Geology For Dummies

Geology For Dummies
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Get a rock-solid grasp on geology Geology For Dummies is ideal reading for anyonewith an interest in the fundamental concepts of geology, whether they're lifelong learners with a fascination for the subject or college students interested in pursuing geology or earth sciences. Presented in a straightforward, trusted format—and tracking to a typical introductory geology course at the college level—this book features a thorough introduction to the study of earth, its materials, and its processes. Rock records and geologic time Large-scale motion of tectonic plates Matter, minerals, and rocks The geological processes on earth's surface Rock that geology class with Geology For Dummies !

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Alecia M. Spooner. Geology For Dummies

Geology For Dummies® To view this book's Cheat Sheet, simply go to www.dummies.com and search for “Geology For Dummies Cheat Sheet” in the Search box. Table of Contents

List of Tables

List of Illustrations

Guide

Pages

Introduction

About This Book

Foolish Assumptions

Icons Used in This Book

Beyond the Book

Where to Go from Here

Studying the Earth

Rocks for Jocks (and Everybody Else)

Finding Your Inner Scientist

Making observations every day

Jumping to conclusions

Focusing on Rock Formation and Transformation

Understanding how rocks form

Tumbling through the rock cycle

Mapping Continental Movements

Unifying geology with plate tectonics theory

Debating a mechanism for plate movements

Moving Rocks around on Earth’s Surface

Interpreting a Long History of Life on Earth

Using relative versus absolute dating

Witnessing evolution in the fossil record

Observing Earth through a Scientific Lens

Realizing That Science Is Not Just for Scientists

Using a Methodical Approach: The Scientific Method

Sensing something new

I have a hypothesis!

Testing your hypothesis: Experiments

Crunching the numbers

Interpreting results

Sharing the findings

Building New Knowledge: A Scientific Theory

It’s never “just a theory”

Scientific theory versus scientific law

The road to paradigms

Speaking in Tongues: Why Geologists Seem to Speak a Separate Language

Lamination vs. foliation: Similar outcomes from different processes

Gabbro vs. basalt: Different outcomes from similar processes

From Here to Eternity: The Past, Present, and Future of Geologic Thought

Catastrophe Strikes Again and Again

Early Thoughts on the Origin of Rocks

Developing Modern Geologic Understanding

Reading the rock layers: Steno’s stratigraphy

These things take time! Hutton’s hypothesis

FINDING SHARKS’ TEETH ON MOUNTAINTOPS

What has been will be: Lyell’s principles

Uniformi-what? Understanding the Earth through Uniformitarianism

Pulling It All Together: The Theory of Plate Tectonics

Forging Ahead into New Frontiers

Asking how, where, and why: Mountain building and plate boundaries

Mysteries of the past: Snowball earth, first life, and mass extinctions

Snowball earth

Earliest life

Mass extinctions

Predicting the future: Earthquakes and climate change

Earthquake warnings

Climate change

Out of this world: Planetary geology and the search for life

Home Sweet Home: Planet Earth

Earth’s Spheres

Examining Earth’s Geosphere

Defining Earth’s layers

Examining each layer

Heavy metal: The earth’s core

Flowing and solid: The earth’s mantle

It’s only skin deep: The earth’s crust

DRILLING FOR THE MOHO

Elements, Minerals, and Rocks

It’s Elemental, My Dear: A Very Basic Chemistry of Elements and Compounds

The Smallest Matter: Atoms and Atomic Structure

Getting to know the periodic table

Interpreting isotopes

Charging particles: Ions

Chemically Bonding

Donating electrons (ionic bonds)

Sharing electrons (covalent bonds)

Migrating electrons (metallic bonds)

Formulating Compounds

Minerals: The Building Blocks of Rocks

Meeting Mineral Requirements

Making Crystals

Identifying Minerals Using Physical Characteristics

Observing transparency, color, luster, and streak

Measuring mineral strength

Hardness

Tenacity

Cleavage and fracture

CONCHOIDAL FRACTURES AND STONE AGE TOOLS

If it tastes like salt, it must be halite: Noting unique mineral properties

Measuring properties in the lab

Realizing Most Rocks Are Built from Silicate Minerals

Finding silicates in many shapes

Grouping silicate minerals

Remembering the Nonsilicate Minerals

Carbonates

Sulfides and sulfates

Oxides

Native elements

Evaporites

Gemstones

DIAMONDS

Recognizing Rocks: Igneous, Sedimentary, and Metamorphic Types

Mama Magma: Birthing Igneous Rocks

Remembering how magma is made

Classifying melt composition

Reacting in sequence: Bowen’s reaction series

Evolving magmas

Crystallizing one way or another: Igneous rocks

Classifying igneous rocks

Counting silicate minerals in igneous rocks

Observing textures of igneous rocks

A BASALT BY ANY OTHER NAME: PAHOEHOE AND A’A

Studying volcanic structures

Spotting volcanic features

Distinguishing three types of volcanoes

SHIELD VOLCANOES

STRATOVOLCANOES

CINDER CONES

Looking below the surface

Merging Many Single Grains of Sand: Sedimentary Rocks

DIGGING IN THE DIRT: SOILS

Weathering rocks into sediments

Chipping away: Mechanical weathering

Reacting with water and air: Chemical weathering

Changing from sediment into rock

Sizing up the grains: Classifying sedimentary rocks

Detrital sedimentary rocks

No grains at all: Chemical sedimentary rocks

Searching for sedimentary basins

Telling stories of the past: Sedimentary structures

Stuck between a Rock and a Hard Place: Metamorphic Rocks

Turning up the heat and pressure: Metamorphism

Grading metamorphism with index minerals

Between the mineral sheets: Foliation, or maybe not

Categorizing metamorphic rocks

Transforming sedimentary rocks

Transforming igneous rocks

Creating hornfels

Tumbling through the Rock Cycle: How Rocks Change from One Type to Another

One Theory to Explain It All: Plate Tectonics

Adding Up the Evidence for Plate Tectonics

Drifting Apart: Wegener’s Idea of Continental Drift

Continental puzzle solving

Fossil matching

Stratigraphic stories

Icy cold climates of long ago

Meeting at the equator

Searching for a mechanism

Coming Together: How Technology Sheds Light on Plate Tectonics

Mapping the seafloor

IMAGING THE SEAFLOOR: MARIE THARP AND SEAFLOOR MAPPING

Flip-flopping magnetic poles: Paleomagnetism and seafloor spreading

SHARKS AND THE EARTH’S MAGNETISM

Measuring plate movements

Unifying the theory

When Crustal Plates Meet, It’s All Relative

Density Is Key

Two of a Kind: Continental and Oceanic Crust

Dark and dense: Oceanic crust

Thick and fluffy: Continental crust

Understanding Why Density Matters: Isostasy

Defining Plate Boundaries by Their Relative Motion

Driving apart: Divergent plate boundaries

Ripping open the ocean floor

Parting the Red Sea

Crashing together: Convergent plate boundaries

One goes up and one must go down

Diving into the abyss

Reaching for the sky

Slip-sliding along: Transform plate boundaries

Shaping Topography with Plate Movements

Deforming the crust at plate boundaries

Compressing rocks into folds

Faulting in response to stress

Dipping and slipping

Striking and slipping

Joints

Building mountains

Volcanoes and accretion

Stretching and thinning

Crushing and lifting

Who’s Driving This Thing? Mantle Convection and Plate Movement

Running in Circles: Models of Mantle Convection

Mantle plumes: Just like the lava in your lamp

The slab-pull and ridge-push models

Using Convection to Explain Magma, Volcanoes, and Underwater Mountains

Plate friction: Melting rock beneath the earth’s crust

Creating volcanic arcs and hotspots

Volcanic arcs

Volcanic hot spots

Remembering the ridges

Birthing new seafloor at mid-ocean ridges

Shake, Rattle, and Roll: How Plate Movements Cause Earthquakes

Responding elastically

OBSERVING EARTH’S INTERIOR BY PROXY

Sending waves through the earth

Measuring magnitude

Superficially Speaking: About Surface Processes

Gravity Takes Its Toll: Mass Wasting

Holding Steady or Falling Down: Friction versus Gravity

Focusing on the Materials Involved

Loose materials: Resting at the angle of repose

Bedrock: Losing its stability

Triggering Mass Movements

Adding water to the mix

Changing the slope angle

Shaking things up: Earthquakes

Removing vegetation

Moving Massive Amounts of Earth, Quickly

Falls

Slides and slumps

Flows

A More Subtle Approach: Creep and Soil Flow (Solifluction)

Water: Above and Below Ground

Hydrologic Cycling

Driving the cycle with evaporation

Traveling across a continent

Streams: Moving Sediments toward the Ocean

Draining the basin

Two types of flow

Measuring stream characteristics

Gradient

Velocity

Discharge

Carrying a heavy load

Suspended load

Bed load

Dissolved load

Measuring what is transported

Eroding a Stream Channel to Base Level

Seeking Equilibrium after Changes in Base Level

Leaving Their Mark: How Streams Create Landforms

Draining the basin

Meandering along

Braided streams

Meandering streams

Straight stream channels

Depositing sediments along the way

Reaching the sea

Flowing beneath Your Feet: Groundwater

Infiltrating tiny spaces underground

Measuring porosity and permeability

Setting the water table

Springing from rocks

Confining an aquifer

Heating up underground: Geysers

That sinking feeling: Karst, caves, and sinkholes

Drip, drip, dripping: The formation of dripstones

Sinkholes and disappearing streams

Flowing Slowly toward the Sea: Glaciers

Identifying Three Types of Glaciers

Understanding Ice as a Geologic Force

Transforming snow into ice

Balancing the glacial budget

Flowing solidly down the mountain

Eroding at a Snail’s Pace: Landforms Created by Glacial Erosion

Plucking and abrading along the way

Creating their own valleys

Speaking French: Cirques, arêtes, et roche moutonnées

Alpine glacial erosion

Ice sheet glacial erosion

FRENCH LESSONS

Leaving It All Behind: Glacial Deposits

Depositing the till

Moraines

Drumlins

Plains, trains, eskers, and kames

Outwash plains

Eskers and kames

Behaving erratically: Large boulders in odd places

Where Have All the Glaciers Gone?

Filling the erosional gaps

Cycling through ice ages

Moving to colder regions

Orbiting, spinning, and tilting around the sun

Rebounding isostatically

Blowing in the Wind: Moving Sediments without Water

Lacking Water: Arid Regions of the Earth

Transporting Particles by Air

Skipping right along: Bed load and saltation

Suspending particles in air

Deflating and Abrading: Features of Wind Erosion

Removing sediments

Scratching the surface

Just Add Wind: Dunes and Other Depositional Wind Features

Migrating piles of sand: Dunes

Shaping sand

Barchan dunes

Parabolic dunes

Transverse dunes

Longitudinal dunes

Star dunes

Laying down layers of loess

LIKE DUST IN THE WIND: THE ECOLOGICAL THREAT OF DESERTIFICATION

Paving the Desert: Deposition or Erosion?

Catch a Wave: The Evolution of Shorelines

Breaking Free: Waves and Wave Motion

Dissecting wave anatomy

Starting to roll

Going with the flow: Currents and tides

Shaping Shorelines

Carving cliffs and other features

Budgeting to build sandbars

Categorizing Coastlines

HEADING FOR HIGHER GROUND: TSUNAMIS

Long, Long Ago in This Galaxy Right Here

Getting a Grip on Geologic Time

The Layer Cake of Time: Stratigraphy and Relative Dating

Speaking relatively

Sorting out the strata

Putting rock layers in the right order

Losing time in the layers

Show Me the Numbers: Methods of Absolute Dating

Measuring radioactive decay

Three ways to decay

It takes a half-life: Transforming parent isotopes to daughter isotopes

Common radioactive isotopes for geological dating

Other exacting methods of geological dating

Fission-track dating

EXPOSING COSMIC RADIATION

COUNTING TREE RINGS

Radiocarbon

Relatively Absolute: Combining Methods for the Best Results

Eons, Eras, and Epochs (Oh My!): Structuring the Geologic Timescale

A Record of Life in the Rocks

Explaining Change, Not Origins: The Theory of Evolution

The Evolution of a Theory

Acquiring traits doesn’t do it

Naturally, selecting for survival

Mendel’s peas please

Genetic nuts and bolts

Spontaneously mutating genes

Speciating right and left

Putting Evolution to the Test

Against All Odds: The Fossilization of Lifeforms

Bones, teeth, and shell: Body fossils

Just passing through: Trace fossils

Correcting for Bias in the Fossil Record

Hypothesizing Relationships: Cladistics

Time before Time Began: The Precambrian

In the Beginning … Earth’s Creation from a Nebulous Cloud

Addressing Archean Rocks

Creating continents

Revving up the rock cycle

Granite- gneiss complexes

Greenstone belts

Piecing observations together

Feeling hot, hot, hot: Evidence for extreme temperatures

Originating with Orogens: Supercontinents of the Proterozoic Eon

Single Cells, Algal Mats, and the Early Atmosphere

Hunting early prokaryotes and eukaryotes

You know it as pond scum: Cyanobacteria

THE COMPLEXITY OF CLASSIFICATION

Waiting to inhale: The formation of Earth’s atmosphere

GOING TO EXTREMES

SNOWBALL EARTH

Questioning the Earliest Complex Life: The Ediacaran Fauna

Teeming with Life: The Paleozoic Era

Exploding with Life: The Cambrian Period

Toughen up! Developing shells

Ruling arthropods of the seafloor: Trilobites

BURGESS SHALE

Building Reefs All Over the Place

Swimming freely: Ammonoids and nautiloids

Exploring freshwater: Eurypterids

Spinal Tapping: Animals with Backbones

Fish evolve body armor, teeth, and … legs?

Placoderms

Cartilaginous fish

Bony fish

Venturing onto land: Early amphibians

Adapting to life on land: The reptiles

Planting Roots: Early Plant Evolution

Tracking the Geologic Events of the Paleozoic

Constructing continents

Reading the rocks: Transgressions and regressions

Fossilizing carbon fuels

Pangaea, the most super of supercontinents

Mesozoic World: When Dinosaurs Dominated

Driving Pangaea Apart at the Seams

One continent becomes many

Influencing global climate

Creating the mountains of North America

Repopulating the Seas after Extinction

The Symbiosis of Flowers

EVOLVING TOGETHER: FLOWERS AND INSECTS

Recognizing All the Mesozoic Reptiles

Swimming in ancient seas

Taking to the skies: Pterosaurs

Flocking together

Climbing the Dinosaur Family Tree

Branching out: Ornithischia and Saurischia

WARMING THEMSELVES FROM WITHIN: WERE DINOSAURS WARM-BLOODED?

Horned faces and armor: Ornithischian dinosaurs

Long necks and meat eaters: Saurischian dinosaurs

Flocking Together: The Evolutionary Road to Birds

Laying the Groundwork for Later Dominance: Early Mammal Evolution

The Cenozoic Era: Mammals Take Over

Putting Continents in Their Proper (Okay, Current) Places

Creating modern geography

The Alpine-Himalayan belt

The Circum-Pacific belt

Consuming the Farallon Plate

Carving the Grand Canyon with uplift

Icing over northern continents

Entering the Age of Mammals

CAUSING GLOBAL COOLING

Regulating body temperature

Filling every niche

Living Large: Massive Mammals Then and Now

Nosing around elephant evolution

Returning to the sea: Whales

Larger than life: Giant mammals of the ice ages

Right Here, Right Now: The Reign of Homo Sapiens

SEEKING ANSWERS TO MYSTERIES OF THE PAST

Arguing for the Anthropocene

Altering the climate

Shaping the landscape

Damming rivers

Shaping waterways

Nourishing beaches

Changing coastlines

Removing mountaintops

Leaving evidence in the rock record

And Then There Were None: Major Extinction Events in Earth’s History

Explaining Extinctions

Heads up! Astronomical impacts

Lava, lava everywhere: Volcanic eruptions and flood basalts

LIVING FOSSILS

Shifting sea levels

Changing climate

End Times, at Least Five Times

Cooling tropical waters

Reducing carbon dioxide levels

The Great Dying

Paving the way for dinosaurs

Demolishing dinosaurs: The K/T boundary

Modern Extinctions and Biodiversity

Hunting the megafauna

Reducing biodiversity

The Part of Tens

Ten Ways You Use Geologic Resources Every Day

Burning Fossil Fuels

Playing with Plastics

Gathering Gemstones

Drinking Water

Creating Concrete

Paving Roads

Accessing Geothermal Heat

Fertilizing with Phosphate

Constructing Computers

Building with Beautiful Stone

Ten Geologic Hazards

Changing Course: River Flooding

Caving In: Sinkholes

Sliding Down: Landslides

Shaking Things Up: Earthquakes

Washing Away Coastal Towns: Tsunamis

Destroying Farmland and Coastal Bluffs: Erosion

Fiery Explosions of Molten Rock: Volcanic Eruptions

Melting Ice with Fire: Jokulhlaups

Flowing Rivers of Mud: Lahars

Watching the Poles: Geomagnetism

Index. A

B

C

D

E

F

G

H

I

J

K

L

M

N

O

P

Q

R

S

T

U

V

W

X

Z

About the Author

Author’s Acknowledgments

Dedication

WILEY END USER LICENSE AGREEMENT

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Geology is the study of the earth. By default this means that geology is a vast, complex, and intricate topic. But “vast, intricate, and complex” does not necessarily mean difficult. Many folks interested in geology just don’t know where to start. Minerals? Rocks? Glaciers? Volcanoes? Fossils? Earthquakes? The sheer number of topics covered under the heading “geology” can be overwhelming.

Enter Geology For Dummies! The goal of this book is to break through the overwhelming array of geology information and provide a quick reference for key concepts in the study of the earth.

.....

One of the advantages of studying geology is being able to learn what mysteries of the past are hidden in the rocks. Sedimentary rocks, formed layer by layer over long periods of time, tell the story of Earth’s living history: changing climates and environments, as well as the evolution of life from single cells to modern complexity.

Scientists use two approaches to determine the age of rocks and rock layers: relative dating and absolute dating.

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