Solutions for Applications and Investigations in Earth Science Plus Mastering Geology with eText -- Access Card Package (8th Edition)
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Chapter 1 - The Study Of MineralsChapter 1.1 - Minerals: Building Blocks Of RockChapter 1.2 - LusterChapter 1.3 - Color And StreakChapter 1.4 - Crystal Shape, Or HabitChapter 1.5 - HardnessChapter 1.6 - Cleavage And FractureChapter 1.7 - Specific GravityChapter 1.8 - Other Properties Of MineralsChapter 1.9 - Identification Of Minerals
Chapter 1.10 - Mineral GroupsChapter 2 - Rocks And The Rock CycleChapter 2.1 - Rock Groups And The Rock CycleChapter 2.2 - Igneous Rock TexturesChapter 2.3 - Composition Of Igneous RocksChapter 2.4 - Identifying Igneous RocksChapter 2.5 - Introduction To Sedimentary RocksChapter 2.6 - Identifying Sedimentary RocksChapter 2.7 - Sedimentary EnvironmentsChapter 3 - Aerial Photographs, Satellite Images, And Topographic MapsChapter 3.1 - Aerial PhotographsChapter 3.2 - Satellite ImagesChapter 3.3 - Topographic MapsChapter 3.4 - Map ScalesChapter 3.6 - Reading Contour LinesChapter 3.7 - Constructing A Contour MapChapter 3.8 - Drawing A Topographic ProfileChapter 3.9 - Analysis Of A Topogrraphic MapChapter 4 - Shaping Earth's Surface: Running Water And GroundwaterChapter 4.1 - Examining The Hydrologic CycleChapter 4.2 - Infiltration And RunoffChapter 4.3 - Infiltration And Runoff In Urban AreasChapter 4.4A - Running Water: Examining The Portage, Montana, Topographic MapChapter 4.4B - Running Water: Examining The Angelica, New York, Topographic MapChapter 4.4C - Running Water: Examining The Campti, Louisiana, Topographic MapChapter 4.5 - GroundwaterChapter 4.6 - Groundwater MovementChapter 4.7 - Ground SubsidenceChapter 4.8 - Karst TopographyChapter 5 - Shaping Earth's Surface: Arid And Glacial LandscapesChapter 5.1 - DesertsChapter 5.2 - Evolution Of A Mountainous Desert LandscapeChapter 5.3 - Glaciers And Ice SheetsChapter 5.4 - Depositional Features Of GlaciersChapter 5.5 - Features Of Continental Ice SheetsChapter 5.6A - Features Of Valley Or Alpine Glaciation: How Glaciation Affects Mountainous TopographyChapter 5.6B - Features Of Valley Or Alpine Glaciation: Alpine Glacial FeaturesChapter 5.6C - Features Of Valley Or Alpine Glaciation: Identifying Glacial Features On A Topographic MapChapter 6 - Earthquakes And Earth's InteriorChapter 6.1 - EarthquakesChapter 6.2A - Locating An Earthquake: Using A Travel-time GraphChapter 6.2B - Locating An Earthquake: Locating An EarthquakeChapter 6.3 - Global Distribution Of EarthquakesChapter 6.4 - The Earth Beyond Our ViewChapter 6.5 - Earth's Internal TemperatureChapter 6.6 - Melting Temperatures Of RocksChapter 7 - Plate TectonicsChapter 7.1 - From Continental Drift To Plate TectonicsChapter 7.2 - Plate BoundariesChapter 7.3A - Evidence: The Continental Jigsaw Puzzle: The Continental Jigsaw PuzzleChapter 7.3B - Evidence: The Continental Jigsaw Puzzle: Matching Rock TypesChapter 7.4 - Evidence: Deep-focus EarthquakesChapter 7.5 - Evidence: PaleomagnetismChapter 7.6A - Paleomagnetism And Seafloor Spreading: Paleomagnetism And Seafloor SpreadingChapter 7.6B - Paleomagnetism And Seafloor Spreading: Calculating The Rate Of Seafloor SpreadingChapter 7.6C - Paleomagnetism And Seafloor Spreading: Determining The Ages Of Ocean BasinsChapter 7.7 - Hot Spots And Plate VelocitiesChapter 8 - Geologic Maps, Block Diagrams, And Rock StructuresChapter 8.1 - DeformationChapter 8.2 - Describing The Orientation Of Geologic Structures: Strike And DipChapter 8.3 - Geologic Maps And Block DiagramsChapter 8.4A - Folds: Rock Structures Formed By Ductile Deformation: Examining FoldsChapter 8.4B - Folds: Rock Structures Formed By Ductile Deformation: Examining Domes And BasinsChapter 8.5 - Faults: Rock Structures Formed By Brittle DeformationChapter 8.6 - Examining Geologic MapsChapter 9 - Geologic TimeChapter 9.1 - Numerical And Relative DatesChapter 9.2 - Principle Of Original Horizontality And Principle Of SuperpositionChapter 9.3 - Principles Of Cross-cutting And Principle Of InclusionsChapter 9.4 - UnconformitiesChapter 9.5 - Applying Relative Dating TechniquesChapter 9.6 - FossilsChapter 9.7 - Fossils As Time IndicatorsChapter 9.8 - Radiometric DatingChapter 9.9 - Applying Multiple Dating TechniquesChapter 9.10 - The Magnitude Of Geologic TimeChapter 10 - Introduction To OceanographyChapter 10.1A - Extent Of The Oceans: Extent Of The OceansChapter 10.1B - Extent Of The Oceans: Distribution Of Land And WaterChapter 10.2 - Measuring Ocean DepthsChapter 10.3 - Ocean Basin TopographyChapter 10.4A - Salinity And Density Currents: Salinity-density ExperimentChapter 10.4B - Salinity And Density Currents: Comparing Water Salinity At Various LatitudesChapter 10.5A - Water Temperatures And Density Currents: Temperature-density ExperimentChapter 10.5B - Water Temperatures And Density Currents: Comparing The Temperature And Density Of SeawaterChapter 11 - Waves, Currents, And TidesChapter 11.1 - Waves CharacteristicsChapter 11.2 - Deep- Versus Shallow-water WavesChapter 11.3 - Wave RefractionChapter 11.4 - Longshore TransportChapter 11.5A - Shoreline Features: Identifying Shoreline FeaturesChapter 11.5B - Shoreline Features: Identifying Shoreline Features On A Topographic MapChapter 11.6 - Surface-ocean CurrentsChapter 11.7 - Deep-ocean CirculationChapter 11.8A - Tides: Spring And Neap TidesChapter 11.8B - Tides: Examining Basic Tidal PatternsChapter 11.8C - Tides: Examining Tidal Data For Long Beach, New YorkChapter 12 - Earth-sun RelationshipsChapter 12.1 - Solar Radiation And The SeasonsChapter 12.2 - Variations In Solar Energy Throughout The YearChapter 12.3 - Using An AnalemmaChapter 12.4 - Calculating The Noon Sun AngleChapter 12.5 - Using The Noon Sun Angle To Determine LatitudeChapter 12.6 - Solar Radiation At The Outer Edge Of The AtmosphereChapter 13 - Heating The AtmosphereChapter 13.1 - Radiation And The Electromagnetic SpectrumChapter 13.2 - What Happens To Incoming Solar Radiation?Chapter 13.3 - Heating Earth's Atmosphere: The Greenhouse EffectChapter 13.4A - Experiment: The Influence Of Color On AlbedoChapter 13.4B - Experiment: Differential Heating Of Land And WaterChapter 13.5 - Air Temperature DataChapter 13.6 - Global Temperature PatternsChapter 13.7 - WindchillChapter 14 - Atmospheric Moisture, Pressure, And WindChapter 14.1A - Changes Of State: Changes Of StateChapter 14.1B - Changes Of State: Latent Heat ExperimentChapter 14.2 - Humidity: Water Vapor In The AirChapter 14.3A - Relative Humidity: Calculating Relative HumidityChapter 14.3B - Relative Humidity: Relative Humidity Versus Water-vapor ContentChapter 14.4 - Dew-point TemperatureChapter 14.5 - Using A PsychrometerChapter 14.6 - Condensation And Dew-point TemperatureChapter 14.7 - Daily Temperature Changes And HumidityChapter 14.8 - Adiabatic Processes And Cloud FormationChapter 14.9 - Atmospheric PressureChapter 14.10 - The Driving Force Of Wind: The Pressure Gradient ForceChapter 14.11 - Factor Affecting Wind Direction: The Coriolis EffectChapter 14.12 - Global Patterns Of PrecipitationChapter 15 - Air Masses, Midlatitude Cyclones, And Weather MapsChapter 15.1 - Air MassesChapter 15.2 - FrontsChapter 15.3 - Midlatitude CyclonesChapter 15.4 - Weather Station Analysis And ForecastingChapter 15.5 - Preparing A Weather Map And ForecastChapter 16 - Global ClimatesChapter 16.1A - Controls Of Climate: Controls Of ClimateChapter 16.1B - Controls Of Climate: Global TemperaturesChapter 16.2 - Using A ClimographChapter 16.3 - The Nature Of ClassificationChapter 16.4 - Koppen System Of Climate ClassificationChapter 16.5 - Humid Tropical (a) ClimatesChapter 16.6 - Dry (b) ClimatesChapter 16.7 - Humid Middle-latitude (c) Climates (mild Winters)Chapter 16.8 - Humid Middle-latitude (d) Climates (severe Winters)Chapter 16.9 - Polar (e) ClimatesChapter 16.10 - Highland ClimatesChapter 16.11 - Climates Of North AmericaChapter 17 - Astronomical ObservationsChapter 17.1A - Measuring The Position Of The Sun: Sunset ObservationsChapter 17.1B - Measuring The Position Of The Sun: Measuring The Noon Sun AngleChapter 17.2 - Measuring The Position Of The MoonChapter 17.3 - Observing The StarsChapter 18 - Patterns In The Solar SystemChapter 18.1 - The Nebular TheoryChapter 18.2 - Comparing The Sizes Of The PlanetsChapter 18.3 - Inclinations Of Planetary OrbitsChapter 18.4A - Mass And Density Of Planets: Comparing Planetary MassesChapter 18.4B - Mass And Density Of Planets: Comparing The Number Of Moons To Planetary MassesChapter 18.4C - Mass And Density Of Planets: Comparing A Planet's Diameter To Its DensityChapter 18.5A - Rotation And Revolution Of The Planets: Rotation And Revolution Of The PlanetsChapter 18.5B - Rotation And Revolution Of The Planets: Kepler's Third Law Of Planetary MotionChapter 18.6 - Temperatures On Terrestrial PlanetsChapter 18.7 - Spacing Of The PlanetsChapter 19 - Locating The PlanetsChapter 19.1A - A Model Of The Inner Solar System: Locating A Planet Using The Reference CircleChapter 19.1B - A Model Of The Inner Solar System: Locating A Planet Among The ConstellationsChapter 19.2 - Comparing Rotational Periods Of The PlanetsChapter 19.3 - Retrograde MotionChapter 19.4 - Viewing A Planet From EarthChapter 20 - Examining The Terrestrial PlanetsChapter 20.1A - Geologic Processes: VolcanismChapter 20.1B - Geologic Processes: Tectonic ActivityChapter 20.1C - Geologic Processes: GradationChapter 20.1D - Geologic Processes: Impact CrateringChapter 20.2 - Landforms On The MoonChapter 20.3 - Landforms On MercuryChapter 20.4 - Landforms On VenusChapter 20.5 - Landforms On MarsChapter 20.6 - Determining The Relative Ages Of LandformsChapter 20.7 - Impact Cratering ExperimentChapter 21 - Motions Of The Earth-moon SystemChapter 21.1A - Phases Of The Moon: Phases Of The MoonChapter 21.1B - Phases Of The Moon: Observing The Phases Of The MoonChapter 21.2 - Synodic And Sideral MonthsChapter 21.3 - EclipsesChapter 22 - Location And Distance On EarthChapter 22.1 - Earth's Grid SystemChapter 22.2 - Determining LatitudeChapter 22.3 - Determining LongitudeChapter 22.4 - Using Earth's Grid SystemChapter 22.5A - Great Circles And Small Circles: Great CirclesChapter 22.5B - Great Circles And Small Circles: Small CirclesChapter 22.6A - Determining Distance Along A Great Circle: Determining Distance Along A Meridian Or The EquatorChapter 22.6B - Determining Distance Along A Great Circle: Globe And String Method For Determining DistanceChapter 22.7 - Determining Distance Along A ParallelChapter 22.8A - Longitude And Solar Time: Longitude And Solar TimeChapter 22.8B - Longitude And Solar Time: Using A Chronometer To Determine LongitudeChapter 22.9 - Latitude And The North StarChapter 23 - The Metric System, Measurements, And Scientific InquiryChapter 23.1 - The Metric SystemChapter 23.2 - Metric ConversionsChapter 23.3 - Metric-english ConversionsChapter 23.4 - Temperature ScalesChapter 23.5A - Other Units Of Measurement: Measuring Very Small ObjectsChapter 23.5B - Other Units Of Measurement: Measuring Very Great DistancesChapter 23.6 - Density And Specific GravityChapter 23.7 - Methods Of Scientific Inquiry
Sample Solutions for this Textbook
We offer sample solutions for Applications and Investigations in Earth Science Plus Mastering Geology with eText -- Access Card Package (8th Edition) homework problems. See examples below:
• Breaks along smooth planes: This physical property exhibited by minerals is known as cleavage. The...Chapter 2, Problem 1LRContour interval is calculated by the given formula: Contour interval=Difference in elevationNumber...Chapter 4, Problem 1LRBasin and range area located in Western U.S has fault-block mountains. The fault-block mountains are...Chapter 6, Problem 1LRChapter 7, Problem 1LRThe method of calculating the strike, angle of dip, and direction of dip includes the measurement of...Chapter 9, Problem 1LR
The Arctic ocean and half of the Atlantic ocean and the pacific ocean are present in the Northern...Pictorial representation: Fig.1 represents the features of the waves and wave particles. Fig.1: The...The width of the incoming sun rays between 0° and 30°N latitude can be calculated as:...The sun produces 100% solar radiation. Out of this 100%, around 20 % of the solar radiation is...Pictorial representation: Fig.1 Depicts the terms for the changes of state. Fig.1 Changes of state....cP stands for continental polar air mass. The source region of cP air mass is high latitude areas....There are six major controls of the climate. These are as follows: • Latitude: Latitude is one of...Pictorial Representation: Fig 1 represents the observed positions of the setting Sun. Fig 1: The...The steps that take place in the formation of the solar system, according to the nebular theory are...Pictorial representation: Fig.1: The orbits of Mercury, Venus, Earth, and Mars. Fig.1: The orbits of...The four main geologic processes that have shaped the surface of the terrestrial planets and the...The new moon takes place when the moon is positioned between the earth and the sun. The three...Pictorial representation: Figure 1 represents the Earth’s grid system. Fig. 1: Earth’s grid system...The basic metric unit for Length is “meter” and it is denoted by the symbol “m.” The basic metric...
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Applications And Investigations In Earth Science
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Mastering Geology With Pearson Etext -- Standalone Access Card -- For Applications And Investigations In Earth Science (9th Edition)
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Applications and Investigations in Earth Science Plus Mastering Geology with Pearson eText -- Access Card Package (9th Edition) (What's New in Geosciences)
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