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EAPS 105 Exam 2 Questions & Answers 2026 | 75+ Practice Questions | Plate Tectonics, Volcanism, Magnetic Fields, Impact Cratering & Planetary Geology | Purdue University

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This comprehensive EAPS 105 Exam 2 study guide contains more than 75 carefully compiled exam-style questions and verified answers covering planetary interiors, heat transfer, plate tectonics, magnetic field generation, volcanism, cryovolcanism, impact cratering, asteroid collisions, planetary evolution, and comparative planetology. The material is specifically designed to help students prepare for EAPS 105 Exam 2, midterm assessments, planetary geology examinations, Earth and Atmospheric Sciences coursework, and introductory planetary science evaluations. The document provides an in-depth exploration of the internal evolution of planets and moons, beginning with planetary heating mechanisms and differentiation processes. Students review how accretional heating, radioactive decay, gravitational compression, and core formation contribute to elevated internal temperatures and drive geological activity. The guide explains why larger planetary bodies remain geologically active longer than smaller bodies and examines the relationship between planetary size, heat retention, volcanism, tectonics, and magnetic field generation. A major focus is placed on planetary heat transfer processes, including conduction, convection, and radiation. Learners gain a detailed understanding of how heat moves through Earth’s inner core, outer core, mantle, and lithosphere, as well as how mantle convection drives plate tectonics. The material explores lithospheric structure, mid-ocean ridges, subduction zones, crustal recycling, and the geological processes that shape Earth's dynamic surface while contrasting these processes with the tectonically inactive surfaces of other terrestrial planets. The guide also provides extensive coverage of planetary magnetic fields and dynamo theory. Students learn the essential requirements for magnetic field generation, including electrically conductive fluids, convection, and planetary rotation. Comparative examples from Earth, Venus, Jupiter, Neptune, and other planetary bodies illustrate why some planets possess strong magnetospheres while others do not. The document further explains the role magnetic fields play in protecting atmospheres from solar wind interactions and sustaining long-term planetary habitability. Volcanology represents another major component of the study material. Students explore the three primary mechanisms that generate magma, including decompression melting, heat-induced melting, and hydration-induced melting. The resource covers hotspot volcanism, volcanic chains, shield volcanoes, stratovolcanoes, explosive and effusive eruptions, pyroclastic flows, caldera formation, eruption columns, and cryovolcanic activity on icy moons such as Enceladus. Comparative planetary examples from Earth, Venus, Mars, and Io demonstrate how gravity, atmospheric density, and tectonic activity influence volcanic processes across the Solar System. The final sections focus on impact cratering and planetary surface evolution. Students review impact velocities, crater formation stages, transient craters, simple and complex crater morphology, ejecta blankets, crater rays, shock metamorphism, asteroid impact evidence, mass extinction events, and planetary defense strategies. Significant attention is given to the Chicxulub impact, dinosaur extinction evidence, Near-Earth Asteroids (NEAs), and modern asteroid deflection techniques designed to mitigate future impact hazards. Key Topics Covered: • Planetary Differentiation and Internal Structure • Accretional Heating and Radioactive Decay • Heat Transfer Mechanisms • Conduction, Convection, and Radiation • Earth’s Core and Mantle Dynamics • Lithosphere and Asthenosphere • Plate Tectonics and Mantle Convection • Mid-Ocean Ridges and Subduction Zones • Comparative Planetary Geology • Planetary Cooling Processes • Magnetic Field Generation (Planetary Dynamo) • Magnetospheres and Solar Wind Protection • Jupiter and Neptune Magnetic Fields • Volcanism and Magma Formation • Hotspot Volcanism • Shield Volcanoes and Stratovolcanoes • Explosive and Effusive Eruptions • Pyroclastic Flows and Calderas • Cryovolcanism on Icy Worlds • Olympus Mons and Martian Geology • Planetary Gravity and Volcanic Activity • Impact Cratering Processes • Simple and Complex Craters • Ejecta Blankets and Crater Rays • Chicxulub Impact Event • Dinosaur Extinction Evidence • Near-Earth Asteroids (NEAs) • Asteroid Deflection Strategies • Planetary Hazard Assessment According to Planetary Sciences by Imke de Pater and Jack J. Lissauer, Earth: Portrait of a Planet by Stephen Marshak, and research published in Icarus, Journal of Geophysical Research: Planets, Nature Geoscience, and Annual Review of Earth and Planetary Sciences, planetary interiors, tectonic activity, volcanism, magnetic fields, and impact processes are fundamental mechanisms governing planetary evolution. Modern planetary geology integrates geophysics, geochemistry, astronomy, and comparative planetology to understand how terrestrial planets and moons develop over billions of years. The concepts covered throughout this exam closely align with foundational scientific principles taught in university-level Earth and planetary science programs. Relevant for: EAPS 105 Students Introduction to Planet Earth Students Planetary Science Students Planetary Geology Students Earth and Atmospheric Sciences Students Geology Students Earth Science Students Astronomy Students Geophysics Students Environmental Science Students STEM Undergraduates Physical Science Students Midterm Exam Preparation Students Final Exam Review Students Comparative Planetology Students Space Science Students Planetary Exploration Students Earth System Science Students Undergraduate Science Majors General Education Science Students Keywords EAPS 105 Exam 2, EAPS 105 answers, planetary geology, plate tectonics, mantle convection, lithosphere, asthenosphere, heat transfer, conduction, convection, radiation, planetary differentiation, planetary interiors, radioactive decay, accretional heating, magnetic fields, planetary dynamo, magnetosphere, volcanism, hotspot volcanism, shield volcanoes, stratovolcanoes, explosive eruptions, effusive eruptions, pyroclastic flows, caldera formation, cryovolcanism, Olympus Mons, planetary cooling, impact cratering, simple craters, complex craters, ejecta blankets, crater rays, Chicxulub crater, asteroid impacts, Near Earth Asteroids, planetary defense, comparative planetology, Purdue University EAPS 105

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EAPS 105 Exam 2 2026 Exam
Questions and Answers |
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The consequences of a planet or moon being hot inside - ANSWER

✔✔differentiation, volcanism, plate tectonics, magnetic fields


How hot the Earth is on the inside compared to the surface of the Sun -

ANSWER ✔✔the inner core is almost as hot as the surface of the

Sun, but is solid because the higher pressure raises the melting

temperature

, The relationship between heat and motion in atoms - ANSWER

✔✔when an object is stopped, the kinetic energy is converted into

atomic scale motion (vibration of atoms), which is the very definition of

heat

How core formation leads to an increase in internal temperature -

ANSWER ✔✔the motion of the falling iron is converted into

deformation at the surface of the growing core, producing heat


Why Io is hot inside - ANSWER ✔✔Io's elliptical orbit around Jupiter

causes the gravitational force between the two to vary, changing how

much Io's shape distorts as it orbits. This deformation generates enough

heat to melt Io's interior making it the most volcanically active body in the

Solar System


How radioactive decay produces heat - ANSWER ✔✔radioactive

decay is the process through which the nucleus of an unstable atom

transforms into a stable one by throwing off neutrons or protons, causing

collisions that produce heat


Why smaller planets cool faster than larger ones - ANSWER ✔✔less

primordial heat (less impacts smaller core), less radioactive elements to

keep them hot, smaller bodies have larger surface areas compared to

volume: can more efficiently get rid of heat

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