Browse All Chapters of This Textbook
Chapter 1 - The Earth In ContextChapter 1.2 - An Image Of Our UniverseChapter 1.3 - Forming The UniverseChapter 1.4 - Farming The Solar System, Including The EarthChapter 1.5 - Earth's Moon And Magnetic FieldChapter 1.6 - Introducing The Earth SystemChapter 1.7 - Looking Inwarddiscovering The Earth's InteriorChapter 2 - The Way The Earth Works: Plate TectonicsChapter 2.2 - Wegener's Evidence For Continental DriftChapter 2.3 - Paleomagnetism-proving That Continents Move
Chapter 2.4 - The Discovery Of Seafloor SpreadingChapter 2.5 - Evidence Far Seafloor SpreadingChapter 2.6 - What Do We Mean By Plate Tectonics?Chapter 2.7 - Divergent Plate Boundaries And Seafloor SpreadingChapter 2.8 - Convergent Plate Boundaries And SubductionChapter 2.9 - Transform Plate BoundariesChapter 2.10 - Special Locations In The Plate MosaicChapter 2.11 - How Do Plate Boundaries Farm And Die?Chapter 2.12 - Moving PlatesChapter 3 - Patterns In Nature: MineralsChapter 3.2 - What Is A Mineral?Chapter 3.3 - Beauty In Patterns: Crystals And Their StructureChapter 3.4 - Haw Can You Tell One Mineral Tram Another?Chapter 3.5 - Organizing Your Knowledge: Mineral ClassificationChapter 3.6 - Something Preciousgems!Chapter 4 - Up From The Inferno: Magma And Igneous RocksChapter 4.2 - Why Does Magma Farm, And What Is It Made Of?Chapter 4.3 - Movement And Solidification Of Molten RackChapter 4.4 - How Do You Describe An Igneous Rack?Chapter 4.5 - Plate-tectonic Context Af Igneous ActivityChapter 5 - The Wrath Of Vulcan: Volcanic EruptionsChapter 5.2 - The Products Of Volcanic EruptionsChapter 5.3 - Structure And Eruptive StyleChapter 5.4 - Geologic Settings At VolcanismChapter 5.5 - Beware: Volcanoes Are Hazards!Chapter 5.6 - Protection From Vulcan's WrathChapter 5.7 - Effect Of Volcanoes On Climate And CivilizationChapter 5.8 - Volcanoes Elsewhere In The Solar SystemChapter 6 - Pages Of Earth's Past: Sedimentary RocksChapter 6.2 - Classes At Sedimentary RacksChapter 6.3 - Sedimentary StructuresChapter 6.4 - How Do We Recognize Depositional Environments?Chapter 6.5 - Sedimentary BasinsChapter 7 - Metamorphism: A Process Of ChangeChapter 7.1 - IntroductionChapter 7.2 - Consequences And Causes Of MetamorphismChapter 7.3 - Types Of Metamorphic RacksChapter 7.4 - Where Does Metamorphism Occur?Chapter 8 - A Violent Pulse: EarthquakesChapter 8.2 - Faulting And The Generation Of EarthquakesChapter 8.3 - Seismic Waves And Their MeasurementChapter 8.4 - Defining The Size Of EarthquakesChapter 8.5 - Where And Why Do Earthquakes Occur?Chapter 8.6 - How Do Earthquakes Cause Damage?Chapter 8.7 - Can We Predict The "big One"?Chapter 8.8 - Earthquake Engineering And ZoningChapter 9 - Crags, Cracks, And Crumples: Geologic Structures And Mountain BuildingChapter 9.2 - Rack Deformation In The Earth's CrustChapter 9.3 - Brittle StructuresChapter 9.4 - Folds And FoliationsChapter 9.5 - Causes Of Mountain BuildingChapter 9.6 - Other Consequences Of Mountain BuildingChapter 9.7 - Basins And Domes In CratonsChapter 10 - Deep Time: How Old Is Old?Chapter 10.2 - The Concept Of Geologic TimeChapter 10.3 - Geologic Principles Far Defining Relative AgeChapter 10.4 - Unconformities: Gaps In The RecordChapter 10.5 - Stratigraphic Formations And Their CorrelationChapter 10.6 - The Geologic ColumnChapter 10.7 - How Do We Determine Numerical Ages?Chapter 10.8 - Numerical Ages And Geologic TimeChapter 11 - A Biography Of EarthChapter 11.2 - Hadean And Archean Time: Earth's Early DaysChapter 11.3 - The Proterozoic: The Earth In TransitionChapter 11.4 - The Paleozoic Era: Continents Reassemble, And Life Gets ComplexChapter 11.5 - The Mesozoic Era: When Dinosaurs RuledChapter 11.6 - The Cenozoic Era: The Modern World Comes To BeChapter 12 - Riches In Rock: Energy And Mineral ResourcesChapter 12.2 - Sources Of Energy In The Earth SystemChapter 12.3 - Introducing Hydrocarbon ResourcesChapter 12.4 - Conventional Hydrocarbon SystemsChapter 12.5 - Unconventional Hydrocarbon ReservesChapter 12.6 - Coal: Energy Tram The Swamps At The PastChapter 12.7 - Nuclear PowerChapter 12.8 - Other Energy SourcesChapter 12.9 - Energy Choices, Energy ChallengesChapter 12.10 - Mineral ResourcesChapter 12.11 - Nonmetallic Mineral ResourcesChapter 12.12 - Global Mineral NeedsChapter 13 - Unsafe Ground: Landslides And Other Mass MovementsChapter 13.2 - Types Of Mass MovementChapter 13.4 - Haw Can We Protect Against Mass-movement Disasters?Chapter 14 - Streams And Floods: The Geology Of Running WaterChapter 14.2 - Draining The LandChapter 14.3 - Describing Flow In Streams: Discharge And TurbulenceChapter 14.4 - Thewark Of Running WaterChapter 14.5 - Streams In The LandscapeChapter 14.6 - The Evolution Of DrainageChapter 14.7 - Raging WatersChapter 14.8 - Human Impact On RiversChapter 15 - Restless Realm: Oceans And Coast SChapter 15.2 - Landscape Beneath The SeaChapter 15.3 - Ocean Water And Its MovementChapter 15.4 - Where Land Meets Sea: Coastal LandformsChapter 15.5 - Causes Of Coastal VariabilityChapter 15.6 - Coastal Problems And SolutionsChapter 16 - A Hidden Reserve: GroundwaterChapter 16.2 - Where Does Groundwater Reside?Chapter 16.3 - Groundwater FlowChapter 16.4 - Tapping Groundwater SuppliesChapter 16.5 - Hot Springs And GeysersChapter 16.6 - Groundwater ProblemsChapter 16.7 - Caves And KarstChapter 17 - Dry Regions: The Geology Of DesertsChapter 17.2 - The Nature And Locations Of DesertsChapter 17.3 - Producing Desert LandscapesChapter 17.4 - Deposition In DesertsChapter 17.5 - Desert Landscapes And Desert LifeChapter 17.6 - Desert ProblemsChapter 18 - Amazing Ice: Glaciers And Ice AgesChapter 18.2 - Ice And The Nature Of GlaciersChapter 18.3 - Carving And Carrying By LceChapter 18.4 - Deposition Associated With GlaciationChapter 18.5 - Other Consequences Of Continental GlaciationChapter 18.6 - The Pleistocene Ice AgeChapter 18.7 - The Causes Of Ice AgesChapter 19 - Global Change In The Earth SystemChapter 19.2 - Unidirectional ChangesChapter 19.3 - Cyclic ChangesChapter 19.4 - Global Climate ChangeChapter 19.5 - Contemporary Global WarmingChapter 19.6 - Other Human Impacts On The Earth SystemChapter 19.7 - The Future Of The Earth
Book Details
Essentials of Geology, integrates Marshak’s popular and proven text approach with exciting new media and assessment resources that guide students to a clearer understanding of the course material. Marshak has personally applied his expertise, with an emphasis on the visuals, to this robust suite of videos, animations and simulations, art, and interactive assessment questions that get students seeing and engaging with geologic concepts as a geologist would.
Sample Solutions for this Textbook
We offer sample solutions for Essentials of Geology (Fifth Edition) homework problems. See examples below:
Ptolemy assumed that all the planets revolved around the Earth in a circular path, including the...Explanation: Alfred Wegener is a German geologist who formulated the idea of the continental drift...Explanation: “A mineral is a naturally occurring solid, formed by geologic processes, that has a...Explanation: Magma is the molten rock that is present deep inside the surface. When it reaches the...Explanation: A volcanic eruption brings materials from inside the earth to surface of the earth. The...Explanation: The erosion, transportation and deposition and subsequent compaction of sediments by...Explanation: The igneous rocks are formed when the molten magma or lava consolidates completely....Explanation: A fault is a planar fracture or discontinuity in a volume of rock, across which there...Explanation: The Alps, is a result of collision tectonics. Here, the continental plate boundaries...
Explanation: According to the principle of uniformitarianism, we observe that there is no...Explanation: The rocks present on the surface of the earth are classified into three types based on...Explanation: There are several fundamental sources of energy in the Earth’s system and they are...Explanation: “The down slope transport of rock, regolith (soil, and loose sediment or debris), snow,...Explanation: A hydrological cycle, also known as water cycle, deals with the continuous circulation...Explanation: When viewing from space, the Earth glows blue in color; the presence of oceans are the...Explanation: Any open space present within the rock sediment or a given volume of rock is known as...Explanation: “A desert is a region that is so arid (dry) that it supports very little vegetation.” A...Explanation: An ice age is a period in the Earth’s history in which the climates were extremely...Explanation: “The global interconnecting web of physical and biological phenomena on the Earth is...
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