Geology 1110 Test 1

Atom

Smallest individual particle retaining properties of an element

Element

Fundamental substances into which matter can be broken down chemically

Mineral

Naturally formed inorganic solid that has a specific chemical composition and a distinct crystal structure; composed of elements

Rock

Naturally formed, coherent mass of one or more minerals, sometimes including organic debris

What characteristics does a mineral have?

1) Naturally formed; 2) inorganic; 3) solid; 4) specific chemical composition 5; ) characteristic crystal structure

Mineraloids

Lack specific composition and/or characteristic crystal structure

What is a nucleus?

It is the central part of an atom that is made of protons and neutrons and despite its small volume contains most of the mass of the atom

Atomic Number

Number of protons in nucleus

Mass Number

Total number of protons plus neutrons

Isotopes

Atoms with the same atomic number but different mass numbers

Electrons

Contribute very little mass; move around nucleus in complex
3-D patterns called orbitals; energy-level shells are groupings of orbitals

Ion

Atom with excess positive or negative charge caused by electron transfer

What charge does a Cation have?

Positive

What charge does a anion have?

Negative

Compounds

Atoms of two or more elements combined in a specific ratio

Molecule

the smallest unit

What are the different types of bonds?

Ionic, Covalent, Metallic, and van der Waals

Ionic

Electrostatic attraction between + & - charged particles

Covalent

The strongest of the bonds that occurs when atoms share electrons

Metallic

Closely packed atoms; electrons shared between several atoms

van der Waals

Weak secondary attraction between certain molecules

Complex ions

Two or more ions that act as a single entity

Crystal Structure

geometric patterns of atoms in a solid

Crystalline

Has a crystal structure

Amorphous

Lack Crystal structure

Ionic Substitution

Ions with similar sizes and charges can substitute for each other

Mineral Group

Displays extensive ionic substitution w/o changing cation:anion ratio

Crystal form (and growth habit)

Geometric arrangement of crystal faces

Polymorphs

2+ minerals w/ same composition but different crystal structures

What are the different properties of minerals?

cleavage, luster, color, streak, hardness, density, and specific gravity

Cleavage

Mineral's tendency to break in preferred directions along planar surfaces

Luster

Quality and intensity of light reflected from a mineral

Color

Often striking, but unreliable means of identification

Streak

Thin layer of powdered mineral made by rubbing it on non-glazed porcelain

Hardness

Mineral's relative resistance to scratching

Mohs hardness scale

(I) talc, (2) gypsum, (3) calcite, (4) fluorite, (5) apatite,
(6) orthoclase (feldspar), (7) quartz, (8) topaz, (9) corundum and (10) diamond

Density

mass/unit volume

specific gravity

ratio of mass of substance to mass of equal volume of water

What are the 12 most abundant elements?

O,Si,AI,Fe,Ca,Mg,Na,K,Ti,H,Mn & P

What parcentage of the earths crust do the 12 most abundant elements make?

(99.23% of crust)

Silicates

Minerals that contain silicate anion (Si0,), they are also the most abundant group

Silicate Tetrahedron

Four oxygen atoms (large) surrounding silicon atom (small);
oxygen atoms must: (1) bond with other cations and/or
(2) bond with two silicon atoms at one time

Polymerization

Process of linking silicate tetrahedra

What are the common minerals?

Olivine group, Garnet group, Pyroxene group, Amphibole group, Micas, Quartz, Feldspar group, Carbonates, Phosphates, and Sulfates

What are the Ore Mineral Groups?

Sulfides and oxides

Olivine group

Isolated silicate tetrahedra; (Mg,Fe),SiO,; distinctive green color

Garnet group

Isolated tetrahedra; A3B,(SiO4),, A=Mg,~e,',ca,Mn, & B=AI,F~,',C~

Pyroxene group

Single chains of tetrahedra; AB(SiO,),; augite most common

Amphibole group

Double chains; A,B,(Si,O,,),(OH),; hornblende most common

Micas (clays, chlorites & serpentines)

Sheets; (Si401,)4-; muscovite & biotite (micas)

Quartz

1 5% of crust; SiO,; chalcedony (cryptocrystalline) precipitated from water

Feldspar group

60% of crust; AI(l,,Si(3.2,0,; K-feldspar & plagioclase (Na & Ca)

Carbonates

Calcite, aragonite, dolomite

Phosphates

Apatite

Sulfates

Gypsum, anhydrite

Sulfides

Pyrite, galena, sphalerite, chalcopyrite (ore minerals)

Oxides

Magnetite, hematite (ore minerals)

What are the types of rocks?

Igneous, Metamorphic, and Sedimentary

Igneous Rocks

Form from cooling and solidification of magma

Sedimentary

Form from consolidation of sediment (Made from any other rocks)

Metamorphic

Original form has been altered by high To and/or P

What is the Rock Cycle?

Exposed rocks are transformed into sediment; sediment is buried
and compacted, becoming sedimentary rock; deeper burial turns it
into metamorphic rock, and even deeper burial may cause rock to
melt, forming magma from which igneous rock will form.
Uplift=

What is rock texture?

size, shape and arrangement of mineral grains

mineral assemblage

varieties and abundances of minerals present

What are the 2 types of igneous rocks?

Extrusive, and Intrusive

Extrusive (volcanic)

Formed by solidification of lava and/or tephra on earth's surface. Formed on the Earth surface.

Intrusive (plutonic)

Formed by solidification of magma within earth's crust.

Texture

Size and packing of mineral grains (Both intrusive and extrusive have the same type of ingredients but have different texture)

What are the sizes of rocks?

Intrusive, Phanerite, Pegmatite, Aphanite, Pophyry, and Glassy

lntrusive

Coarse grained (slow cooling)

Phanerite

Coarse grained (>2mm) (intrusive)

Pegmatite

Unusually large mineral grains (>2cm)

Aphanite

Fine grained (<2mm) (extrusive)

Pophyry

Coarse grains (phenocrysts) in a fine-grained groundmass,

Glassy

Cools so quickly that atoms aren't able to organize into minerals.

What is an example of glassy rock?

Obsidian

Mineral Assemblage

Along with texture, determines names of igneous rocks.

What are 3 intrusive igneous rocks?

Granite, Diorite and Gabbro

Granite

Contains quarts, potasiumfeldspare, sodium, micas, amphibole and is the most common intusive rock

Diorite

Intusive rock does not contain quarts and is a lot less common than granite

Gabbro

Very rare Intrusive rock

3 extrusive igneous rock

Rhyolite, Andesite, Basalt

Rhyolite

Aphanitic equivalent of granite; pale; quartz & feldspar phenocrysts; rare. High in silica

Andesite

Aphanitic equivalent of diorite; darker; plagioclase & amphibole/pyroxene phenocrysts; more common. Named after the Andes mountain range.

Basalt

Aphanitic equivalent of gabbro; dark gray or black; plagioclase & pyroxenelolivine phenocrysts; most common. No Quarts usually olivine.

Pyroclast

Fragment of rock ejected during volcanic eruption

Pyro

fire

Clast

many bits

Pyroclastic rocks

Formed from pyroclasts

Tephra

Deposit of pyroclasts; includes bombs (>64mm), lapilli (2-64mm), and ash (<2mm). Based on size.
bombs =>lapilli =>ash

Ash

A powdered volcanic glass.

Agglomerate

Coarse (bomb-sized) tephra particles

Tuff

Fine (lapilli- to ash-sized) tephra particles

Welded tuff

Glassy; produced when individual hot ash particles fuse. Glassy shards of ask weld together. Pompeii

Plutons

All bodies of intrusive igneous rock, regardless of size or shape.

What are the minor plutons?

Dike, Sills, Laccolith, and Volcanic pipe

Dike

Tabular, sheet-like body that cuts across layering of rock it intrudes

What is an example of a dike?

The Black Dike on Mount Morand in the grand Tetons.

Sills

Tabular, sheet-like bodies that are parallel to layering of rock they intrude

Laccolith

Parallel to layering of rock, but has bent layers above it into a dome

What is an example of a Laccolith

The Hennery Moutains

Volcanic pipe

Cylindrical conduit that fed magma to vent; if erosion strips away surrounding rock, rock that filled pipe is a volcanic neck

What is an example of a volcanic neck? and how was it formed?

Ship rock in new Mexico is a volcanic neck (formed by the volcano eroding away but leaving the volcanic pipe)

What are the Major Plutons?

Batholith, Stoping, Xenolith, and Stock

Batholith

Large, irregularly-shaped pluton that cuts across layering of rock and are the largest intrusive bodies. They are formed when large magma chambers move to the surface.

What is an example of a Batholith?

The Idaho Batholiths in Yosemite national park.

Stoping

Rising magma body dislodges fragments of overlying rock. When country rock falls into the batholith as it moves to the surface.

Xenolith

Stoped fragment enclosed in magmatic body when it solidifies. It is the result of Stoping.

Stock

Irregularly-shaped plutons, like batholiths, but smaller

What is an example of a stock?

Big Cottonwood Canyon

Magmatic Differentiation by Fractional Crystallization

Compositional changes caused by sinking of early crystallized minerals to bottom of magma chamber (Isn't how it usually work)

Bowen's Reaction Series

Sequence in which minerals crystallize from cooling magma; minerals with highest melting points crystallize first.

Continuous Reaction Series

Makes Ca-rich plagioclase then when it runs out of Ca it starts using Na and making Na-rich plagioclase.

Discontinuous reaction series

Olivine -> Pyroxene -> Amphibole -> Biotite

Late stage

K-spar (and/or muscovite if water pressure is high); excess SiO2, will crystallize as quartz (not a reaction series.

Magma

Molten rock, together with any suspended mineral grains and dissolved gases, that forms by melting of rock in crust and mantle.

Volcano

Vent from which magma, solid rock debris, and gases are erupted

Lava

Magma that reaches earth's surface

What is a predominant ingredient in Magma?

SiO, always predominant; characterized by high To; has ability to flow

What is the most common gas in Magma?

Water

What is the composition of Basaltic Magma?

-50% SiO

What is the composition of Andesitic Magma? ;

-60% SiO

What is the composition of Rhyolitic Magma?

-70%

Viscosity

a liquid's resistance to flow.

What does the viscosity depend on?

It Depends on temperature and composition.

Pahoehoe

Smooth, ropy-surfaced lava formed from very hot, fluid lava

Aa

Rubbly, rough-looking lava formed from cooler, very viscous lava

Eruption of Magma

Lower density causes magma to slowly rise; as pressure decreases, gas comes out of solution (exsolves)

Nonexplosive Eruption

Low-viscosity (basaltic) magma and low dissolved-gas content

What are the nonexplosive eruptions of a volcano?

lava fountain, spatter cone, lava tube, vesicles, amygdules

Lava fountain Eruption

Forms when basaltic magma rises so rapidly that gas bubbles from solution

Spatter cone

Forms when bits of falling lava pile up beside vent

Lava tube

Subsurface channels in pahoehoe lava flows

Vesicles

Gas bubble holes preserved in solidified rock; produces rock w/vesicular texture

Amygdules

Vesicles filled by secondary minerals

Explosive

Viscous (andesimtic/rhyoliticm)magma with high dissolved-gas content

What are examples of Explosive Eruptions?

Pumice, Ash, Eruption column, Tephra fall, Pyroclastic, lgnimbrite, and lateral blast

Pumice

Froth of innumerable, glass-walled bubbles

Ash

Tiny fragments of shattered, solidified magma

Eruption column

Mixture of hot gas and tephra rising rapidly into air

Tephra fall

Rain of debris particles as eruption cloud drifts w/upper winds

Pyroclastic flow

Denser-than-air mixture of hot gas & ash; fast & lethal

ignimbrite

Solidified deposit resulting from pyroclastic flow

Lateral blast

Sideways eruption

What are the three types of volcanos?

Shield volcanoes, Tephra cones (cinder cones), Stratovolcanoes (composite cones)

Shield volcanoes

Built up of very fluid (basaltic) lava flows; broad, dome-shaped; gentle slopes

Tephra cones (cinder cones)

Formed from pyroclastic debris around a vent; magma is gasrich; slopes typically about 30" (angle of repose)

Stratovolcanoes (composite cones)

Emit both tephra and lava; build up steep, conical mounds; much larger than tephra cones

Crater

Depressions near summit from which volcanic materials are ejected

Lava domes

Late-stage, very viscous lava extruded after most gas exsolved

Calderas

Circular, steep-walled basins >kIm in diameter near summit

Resurgent domes

Due to uplift of caldera; also small tephra conesllava flows

Diatremes

Volcanic pipes filled w/ rubble of broken rock