Earth Science Quiz
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Questions and Answers

Which of the following best describes the difference between atomic number and atomic mass?

  • Atomic number is the number of electrons while atomic mass is the number of protons.
  • Atomic number is the total number of protons and neutrons, while atomic mass is the number of protons.
  • Atomic number is the number of neutrons while atomic mass is the number of protons.
  • Atomic number is the number of protons while atomic mass is the total number of protons and neutrons. (correct)
  • A cation is a negatively charged ion.

    False (B)

    What type of chemical bond involves the sharing of electrons between atoms?

    covalent

    Minerals that have the same chemical composition but different crystal structures are called ______.

    <p>polymorphs</p> Signup and view all the answers

    Match each mineral property with its description:

    <p>Color = Visual appearance of a mineral's surface Streak = Color of a mineral's powder Luster = How a mineral reflects light Hardness = Resistance of a mineral to being scratched</p> Signup and view all the answers

    Which of the following best describes the primary reason why the Kola Superdeep Borehole project was unlikely to reach the Earth's mantle?

    <p>The immense heat at deep layers of the earth would melt the drill. (B)</p> Signup and view all the answers

    The geocentric model of the universe places the Sun at the center of the solar system.

    <p>False (B)</p> Signup and view all the answers

    What is the name of the theory that explains how the solar system formed?

    <p>Nebular Theory</p> Signup and view all the answers

    The two most abundant elements in Earth's atmosphere are ______ and ______.

    Signup and view all the answers

    Which of the following best describes the Doppler Effect?

    <p>The apparent change in the frequency of a wave due to the motion of the source or the observer. (C)</p> Signup and view all the answers

    The lithosphere is a layer of the Earth that is composed primarily of molten rock?

    <p>False (B)</p> Signup and view all the answers

    What two elements make up the majority of silica?

    <p>silicon and oxygen</p> Signup and view all the answers

    The process in which dense materials sink towards the Earth's center and less dense materials float toward the surface is called ______ .

    <p>differentiation</p> Signup and view all the answers

    Match the following scientists with their geological contribution:

    <p>Alfred Wegener = Proposed the theory of Continental Drift Hubble = Demonstrated the expansion of the Universe James Webb = Advanced the study of the early Universe Moho = Boundary between the crust and the mantle</p> Signup and view all the answers

    Which of these is NOT one of the four observations used by Wegener to support his continental drift hypothesis?

    <p>The presence of mid-ocean ridges (C)</p> Signup and view all the answers

    Oceanic crust is generally older than continental crust.

    <p>False (B)</p> Signup and view all the answers

    What is the name of the supercontinent that existed before the continents split apart?

    <p>Pangea</p> Signup and view all the answers

    Study Notes

    Geology Introduction

    • Geology is the study of the Earth.

    • Science is a systematic process of observation, experimentation, and analysis to understand the natural world.

    Kola Superdeep Borehole

    • The Kola Superdeep Borehole was a very deep drilling project.

    • The project aimed to reach the Earth's mantle but was ultimately unsuccessful in achieving the goal. It was anticipated to be too expensive and dangerous in the future.

    Crustal Differences

    • Continental crust is thicker and less dense than oceanic crust.

    • Oceanic crust is thinner and denser than continental crust.

    Earth in Context: Scientific Method

    • Scientific Method: A systematic approach to understanding natural phenomena, involving observation, hypothesis formulation, experimentation, and analysis.

    • Geocentric Model: A model of the solar system placing Earth at the center.

    • Heliocentric Model: A model of the solar system placing the Sun at the center.

    Milky Way and Universe

    • The Milky Way galaxy is vast, containing billions of stars.

    • The approximate number of stars in the Milky Way is billions.

    • The estimated number of galaxies in the universe, using Hubble, is large.

    • The estimated number of galaxies in the universe, using James Webb, is also large (likely larger).

    Doppler Effect

    • The Doppler Effect describes how the wavelength of a wave (like light) changes depending on the relative motion of the source and the observer.

    Big Bang Theory

    • Key Points: The universe began from a hot, dense state and has been expanding and cooling ever since.

    • Element Creation (besides Hydrogen and Helium): Most elements are created by nuclear fusion within stars.

    • Early Universe Composition: Primordial hydrogen and helium were the primary components of the early universe.

    Nebular Theory

    • Nebular Theory: The prevailing model explaining the formation of our solar system, proposing cloud collapse and accretion.

    Solar System Planets

    • Our solar system's planets (order from the Sun): Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, Neptune.

    Differentiation of Earth's Interior

    • Earth's interior layers differentiated based on density, forming a layered structure.

    • Earth Formation: Layers formed due to density differences during Earth's early molten stage.

    • Moon Formation: The leading hypothesis is that a Mars-sized object collided with the early Earth, the debris coalesced to form the Moon.

    Earth's Magnetic Field

    • Earth's magnetic field is crucial for shielding the planet from harmful solar radiation.

    • Mechanism of Magnetic Field: Generated by the movement of molten iron in Earth's outer core.

    Earth's Atmosphere

    • Earth's atmosphere is primarily composed of nitrogen and oxygen.

    Minerals and Glass

    • Glass: A non-crystalline solid, not a true mineral.

    • Silica: Composed of silicon and oxygen.

    Earth's Interior Variations

    • Pressure and temperature increase with depth within Earth.

    • Geothermal Gradient: The rate at which temperature increases with depth in the Earth.

    Crust, Mantle, and Core

    • Earth's layers: Crust, Mantle, and Core.

    • Thickness of each layer: Information on exact thicknesses is not needed at this level.

    Moho

    • Moho: The boundary separating the Earth's crust and mantle.

    Asthenosphere and Lithosphere

    • Asthenosphere: A zone of the upper mantle that exhibits ductile behavior due to high temperature and pressure.

    • Lithosphere: A rigid outer layer of the Earth encompassing the crust and part of the upper mantle.

    Plate Tectonics: Wegener's Contribution

    • Alfred Wegener: Proposed the continental drift hypothesis based on observations of continental shapes, fossil distribution, and paleoclimate data.

    Wegener's Observations

    • Fit of Continents: Continents seem to fit together like puzzle pieces.

    • Paleoclimate Data: Evidence of past climates across different continents.

    • Fossil Distribution: Matching fossil types across continents.

    • Matching Geologic Units: Similarities between rock formations on different continents.

    Pangea

    • Pangea: A supercontinent that existed millions of years ago.

    Paleomagnetism

    • Paleomagnetism: The study of past Earth's magnetic field recorded in rocks.

    Seafloor Spreading

    • Seafloor Spreading: The process of new seafloor creation at mid-ocean ridges and moving away from the ridge.

    Geographic vs. Magnetic Poles

    • Geographic poles are defined by Earth's spin axis, while magnetic poles reflect Earth's magnetic field.

    Bathymetry

    • Bathymetry: Mapping the ocean floor.

    Seafloor Age

    • The age of seafloor rock increases as you move away from a mid-ocean ridge (newest at the ridge).

    Magnetic Reversals

    • Magnetic Reversals: Changes in the Earth's magnetic field polarity (North and South poles interchange).

    Plate Tectonic Theory

    • Plate Tectonic Theory: A unifying theory describing the movement of Earth's lithospheric plates.

    Oceanic Crust vs. Earth

    • Oceanic crust is relatively young compared to the Earth as a whole due to the process of seafloor spreading.

    Plate Boundaries

    • Divergent: Plates move apart (e.g., mid-ocean ridges).

    • Convergent: Plates move together (3 types: ocean-continent, ocean-ocean, continent-continent collisions)

    • Transform: Plates slide past each other (e.g., San Andreas Fault).

    Plate Movement Rates

    • Average rate of plate movement.

    Continental Margins

    • Active continental margin: Continental margins near plate boundaries (more active).

    • Passive continental margin: Continental margins further from plate boundaries (less active).

    Hot Spots

    • Hot spots: Areas of volcanic activity associated with mantle plumes.

    Triple Junctions

    • Triple junctions: Points where three tectonic plates meet.

    Ridge Push vs. Slab Pull

    • Ridge push: Gravitational force pushing plates apart at mid-ocean ridges.

    • Slab pull: Gravitational force pulling plates into subduction zones.

    Chapter 3: Minerals: Introduction

    • Elements: Fundamental building blocks of matter.

    • Atomic Number vs. Atomic Weight: Atomic number represents the number of protons, while atomic weight reflects the average mass of an atom.

    • Ions: Charged atoms formed by loss or gain of electrons.

    • Cations: Positively charged ions.

    • Anions: Negatively charged ions.

    • Chemical Bonds: Interactions holding atoms together in molecules including; Ionic, covalent, metallic, and van der Waals bonds.

    • Molecule vs. Compound: A molecule is the smallest unit of a substance, while a compound is a substance formed from multiple elements.

    • Definition of a Mineral: A naturally occurring, inorganic, solid substance with a definite chemical composition and ordered atomic arrangement.

    Polymorphs

    • Polymorphs: Minerals with the same chemical composition but different crystal structures.

    Minerals: Identifying Properties

    • Methods of mineral identification: Color, Streak, Luster, Hardness, Specific Gravity, Crystal Habit/Form, Cleavage, Fracture, and Special Properties (like taste or magnetism).

    Identifying Minerals: Challenges and Considerations

    • Limitations of using color in mineral identification.

    Hardness Scale

    • Mohs hardness scale: A scale ranking mineral hardness.

    Mineral Groups

    • Mineral Groups: Major categories of minerals (e.g., silicates, oxides, sulfides, halides, carbonates, native metals).
    • Most common within continental crust are silicates.

    Silica Tetrahedra

    • Silica tetrahedra: Basic structural units in most silicate minerals built from silicon and oxygen atoms.

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    Test your knowledge on key concepts in Earth Science, including atomic structure, chemical bonding, and mineral properties. This quiz covers essential topics that shape our understanding of the Earth and its atmosphere.

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