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Questions and Answers

What percentage of parent atoms remain after two half-lives in a radioactive decay process?

  • 12.5%
  • 75%
  • 50%
  • 25% (correct)

If a sample of a radioactive isotope initially contains 1000 atoms, and after a certain period, 750 atoms have decayed into daughter atoms, how many half-lives have passed?

  • 2 (correct)
  • 1/4
  • 1
  • 1/2

Elements are defined by which of the following properties?

  • Number of electrons
  • Number of neutrons
  • Number of protons (correct)
  • Atomic mass

Which statement accurately describes isotopes of an element?

<p>They have the same number of protons but a different number of neutrons. (D)</p> Signup and view all the answers

Which of the following isotopes of hydrogen is/are NOT radioactive?

<p>$^1H$ and $^2H$ (B)</p> Signup and view all the answers

The Earth's layers can be defined by composition/chemistry and physical strength. Which layer is defined as metallic and very dense?

<p>Core (A)</p> Signup and view all the answers

A rock subjected to stress deforms permanently without fracturing. Which type of behavior does this demonstrate?

<p>Ductile (C)</p> Signup and view all the answers

Which statement accurately describes the Asthenosphere's role in plate tectonics?

<p>It is a 'mushy' layer within the mantle that allows the plates to move. (C)</p> Signup and view all the answers

The Lithosphere is best described as which of the following?

<p>The crust plus the uppermost mantle, a rigid layer which forms tectonic plates (B)</p> Signup and view all the answers

If a material undergoes deformation and returns to its original shape once the stress is removed, it is exhibiting what kind of behavior?

<p>Elastic (D)</p> Signup and view all the answers

How does the behavior of a material described as 'brittle' differ from one described as 'ductile' under stress?

<p>A brittle material will fracture, whereas a ductile material will bend and flow. (C)</p> Signup and view all the answers

What is the approximate thickness range of the Earth's crust?

<p>5-60 kilometers (B)</p> Signup and view all the answers

Which of the following statements correctly distinguishes between the crust and a tectonic plate?

<p>The crust is a geochemical/density layer, while the tectonic plate is a physical layer comprising the crust and uppermost rigid mantle. (C)</p> Signup and view all the answers

Which of the following best describes the initial state of the solar system before the formation of the Sun and planets?

<p>A rotating spherical cloud of gas, ice, dust, and debris. (C)</p> Signup and view all the answers

The formation of the solar system involved a transformation of energy. What was the primary force driving the initial contraction and flattening of the solar system cloud?

<p>Gravity (C)</p> Signup and view all the answers

Approximately how long ago did the Sun and planets form?

<p>4.6 billion years ago (D)</p> Signup and view all the answers

Planet formation released significant heat. Which of the following was NOT a primary source of this initial heat?

<p>Solar radiation (D)</p> Signup and view all the answers

What is the estimated time frame for the Earth's initial formation through the aggregation of particles and gases?

<p>30 to 100 million years (B)</p> Signup and view all the answers

Which of the following is the LEAST significant source of Earth's current internal heat?

<p>Accretion heat (D)</p> Signup and view all the answers

How did gravitational energy contribute to the Earth's internal heat?

<p>By the core sinking to the middle of the Earth. (C)</p> Signup and view all the answers

Which of the following elements is a major source of radioactive heat within the Earth?

<p>Uranium (A)</p> Signup and view all the answers

What is the primary source of heat within the Earth through geologic time?

<p>Radiogenic heat from radioactive decay. (B)</p> Signup and view all the answers

Which of the following describes radioactive isotopes?

<p>Atoms of the same element with different numbers of neutrons. (D)</p> Signup and view all the answers

What occurs during alpha decay?

<p>The emission of a helium nucleus from the nucleus. (D)</p> Signup and view all the answers

Which set of elements is most important for generating radiogenic heat within the Earth?

<p>Uranium, Thorium, Potassium (B)</p> Signup and view all the answers

If a radioactive element has a half-life of 1 million years, approximately what fraction of the parent atoms will remain after 3 million years?

<p>$1/8$ (D)</p> Signup and view all the answers

Why was the early Earth significantly hotter than it is today?

<p>There were more short-lived radioactive elements present. (B)</p> Signup and view all the answers

What is the correct definition of 'half-life'?

<p>The time it takes for half of a radioactive element to decay into its daughter atoms. (C)</p> Signup and view all the answers

Imagine you start with 400 radioactive atoms. If the half-life of the element is 10 days, how many atoms will remain after 20 days?

<p>100 (B)</p> Signup and view all the answers

If the entire history of Earth were compressed into a single year, approximately how long ago did the dinosaurs become extinct?

<p>7.8 months ago (A)</p> Signup and view all the answers

Which of the following statements best describes the contribution of accretion heat to Earth’s internal energy over geologic time?

<p>It is uncertain how much of the initial accretion heat remains within the Earth. (D)</p> Signup and view all the answers

The Earth's internal temperature has been declining since its early formation. Which of the following geological activities is still largely driven by this internal heat?

<p>Plate tectonics (C)</p> Signup and view all the answers

What is the primary process that caused the Earth to differentiate into layers such as the crust, mantle, and core?

<p>The differing densities of materials (B)</p> Signup and view all the answers

Which of the following contributes heat to the Earth's interior today, and will continue doing so into the future?

<p>Decay of radioactive materials (C)</p> Signup and view all the answers

Imagine two hypothetical planets with identical mass and volume. Planet A is composed primarily of iron, while Planet B is composed primarily of silicate rocks. Which of the following statements is most accurate?

<p>Planet A has a higher density than Planet B. (D)</p> Signup and view all the answers

How did the differentiation of Earth into layers affect the distribution of elements?

<p>Heavy elements concentrated in the core, light elements in the crust (C)</p> Signup and view all the answers

Why is the understanding of Earth's internal heat sources important in studying plate tectonics?

<p>Internal heat provides the energy for plate movement. (C)</p> Signup and view all the answers

If a rock sample has a mass of 600 kg and a volume of 0.2 m³, what is its density?

<p>3000 kg/m³ (C)</p> Signup and view all the answers

A geologist discovers a new mineral. She determines its density to be 4.5 g/cm³. If she has a 500 cm³ sample, what is the mass of the sample in kilograms?

<p>2.25 kg (A)</p> Signup and view all the answers

Which of the following statements best describes the concept of isostasy?

<p>The balance between gravity and buoyancy, where less dense materials float on top of more dense materials. (A)</p> Signup and view all the answers

Why does continental crust generally have a higher average elevation compared to oceanic crust?

<p>Continental crust is thicker and less dense than oceanic crust, allowing it to 'float' higher on the mantle. (D)</p> Signup and view all the answers

If a certain volume of mantle material is found to have a higher density than expected, what implications might this have for the surrounding crustal elevation, assuming isostatic equilibrium?

<p>The crustal elevation in that area would likely be lower as the denser mantle supports less crust. (A)</p> Signup and view all the answers

Which of the following statements accurately compares the density of Earth's layers?

<p>The core is the densest layer, followed by the mantle, crust, and atmosphere. (D)</p> Signup and view all the answers

Considering the average densities of continental crust (2700 kg/m³) and oceanic crust (3000 kg/m³), what would happen if a large section of continental crust were to collide with and override a section oceanic crust?

<p>The oceanic crust would sink beneath the continental crust due to its higher density. (B)</p> Signup and view all the answers

How does partial melting of rock contribute to the density stratification within the Earth?

<p>Partial melting allows low-density melts to rise through higher-density rock, enhancing density differences. (B)</p> Signup and view all the answers

Flashcards

Half-life

The time it takes for half of the radioactive atoms in a sample to decay.

Daughter atoms after two half-lives

After two half-lives, 75% parent atoms decay into daughter atoms, leaving 25% of parent atoms. The ratio of the daughter atoms will be 3/4.

Isotopes

Atoms of the same element with different numbers of neutrons.

Elements

Defined by the number of protons in the nucleus.

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Radioactive Isotopes

Isotopes that spontaneously decay releasing energy in the form of particles or electromagnetic waves.

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Source of Natural Disasters

Natural disasters result from the rapid release of concentrated energy.

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Solar System Origin

The solar system originated from a rotating cloud of gas, ice, dust and debris.

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Cloud Evolution to Disk

The cloud of gas, ice, dust and debris contracted, sped up, and flattened into a disk due to gravity.

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Age of Solar System

The Sun and planets formed simultaneously approximately 4.6 billion years ago.

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Planet Formation Heat

The processes of planet formation generated significant quantities of heat.

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Earth's Formation

Earth began as an aggregating mass of particles and gases around 4.6 billion years ago.

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Sources of Earth's Internal Heat

Impact energy, decay of radioactive elements and gravitational energy are all contribute to Earth's heat.

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Accretion Heat

Kinetic energy of colliding bolides, converted to heat.

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"Gravitational Heat"

Heat from core separating and sinking.

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Radioactive Heat

Heat from the decay of elements inside Earth.

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Internal Sources of Earth's Energy

Heat from Earth's formation (impact and gravitational energy) and radioactive decay of isotopes.

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Primordial Heat

The energy released during Earth's formation as materials collided and compressed.

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Early Earth's Internal Energy

Impacts, gravity, and radioactive elements.

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Earth's Differentiated Layers

Crust, mantle, and core

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Gravitational Energy

Energy released as heavy materials sank to the core, compressing Earth's interior.

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Density Differentiation

Sinking of heavy elements toward the middle.

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Density

Mass per unit volume. How much "stuff" in a space.

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A ton of bricks or feathers?

Both weigh the same.

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Radioactive Decay

The process by which unstable atomic nuclei lose energy by emitting radiation.

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Key Heat-Producing Elements

Uranium (U), Thorium (Th), and Potassium (K).

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Density Layering

The Earth is layered by density, with the core being the most dense, followed by the mantle, and then the crust.

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Earth's Core

Metallic, very dense (~10-16 gm/cm3), and makes up about half of Earth's radius.

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Earth's Mantle

Solid rock with a density of 3 to 6 gm/cm3, making up about half of Earth's radius

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Earth's Crust

Solid rock, lighter (2.7 to 3 gm/cm3) and very thin (5-60 km)

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Elastic Behavior

Material returns to its original shape after stress is removed.

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Ductile (Plastic) Behavior

Material deforms permanently under stress.

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Brittle Behavior

Material breaks or fractures under stress.

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Lithosphere

The rigid outer layer of the Earth, including the crust and uppermost mantle (approximately 100km thick).

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Density Formula

Density equals mass divided by volume (mass/volume) or number divided by volume (#/volume). More dense means less space between.

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Density (kg/m³)

Mass divided by volume. Measured in kilograms per cubic meter (kg/m³).

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Isostasy & Density

Less dense materials float on top of more dense materials.

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Earth's Density Layers

Earth's layers are arranged by density, with the least dense (Atmosphere) on the outside and the most dense (Core) at the center.

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Oceanic vs. Continental Crust

Oceanic crust is more dense (3000 kg/m³) and thinner than continental crust, which is less dense (2700 kg/m³) and thicker.

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Isostasy Definition

The balance between gravity and buoyancy, where less dense crust 'floats' on the denser mantle.

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Isostasy - Crust & Mantle

Describes how the Earth's crust floats on the mantle, with oceanic crust sitting lower than continental crust. Mountains on continents have deep 'roots'.

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Study Notes

  • The lecture covers the formation and structure of the Earth, focusing on geological disasters and society. It includes online lectures about energy in the Earth system, the formation of the Earth and solar system, how the Earth differentiates into layers, and the chemistry versus physics of these layers.

Solar System Formation

  • The solar system's origin involved a rotating spherical cloud of gas, ice, dust, and debris.
  • Gravity caused the cloud to contract, accelerate its rotation, and flatten into a disk.
  • The Sun and planets formed concurrently about 4.6 billion years ago.

Earth's History

  • Earth began as an aggregating mass of particles and gases.
  • Aggregation of particles to form took approximately 30 to 100 million years.
  • Planet formation involved processes that produced substantial heat, including impact energy, decay of radioactive elements, gravitational energy, and differentiation into layers.

Earth's Internal Heat Sources

  • Accretion heat is the kinetic energy of bolides converted to heat upon collision.
  • Gravitational heat represents the energy converted to heat as the core separated and sank.
  • Radioactive heat comes from the decay of uranium, thorium, and potassium-40 inside the Earth, likely the main heat source through geologic time and today.

Internal Energy Sources

  • Impact energy from collisions heated Earth during its formation.
  • Gravitational energy: As heavy elements sank and compressed to form the core, it heated the Earth.
  • Isotopes are forms of the same element with differing numbers of neutrons.
  • Radioactive isotopes are unstable and decay into stable isotopes, releasing heat and energy.
  • Radioactive atoms decay and release heat; Uranium, Thorium, and Potassium are the most significant elements in this process.
  • Half-life is the time required for half of the radioactive parent atoms to decay into daughter atoms.
  • 235U has 92 protons and 143 neutrons, while 238U has 92 protons and 146 neutrons.
  • Radioactive isotopes are unstable and release energy during decay, transforming into more stable isotopes.
  • Measuring the ratio of radioactive isotopes to their decay products helps date rocks.

Earth's Timeline

  • The oldest solar system materials measure 4.57 billion years old.
  • The oldest Earth rocks found in northwest Canada date back 4.055 billion years.

Earth's Structure

  • Earth consists of density-stratified layers.
  • Atmosphere forms the least dense layer
  • Continents have a crust primarily of granite (~2.7 g/cm³).
  • Oceans have crust mainly of basalt (~3.0 g/cm³).
  • The core consists of metal, and its density can reach up to 16 g/cm³.
  • Earth differentiates into the crust, mantle, and core based on density, with heavier elements sinking and lighter elements floating.

Density as a Concept

  • Density signifies the relationship between mass and volume.
  • The density of a substance determines its buoyancy, or ability to float.
  • Less dense materials float on top of denser materials.

Chemical vs Physical Properties

  • The crust is the outermost layer, composed of lighter, low-density rock & is light in color.
  • The mantle is the middle layer, consisting of dark-colored, heavy rock.
  • The core is the innermost layer, composed of metallic elements.
  • The lithosphere includes the crust and uppermost mantle and behaves as a rigid layer, forming tectonic plates.
  • The asthenosphere is a layer within the mantle that is solid but can flow like plastic, enabling plate movement.
  • The mesosphere is a stiff plastic layer within the interior.
  • The outer core is liquid
  • The inner core is solid

Isostasy

  • Isostasy is the balance between gravity and buoyancy and also means less dense materials float on top of more dense material.
  • Mountains on continents have thicker, lower-density crust and deep roots.
  • Oceanic crust floats lower on the mantle than continental crust because of it's higher density.

Mechanical Behavior of Materials

  • Elastic materials recover after deformation.
  • Ductile (plastic) materials deform permanently.
  • Brittle materials break.

Continental vs. Oceanic Crust

  • Continental crust is thicker (30-35 km) and less dense (~2.7 g/cm³) made of primarily granite.
  • Oceanic crust is thinner (~7 km) and denser (~3 g/cm³) and consists mainly of basalt.

Plate Tectonics Framework

  • Tectonic plates are composed of a strong lithosphere overlying a weak asthenosphere.
  • The internal energy within earth drives plate tectonics.

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