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GLY1880 Exam 1 Questions (150) – Plate Tectonics, Earthquakes, Volcanoes & Natural Hazards – University of Florida

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This document contains 150 exam-style questions with correct answers designed for GLY1880 Earth Science / Physical Geology Exam 1 at the University of Florida, covering material from Chapters 1–5 of the course. The questions focus on key geological concepts including plate tectonics, earthquake processes, seismic hazards, volcanic activity, and natural disaster mitigation. The material is organized in a format commonly used in university assessments, making it an effective study resource for reviewing foundational Earth science concepts and preparing for quizzes, midterms, and final exams. A significant portion of the document focuses on earthquake science and seismic hazards, including topics such as subduction zones, fault movement, liquefaction, seismic wave behavior, and earthquake intensity measurements. The questions explore the mechanics of earthquakes through concepts such as the elastic rebound theory, seismic wave propagation (P-waves, S-waves, and surface waves), epicenter location using seismographs, and the factors that determine earthquake damage in populated areas. Real-world examples such as the New Madrid Seismic Zone earthquake sequence of 1811–1812 are used to illustrate the impact of large earthquakes and the challenges of disaster planning and mitigation in vulnerable regions. The document also provides detailed coverage of volcanology and magma processes, including magma composition, viscosity, eruption styles, and volcanic landforms. Students review concepts such as basaltic versus rhyolitic magma, explosive eruptions, eruption columns, caldera formation, lava domes, and volcanic hazards like lahars and pyroclastic flows. The relationship between water content, pressure changes, and explosive eruptions is also examined, highlighting how dissolved gases within magma contribute to volcanic explosivity. Another major section explores plate tectonics and global geologic processes, including divergent, convergent, and transform plate boundaries, seafloor spreading, mantle convection, and lithosphere–asthenosphere interactions. The document explains how tectonic plate movement drives the distribution of earthquakes and volcanoes around the globe. Concepts such as continental drift, the formation of new crust at mid-ocean ridges, and the structure and thickness of Earth’s lithosphere are also discussed. The material further introduces natural hazard mitigation and disaster preparedness, emphasizing how infrastructure planning, seismic building codes, and monitoring technologies can reduce the impact of earthquakes and volcanic eruptions. Monitoring techniques discussed in the questions include gas emission monitoring, tiltmeters, GPS measurements, strainmeters, and seismic monitoring systems used to detect magma movement and predict potential eruptions. The topics and terminology used throughout the document align closely with widely used introductory geology textbooks such as “Earth: An Introduction to Physical Geology” by Edward J. Tarbuck, Frederick K. Lutgens, and Dennis Tasa, which is commonly used in university Earth science and geology courses. As a result, the content reflects the types of questions and conceptual understanding typically assessed in undergraduate geology and Earth science examinations. This document may be useful for students enrolled in courses such as: Physical Geology Earth Science Introduction to Geology Natural Hazards and Disaster Science Environmental Geology Volcanology and Seismology It is particularly relevant for students studying in programs including: Geology Earth and Environmental Science Environmental Studies Geography Environmental Engineering Natural Resource Management Keywords: earth science exam questions, physical geology study guide, plate tectonics geology, earthquake hazards geology, seismic waves p waves s waves, elastic rebound theory, liquefaction earthquakes, tsunami generation subduction zones, volcanic eruptions geology, magma viscosity rhyolitic basaltic, caldera formation volcanoes, shield volcano eruptions, lahar volcanic hazards, volcanic monitoring methods, seismic hazard mitigation, new madrid seismic zone earthquakes, lithosphere asthenosphere structure, mantle convection plate tectonics, seafloor spreading geology

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Exam 1 UF GLY1880 (Chapters
1-5) 2026 Exam Questions with
100% Correct Answers | Latest
Update



Which plate boundary type is most likely to have earthquakes that generate

large tsunamis? - 🧠 ANSWER ✔✔-subduction zones


-transform

-divergent

,-collision




answer: subduction zones

Where would be the safest location during a subduction zone earthquake?

Assume the same building height and construction in all locations. - 🧠

ANSWER ✔✔-at the beach


-in the center of a valley full of sediment

-(answer) on a flat area of bedrock that is not saturated

-all of these would be equally safe

If all saturated, which of the following would be most likely to experience

liquefaction during an earthquake? - 🧠 ANSWER ✔✔-(answer) sand


-basalt

-granite

-limestone

If you are in a region affected by an earthquake, shaking is likely to be

greatest in which of the following settings? - 🧠 ANSWER ✔✔-(answer) a

river valley full of sediments where the water table is near the surface

,-on sand dunes where the water table is deep below the surface

-on the side of a sandstone hill

-at the top of a gneiss mountain


Which of the following is true of tsunamis? - 🧠 ANSWER ✔✔-(answer)

wave height is tallest in shallow near shore environments

-they can be caused by tidal action

-tsunamis are isolated (single-wave) events and never followed by

secondary waves

-the wave height is largest at sea in deep water

Compared to wind-generated waves, tsunami waves in the open ocean

(away from shore) are: - 🧠 ANSWER ✔✔-have a shorter period (time

between waves)

-(answer) much faster

-much taller (larger amplitude)

An earthquake of the same magnitude in California, USA and Turkey would

result in: - 🧠 ANSWER ✔✔-the results in terms of casualties would be about

equal


COPYRIGHT©PROFFKERRYMARTIN 2025/2026. YEAR PUBLISHED 2026. COMPANY REGISTRATION NUMBER: 619652435. TERMS OF USE.
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, -(answer) more casualties in Turkey because of the lack of earthquake

resistant building practices

-more casualties in California because of a higher population density

The epicenter of the 1895 Mexico City earthquake was actually not

anywhere near Mexico City. The primary reason shaking was so much

greater in Mexico City was: - 🧠 ANSWER ✔✔-the earthquake generated a

large tsunami

-the epicenter of the earthquake was in the densely populated downtown

area

-(answer) the saturated lakebed sediments the city is built on

-the hard bedrock the city is built on


Most earthquake-related fatalities are due to: - 🧠 ANSWER ✔✔-(answer)

shaking-related damage to structures

-tsunamis

-landslides

-people falling into earth fissures (cracks)

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