Lecture8 rocks

28
Rocks

Transcript of Lecture8 rocks

Page 1: Lecture8 rocks

Rocks

Page 2: Lecture8 rocks

3 types of rocks

• igneous

• sedimentary

• metamorphic

Page 3: Lecture8 rocks

1. Igneous rocks (fire-formed)= rock that solidified from a molten state

• majority of crustal rock (although it is often covered with sedimentary rocks)

• consists of silicate minerals w/ metallic elements

• “interlocking grains”

e.g. granite, basalt, obsidian, pumice

Magma: molten rock beneath Earth’s surface

Page 4: Lecture8 rocks

GraniteBasalt

ObsidianPumice

Page 5: Lecture8 rocks

Composition of igneous rocks

Felsic Mafic

Elements Si & Al Fe & Mg

Melting pt low temp. high temp.

Density low (light) high (heavy)

Color light dark

e.g. granite, diorite basalt, gabbro

Page 6: Lecture8 rocks

Global Composition Distribution

Continents- Felsic

Oceans- Mafic

Digital Elevation Model (DEM)

Page 7: Lecture8 rocks

Cooling and crystals

Slow cooling = bigger crystals

Fast cooling = smaller crystals

So, the cooling history of an igneous rock determines how big its crystals will be

Page 8: Lecture8 rocks

Intrusive“Plutonic”

• cools slowly under the surface

• large crystals

• e.g. granite

Extrusive“Volcanic”

• cools quickly above the surface

• small crystals

• e.g. basalt

Page 9: Lecture8 rocks

Felsic Intermediate Mafic

Intr

usiv

eE

xtru

sive

Rhyolite

Classifying igneous rocks

Andesite Basalt

Granite Diorite Gabbro

Page 10: Lecture8 rocks

RhyoliteRhyolite

AndesiteAndesite

BasaltBasalt

GraniteGranite

DioriteDiorite

GabbroGabbro

YellowstoneYellowstone

Sierra NevadaSierra Nevada

AndesAndes

Ocean basementOcean basement

HawaiiHawaii

New ZealandNew Zealand

Page 11: Lecture8 rocks

Intrusive features

batholith dike(vertical)

sill(horizontal)

Pluton: body of intrusive rock

Page 12: Lecture8 rocks

Famous extrusive rocks

Page 13: Lecture8 rocks

Famous intrusive rocks

Page 14: Lecture8 rocks

2. Sedimentary rocks= formed through erosion, transportation,

deposition, compaction, cementation, and hardening of sediment

Sediment = fine-grained mineral matter transported by air, water or ice

• accumulates at low elevations to form strata (rock layers)

Page 15: Lecture8 rocks

Sedimentary rocks

• majority of surface rock• often fossiliferous• e.g. sandstone, shale, limestone, coal

Page 16: Lecture8 rocks

Classifying sedimentary rocks1. Clastic2. Chemical3. Organic

Page 17: Lecture8 rocks

Classifying sedimentary rocks1. Clastic

- derived from weathered & fragmented rock

- boulder microscopic grain sizes- e.g. mudstone, shale, sandstone

Sandstone Shale

Page 18: Lecture8 rocks

Classifying sedimentary rocks2. Chemical

- dissolved minerals - transported in solution & precipitated- e.g. limestone, evaporites

Limestone

Halite

Page 19: Lecture8 rocks
Page 20: Lecture8 rocks

Classifying sedimentary rocks3. Organic

- remains of dead organisms- e.g. coal

CoquinaCoal

Page 21: Lecture8 rocks

Famous sedimentary rocks

Page 22: Lecture8 rocks

3. Metamorphic rocks (change form)

• rocks changed by heat &/or pressure

• changes structure, appearance , composition, & texture of parent rock WITHOUT MELTING IT

• commonly at roots of mountains

e.g. slate, schist, gneiss

Page 23: Lecture8 rocks

Metamorphic processes

Page 24: Lecture8 rocks

3. Metamorphic rocks

limestone marble

sandstone quartzite

granite gneiss

shale slate schist

Page 25: Lecture8 rocks

Somewhat famous metamorphic rocks

Page 26: Lecture8 rocks

Rock Identification• Break into groups of 4, 5, or 6• Have one person come up and get a set of 3

rocks.• Use the flow chart on the following slide to

identify your rocks.• Determine the type of each rock (igneous,

sedimentary, or metamorphic).• Write your names, rock ID #’s, rock names, and

rock types on a sheet of paper to hand in.

Page 27: Lecture8 rocks

Granite BasaltSandstone ShaleLimestoneGneissSchist

Can you see the mineral grains?

Are the grains interlocking, or cemented together?

Are there layers or stripes(foliation) to the grains? yes no

interlocking cemented

yes no

Is the rock “scaly” or “glittery”?

yes no

Is it very dark colored (mafic)?

yesno

Definitive test: Does it react to a weak acid by “fizzing”?

Ok substitute test for today: is it layered in flat sheets?

noyes

yes no

Double check: is it layered in flat sheets?

noyes

IncludeRock #Rock NameRock Type

Page 28: Lecture8 rocks

Answer key

Granite

Basalt

SandstoneShale

Limestone

Gneiss

Schist 2

1

3

5

4

6

7