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Earth Science Ch. 1

Foundations of Earth Science

QuestionAnswer
____________ are the building blocks of rocks Minerals
Study of minerals is _____________ mineralogy
Defining a Mineral • Geologists’ definition: – Naturally occurring – Inorganic solid – Orderly crystalline structure – Definite chemical composition
___________ are not considered minerals Synthetic materials
Minerals are naturally occurring: – Form by natural geologic processes
Minerals are generally inorganic
Crystalline solids from organic sources are generally not considered minerals generally not considered minerals
Some organisms secrete inorganic compounds like calcium carbonate, this secretion when hardened is Considered a mineral when they become part of the rock record
All Minerals are solid substances except mercury occurs naturally as a liquid
Minerals have an orderly crystalline structure: What is a crystalline structure? – Atoms are arranged in an organized, repetitive manner – Organization is reflected in the crystal shape
Minerals have a chemical composition that allows for some variation such as: – Most minerals are compounds – Can be expressed as a chemical formula – Composition may vary slightly if certain elements substitute for others
Minerals Can be expressed as a chemical formula • Example: quartz = SiO2
Substituting elements about the same size will not change the crystalline structure of the mineral
• A rock is • A rock is a naturally occurring solid aggregate mass of mineral, or mineral-like matter
Most rocks are aggregates of several different minerals
What are the defining characteristics of a mineral? – Naturally occurring – Inorganic – Solid – Crystalline structure – Definite chemical composition
What are the particles that make up an atom? protons Neutrons electrons
do protons have a positive, negative, or neutral charge? positive
do neutrons have a positive, negative, or neutral charge? neutral
do electrons have a positive, negative, or neutral charge negative
All matter — including minerals — is composed of atoms
All atoms ( excluding H and He) formed inside massive stars by nuclear fusion
An atom is the smallest particle that cannot be chemically split
Protons and neutrons have almost identical masses
Electrons are much smaller (1/2000) than protons and t neu rons
– Protons have a charge of +1
Electrons have a charge of -1
Most matter is neutral, because the charges of protons and electrons cancel each other out
Electrons are sometimes shown orbiting the nucleus like planets in a solar system
Electrons actually surround the nucleus like a cloud
Electrons Move around the nucleus in a cloud with different regions called principle shells
Each principle shell of electrons has an energy level and a specific number of electrons
The outer shell of an atom contains valence electrons
The number of protons in the nucleus of an atom gives its atom gives its atomic number atomic number
valence electrons • Interact with valence electrons of other atoms to form chemical bond
atomic number – Determines chemical nature of atom
– All atoms with the same atomic number are known as an element
Approximately __________ naturally occurring l t © 2014 Pearson Education, Inc. elements 90
Elements are arranged in the periodic table
• Elements with similar properties line up in columns
Most minerals are chemical compounds Define chemical compunds – Two or more elements joined together Two or more elements joined together
A few minerals are made up of single elements – Native minerals
What are atomic particles? – Protons – Electrons – Neutrons
– Protons: • Found in the nucleus • H iti h Have a positive charge
– Electrons: • Surround the nucleus like a cloud • Have a negative charge • Valence electrons interact to form bonds
– Neutrons: • Found in the nucleus • Have no charge
Atomic bonding: Elements (excluding noble gasses) form bonds under the temperature and pressure conditions that occur on Earth
Bonds lower the total energy of the atoms and make them more stable
____________valence electrons is a stable arrangement and a full valence shell eight
Elements gain, lose, or share electrons during chemical reactions
• The Octet Rule: – Atoms tend to gain, lose, or share electrons until they have eight valence electrons
A chemical bond is the transfer or sharing of electrons that results in a full valence shell
– Ionic bonds: electrons are transferred Ionic bonds: electrons are transferred
Covalent bonds: electrons are shared
Metallic bonds: electrons move around
When one atom loses or gains valence electron(s): , ions are formed
• Ionic bonds form when ions with opposite charges are attracted
if Electrons are lost: becomes a positive ion
if Electrons are gained: becomes a negative ion
• Ionic bonds form when ions with opposite charges are attracted
NaCl is an ionic compound because: – Na loses a valence electron (becomes positive) – Cl g ( g) ains a valence electron (becomes negativ
• Ionic compounds have very different properties than the bonded elements that make them up
example of ionic bonds: Sodium Chloride – Sodium • Soft, silver, toxic metal that reacts explosively when exposed to water – Chlorine • Poisonous green gas used as a chemical weapon during World War I
A covalent bond forms when electrons are shared between atoms
Metallic bonds form when valence electrons are free to move from one atom to another
metallic bond qualities: All atoms share available valence electrons All atoms share available valence electrons – Movement of valence electrons between atoms results in: • High electrical conductivity • Malleability • Other unique properties of metals
Why do atoms bond? The most stable configuration is eight valence electrons
Ionic bonds form when electrons are transferred from one atom to another
____________ Produces negatively and positively charged ions, which are attracted to each other Ionic bonds
____________form when valence electrons are shared between two atoms covalent bonds
____________form when valence electrons flow Metallic bonds
Minerals have a definite crystalline structure and chemical composition
Luster is the quality of light reflected from the surface of a mineral
– Minerals that look like shiny metal have have a metallic luster
– Nonmetallic luster includes: • Vitreous or glassy, dull, earthy, pearly, silky, and greasy
one physical property of minerls is: Ability to transmit light
Minerals that do not transmit light are opaque
– Minerals that transmit some light, but not an image, Minerals that transmit some light, but not an image, are translucent
Minerals that transmit both light and images are transparent
____________ may be one of the most obvious properties of a mineral, but it is only a diag pp y nostic property for a few minerals Color
Slight variations in the chemical composition of a mineral can change the color dramatically
Streak is the color of a mineral in powdered form
Metallic minerals generally have a dense, dark streak
Nonmetallic minerals generally have a light streak
Not all minerals produce a streak
Streak is obtained by: rubbing the sample on an unglazed porcelain tile known as a streak plate – Streak, unlike color, is generally consistent
Crystal shape or habit is the characteristic shape of individual mineral crystals
The strength of a mineral is determined by the strength of its chemical bonds
Mineral strength determines how minerals break or deform under stress
Tenacity is a mineral’s resistance to breaking or deforming
– Minerals with ionic bonds tend to be brittle • They will shatter
Minerals with metallic bonds are malleable • They can be deformed into shapes and thin sheets
Sectile minerals can be cut into thin shavings
Elastic minerals will return to their original shape after being bent
Hardness is a mineral’s resistance to abrasion or scratching
Hardness is measured on a scale of 1 to 10 Hardness is measured on a scale of 1 to 10: (Moh's Scale)
Cleavage is the tendency of a mineral to break along planes of weak bonding
Cleavage break produces smooth, flat surfaces where the mineral is broken
Fracture is a property resulting from chemical bonds that are approximately equal in strength
Irregular fracture: uneven broken surface
Conchoidal fracture: smooth, curved broken surface
Specific gravity describes the density of a mineral ( weight compared to water volume)
Mineral groups: Economic minerals are less common than rock-forming minerals, but are used extensively in the manufacture of products
eight: The majority of rock-forming minerals are made up of only ___________ elements
Silica and oxygen combine to form the basic building block for the silicates
More than 800 silicate minerals – Make up 90% of the Earth’s crust The remaining mineral groups are often referred to as the nonsilicates
The silicon-oxygen tetrahedron is the building block of all silicates
tetrahedron: Four oxygen atoms surround a much smaller silicon atom
Feldspars are the most plentiful silicates – Over 50% of Earth’s crust
Quartz is second Quartz is second-most-abundant mineral continental crust
Most silicate minerals crystallize from molten rock as it cools
Common light silicate minerals include: – Feldspars – Qua tr z – Muscovite – Clay minerals
___________are the most abundant silicate mineral Feldspars
Feldspars have – 6 on Mohs hardness scale
which silicate mineral Have two directions of cleavage at 90º feldspar
feldspars are found in igneous, sedimentary and metamorphic rocks
Quartz is common in igneous, sedimentary, and metamorphic rocks
Quartz rates a 7 on Mohs hardness scale
quartz – Impurities a variety of colors
Muscovite is a member of the mica family
muscovite has – Excellent cleavage in one direction – 2.5 on Mohs hardness scale
Clay minerals are commonly the weathering product of other silicates
Dark silicate minerals contain iron and magnesium
dark silicate minerals: – Pyroxenes – Amphiboles – Olivine – Biotite – Garnet
Olivine is a major constituent of dark igneous rocks – Abundant in Earth’s upper mantle – Black to olive green color, glassy luster, and granular
Pyroxenes are an important component of dark-col d ore igneous rocks – Augite is black and, opaque and has two directions of cleavage at nearly 90º
The amphibole group includes minerals that commonly make up the dark portion of light-colored rocks
• Nonsilicate minerals are divided into groups based on the negatively charged ion common to the group to the group
Nonsilicates make up only about ______ of Earth’s crust 8%
What are the different mineral groups? Silicates and non silicates
Silicates (the most common) are based on the silicon-oxygen tetrahedron
Subdivided into light and dark groups silicates
– Nonsilicates include negatively charged ions
non silicates are: • Common in sedimentary rocks • Many are economically important
Who thinks your great? Me!
Created by: Sargon
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