Solutions for Essentials of Geology, Books a la Carte Plus Mastering Geology with Pearson eText -- Access Card Package (13th Edition)
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Chapter 1 - An Introduction To GeologyChapter 1.1 - Geology: The Science Of EarthChapter 1.2 - The Development Of GeologyChapter 1.3 - The Nature Of Scientific InquiryChapter 1.4 - Earth As A SystemChapter 1.5 - Origin And Early Evolution Of EarthChapter 1.6 - Earth’s Internal StructureChapter 1.7 - Rocks And The Rock CycleChapter 1.8 - The Face Of EarthChapter 2 - Plate Tectonics: A Scientific Revolution Unfolds
Chapter 2.1 - From Continental Drift To Plate TectonicsChapter 2.2 - Continental Drift: An Idea Before Its TimeChapter 2.3 - The Theory Of Plate TectonicsChapter 2.4 - Divergent Plate Boundaries And Seafloor SpreadingChapter 2.5 - Convergent Plate Boundaries And SubductionChapter 2.6 - Transform Plate BoundariesChapter 2.7 - How Do Plates And Plate Boundaries Change?Chapter 2.8 - Testing The Plate Tectonics ModelChapter 2.9 - How Is Plate Motion Measured?Chapter 2.10 - What Drives Plate Motions?Chapter 3 - Matter And MineralsChapter 3.1 - Minerals: Building Blocks Of RocksChapter 3.2 - Atoms: Building Blocks Of MineralsChapter 3.3 - Why Atoms BondChapter 3.4 - Properties Of MineralsChapter 3.5 - Mineral GroupsChapter 3.6 - The SilicatesChapter 3.7 - Common Silicate MineralsChapter 3.8 - Important Nonsilicate MineralsChapter 3.9 - Minerals: A Nonrenewable ResourceChapter 4 - Magma, Igneous Rocks, And Intrusive ActivityChapter 4.1 - Magma: Parent Material Of Igneous RockChapter 4.2 - Igneous CompositionsChapter 4.3 - Igneous Textures: What Can They Tell Us?Chapter 4.4 - Naming Igneous RocksChapter 4.5 - Origin Of MagmaChapter 4.6 - How Magmas EvolveChapter 4.7 - Partial Melting And Magma CompositionChapter 4.8 - Intrusive Igneous ActivityChapter 4.9 - Mineral Resources & Igneous ProcessesChapter 5 - Volcanoes And Volcanic HazardsChapter 5.1 - Mount St. Helens Versus KilaueaChapter 5.2 - The Nature Of Volcanic EruptionsChapter 5.3 - Materials Extruded During An EruptionChapter 5.4 - Anatomy Of A VolcanoChapter 5.5 - Shield VolcanoesChapter 5.6 - Cinder ConesChapter 5.7 - Composite VolcanoesChapter 5.8 - Volcanic HazardsChapter 5.9 - Other Volcanic LandformsChapter 5.10 - Plate Tectonics And Volcanic ActivityChapter 6 - Weathering And SoilsChapter 6.1 - WeatheringChapter 6.2 - Mechanical WeatheringChapter 6.3 - Chemical WeatheringChapter 6.4 - Rates Of WeatheringChapter 6.5 - Soil: An Indispensable ResourceChapter 6.6 - Describing & Classifying SoilsChapter 6.7 - The Impact Of Human Activities On SoilChapter 6.8 - Weathering & Ore DepositsChapter 7 - Sedimentary RocksChapter 7.1 - An Introduction To Sedimentary RocksChapter 7.2 - Detrital Sedimentary RocksChapter 7.3 - Chemical Sedimentary RocksChapter 7.4 - Coal: An Organic Sedimentary RockChapter 7.5 - Turning Sediment Into Sedimentary Rock: Diagenesis And LithificationChapter 7.6 - Classification Of Sedimentary RocksChapter 7.7 - Sedimentary Rocks Represent Past EnvironmentsChapter 7.8 - Resources From Sedimentary RocksChapter 7.9 - The Carbon Cycle And Sedimentary RocksChapter 8 - Metamorphism And Metamorphic RocksChapter 8.1 - What Is Metamorphism?Chapter 8.2 - What Drives Metamorphism?Chapter 8.3 - Metamorphic TexturesChapter 8.4 - Common Metamorphic RocksChapter 8.5 - Metamorphic EnvironmentsChapter 8.6 - Metamorphic ZonesChapter 9 - Earthquakes & Earth’s InteriorChapter 9.1 - What Is An Earthquake?Chapter 9.2 - Seismology: The Study Of Earthquake WavesChapter 9.3 - Locating The Source Of An EarthquakeChapter 9.4 - Determining The Size Of An EarthquakeChapter 9.5 - Earthquake DestructionChapter 9.6 - Where Do Most Earthquakes Occur?Chapter 9.7 - Can Earthquakes Be Predicted?Chapter 9.8 - Earth’s InteriorChapter 10 - Origin And Evolution Of The Ocean FloorChapter 10.1 - An Emerging Picture Of The Ocean FloorChapter 10.2 - Continental MarginsChapter 10.3 - Features Of Deep-ocean BasinsChapter 10.4 - Anatomy Of The Oceanic RidgeChapter 10.5 - Oceanic Ridges And Seafloor SpreadingChapter 10.6 - The Nature Of Oceanic CrustChapter 10.7 - Continental Rifting: The Birth Of A New Ocean BasinChapter 10.8 - Destruction Of Oceanic LithosphereChapter 11 - Crustal Deformation & Mountain BuildingChapter 11.1 - Crustal DeformationChapter 11.2 - Folds: Rock Structures Formed By Ductile DeformationChapter 11.3 - Faults & Joints: Rock Structures Formed By Brittle DeformationChapter 11.4 - Mountain BuildingChapter 11.5 - Subduction & Mountain BuildingChapter 11.6 - Collisional Mountain BeltsChapter 11.7 - Vertical Motions Of The CrustChapter 12 - Mass Movement On Slopes: The Work Of GravityChapter 12.1 - The Importance Of Mass MovementChapter 12.2 - Controls & Triggers Of Mass MovementChapter 12.3 - Classification Of Mass Movement ProcessesChapter 12.4 - Common Forms Of Mass Movement: Rapid To SlowChapter 12.5 - Very Slow Mass MovementsChapter 13 - Running WaterChapter 13.1 - Earth As A System: The Hydrologic CycleChapter 13.2 - Running WaterChapter 13.3 - Streamflow CharacteristicsChapter 13.4 - The Work Of Running WaterChapter 13.5 - Stream ChannelsChapter 13.6 - Shaping Stream ValleysChapter 13.7 - Depositional LandformsChapter 13.8 - Floods And Flood ControlChapter 14 - GroundwaterChapter 14.1 - The Importance Of GroundwaterChapter 14.2 - Groundwater And The Water TableChapter 14.3 - Storage And Movement Of GroundwaterChapter 14.4 - Wells And Artesian SystemsChapter 14.5 - Springs, Hot Springs, And GeysersChapter 14.6 - Environmental ProblemsChapter 14.7 - The Geologic Work Of GroundwaterChapter 15 - Glaciers And GlaciationChapter 15.1 - Glaciers: A Part Of Two Basic CyclesChapter 15.2 - Formation & Movement Of Glacial IceChapter 15.3 - Glacial ErosionChapter 15.4 - Glacial DepositsChapter 15.5 - Other Effects Of Ice Age GlaciersChapter 15.6 - The Ice AgeChapter 16 - Deserts And WindChapter 16.1 - Distribution And Causes Of Dry LandsChapter 16.2 - Geologic Processes In Arid ClimatesChapter 16.3 - Basin And Range: The Evolution Of A Desert LandscapeChapter 16.4 - Wind ErosionChapter 16.5 - Wind DepositsChapter 17 - ShorelinesChapter 17.1 - The Shoreline & Ocean WavesChapter 17.2 - Beaches & Shoreline ProcessesChapter 17.3 - Shoreline FeaturesChapter 17.4 - Contrasting America’s CoastsChapter 17.5 - Hurricanes: The Ultimate Coastal HazardChapter 17.6 - Stabilizing The ShoreChapter 17.7 - TidesChapter 18 - Geologic TimeChapter 18.1 - Creating A Time Scale: Relative Dating PrinciplesChapter 18.2 - Fossils: Evidence Of Past LifeChapter 18.3 - Correlation Of Rock LayersChapter 18.4 - Numerical Dating With Nuclear DecayChapter 18.5 - Determining Numerical Dates For Sedimentary StrataChapter 18.6 - The Geologic Time ScaleChapter 19 - Earth’s Evolution Through Geologic TimeChapter 19.1 - Is Earth Unique?Chapter 19.2 - Birth Of A PlanetChapter 19.3 - Origin And Evolution Of The Atmosphere And OceansChapter 19.4 - Precambrian History: The Formation Of Earth’s ContinentsChapter 19.5 - Geologic History Of The Phanerozoic: The Formation Of Earth’s Modern ContinentsChapter 19.6 - Earth’s First LifeChapter 19.7 - Paleozoic Era: Life ExplodesChapter 19.8 - Mesozoic Era: Dinosaurs DominantChapter 19.9 - Cenozoic Era: Mammals DiversifyChapter 20 - Global Climate ChangeChapter 20.1 - Climate And GeologyChapter 20.2 - Detecting Climate ChangeChapter 20.3 - Some Atmospheric BasicsChapter 20.4 - Heating The AtmosphereChapter 20.5 - Natural Causes Of Climate ChangeChapter 20.6 - Human Impact On Global ClimateChapter 20.7 - Climate-feedback MechanismsChapter 20.8 - Some Consequences Of Global Warming
Book Details
With the renowned readability of the Lutgens/Tarbuck/Tasa team, the
Eleventh Edition of
Essentials of Geology continues to enhance both the approach and the visual presentation that has made this text a best-seller. This revision incorporates a new active learning approach throughout each chapter which offers the students a structured learning path and provides a reliable, consistent framework for mastering the chapter concepts. It also includes new additions to the visual program and current issues, such as climate change, are thoroughly updated.
Sample Solutions for this Textbook
We offer sample solutions for Essentials of Geology, Books a la Carte Plus Mastering Geology with Pearson eText -- Access Card Package (13th Edition) homework problems. See examples below:
Explanation: Given info: The length of recorded history for humankind is about 5000 years and the...Explanation: The theory of continental drift proposed by a German meteorologist and geophysicist in...Explanation: “A mineral is an inorganic, naturally occurring solid formed by geological processes,...Explanation: The rocks which are formed by the intrusive activity of magma are termed as intrusive...Explanation: The alternate layering of cinders and ash that are erupted, interbedded lava flows with...Explanation: Weathering may be defined as the “physical breakdown and chemical alteration of rocks...Explanation: A huge mass of igneous rock is exposed to the surface of the Earth as a result of...Explanation: The metamorphic rocks that are formed around igneous intrusions where the temperature...Explanation: The earthquakes occur due to the buildup of stresses; the stress acting on the walls of...
Given info: Depth of Challenger Deep = 10994 meters The equation for calculating water depth from...Explanation: Faults are the fractures with displacement. Faults are classified primarily into two...Explanation: The mass movement is the process of sudden transfer of large amount of materials...Explanation: Streams are channels of water that flow on the surface of the earth. Streams flow in...Explanation: Most of the areas in New Orleans, Louisiana is situated below the sea level or...The given information: The number of years taken for the movement is 8 years and the central...Explanation: The factors that control the dryness of an area are annual precipitation and the...Explanation: Ocean waves represent the energy waves that are travelling along the interface between...Explanation: “Principle of cross-cutting relationships states that the geological feature which cuts...Explanation: The 4.5 billion years of the Earth’s history is marked by two major eons, namely the...Explanation: Earth system is a complex combination of various spheres in the Earth. Even the minor...
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