
|
Definition
|
|
Term
| Nearly 97% of the atoms in Earth's crust are represented by the 8 most common elements O, Si, AI, Fe, Ca, Na, K, Mg |
|
Definition
|
|
Term
| O, Si, AI, Fe, Ca, Na, K, Mg are examples of: |
|
Definition
| common elements that make up 97% of the atoms in Earth's crust |
|
|
Term
|
Definition
|
|
Term
| common mineral types which make in most minerals |
|
Definition
|
|
Term
| Mineral structure with regular 3D arrangement of atoms |
|
Definition
|
|
Term
| a negative ion is sometimes called a(n) |
|
Definition
|
|
Term
| attachment of an atom to one or more adjacent atom important in determing properties of minerals |
|
Definition
|
|
Term
| guide used to identify minerals based on the mineral's properties |
|
Definition
|
|
Term
| has the carbonate ion (e.g., calcite, dolomite) |
|
Definition
|
|
Term
| has sulfides in it (pyrite and chalcopyrite) |
|
Definition
|
|
Term
|
Definition
|
|
Term
|
Definition
|
|
Term
| hematite, goethite, magnetite |
|
Definition
|
|
Term
| sulfur, copper, and gold are examples of |
|
Definition
|
|
Term
| glass that is rigid but lacks the ordered arrangement of atoms |
|
Definition
|
|
Term
| minerals in the Bowen's reaction series |
|
Definition
|
|
Term
| used to represent the 4 oxygen atoms surrounding a silicon atom |
|
Definition
|
|
Term
| within a silicon-oxygen tetrahedron, the negative charges exceed the ______. |
|
Definition
|
|
Term
|
Definition
|
|
Term
| for the silicon-oxygen tetrahedron to be stable within a crystal structure it must be balanced by positively charged ions or |
|
Definition
| share oxygen atoms with adjacent tetrahons |
|
|
Term
| For the silicon-oxygen tetrahedron to be stable within a crystal structure it must share oxygen atoms with adjacent tetrahedrons or |
|
Definition
| must be balanced by positively charged ions |
|
|
Term
| and example of an isolated tetrahedra is: |
|
Definition
|
|
Term
| the more shared __ atoms per tetrahedron, the more complex the silicate structure |
|
Definition
|
|
Term
| 2 shared O atoms of a tetrahedron; Augite |
|
Definition
|
|
Term
| alternating 2 and 3 shared O atoms; muscovite & biotite |
|
Definition
|
|
Term
| 4 shared O atoms per tetrahedron; feldspar & quartz |
|
Definition
|
|
Term
| contain CO3 in their structures (e.g., calcite - CaCO3) |
|
Definition
|
|
Term
| contains SO4 in their structures (e.g., gypsum - CaSO4. 2H2O) |
|
Definition
|
|
Term
| contain O, but not bonded to Si, C or S (e.g., hematite - Fe2O3) |
|
Definition
|
|
Term
| composed entirely of one element (e.g., diamond - C; gold Au) |
|
Definition
|
|
Term
| molten rock, forms below Earth's surface or inside the Earth |
|
Definition
|
|
Term
| rocks that crystallize from magma at depth; also known as plutonicc rocks emplaced into surrounding country rock |
|
Definition
|
|
Term
| molten material extruded out into the Earth's surface |
|
Definition
|
|
Term
| rocks that crystallize from lava at the Earth's surface; also known as volcanic rocks |
|
Definition
|
|
Term
| rocks are identified based on |
|
Definition
|
|
Term
| over ___ minerals have been identified |
|
Definition
|
|
Term
| over 90% of Earth's crust is composed of minerals from which 5 groups |
|
Definition
| feldspars, pyroxenes, amphiboles, micas, and quartz |
|
|
Term
| the primary source of metals |
|
Definition
|
|
Term
| to be considered a current resource minerals must |
|
Definition
| be able to be extracted profitably |
|
|
Term
| rocks that crystallize from magma or lava |
|
Definition
|
|
Term
| molten rock or liquid that is mostly silica below Earth's surface |
|
Definition
|
|
Term
| magma that erupted on Earth's surface |
|
Definition
|
|
Term
| igneous rocks that crystallize below Earth's surface |
|
Definition
|
|
Term
| igneous rock that crystallizes above the Earth's surface |
|
Definition
|
|
Term
| overall appearance of a rock; controlled by rate of cooling |
|
Definition
|
|
Term
| mineral makeup of the rock; controlled by the chemical composition of the magma |
|
Definition
|
|
Term
| Earth's crust and mantle are: |
|
Definition
|
|
Term
|
Definition
| liquid, iron-rich, very dense, and remains deep inside the Earth |
|
|
Term
| composed of silica and dissolved gases, high temperature, and ability to flow are: |
|
Definition
|
|
Term
| intergrown crystals that are roughly equal in size; large enough to be seen |
|
Definition
|
|
Term
| individual minerals that make up the rock can only be seen under the microscope |
|
Definition
|
|
Term
| large crystals (phenocrysts) are embedde in an aphanitic matrix (groundmass) |
|
Definition
|
|
Term
| consolidated rock fragments during volcanic eruptions |
|
Definition
|
|
Term
| aphanitic rocks that have vesicles or spherical and elongated openings or cavities |
|
Definition
|
|
Term
| forms when magma is rapidly cooled |
|
Definition
|
|
Term
| volcanic benefits include: |
|
Definition
| Hawaii, geothermal energy, climate |
|
|
Term
|
Definition
|
|
Term
| factors affecting viscosity are |
|
Definition
| composition and temperature |
|
|
Term
| the more ___ ___ present in lava flows, the more fluid the lava flow |
|
Definition
|
|
Term
| One cause of violent volcanic eruptions is the ____ of the magma |
|
Definition
|
|
Term
| quantity of ___ ___ and ease with which they can escape |
|
Definition
|
|