Geology Quiz: Continental Margins and Sediments

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Questions and Answers

Which of the following is a characteristic of active continental margins?

  • Absence of plate boundaries
  • Tectonically quiet regions
  • Frequent earthquakes and volcanoes (correct)
  • Wide continental shelves

The Wilson Cycle describes the life cycle of mountain ranges.

False (B)

What are two ways that sediments can be classified?

Sediments can be classified by their source and by their size.

The depth at which calcium carbonate starts to dissolve is called the ______.

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

Match the following sediment types with their primary composition:

<p>Calcareous ooze = Calcium carbonate Siliceous ooze = Silica Terrestrial sediments = Rock and mineral particles</p> Signup and view all the answers

What is the primary force shaping the seabed, alongside erosion and deposition?

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

Passive continental margins are characterized by frequent earthquakes and volcanic activity.

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

What is bathymetry?

<p>The measurement of ocean depths and the charting of the shape of the ocean floor.</p> Signup and view all the answers

The Cascadia Subduction Zone is an example of an ______ plate boundary.

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

Match the sediment type with its primary material:

<p>Calcareous ooze = Calcium carbonate Siliceous ooze = Silica Lithogenous = Rock fragments Hydrogenous = Precipitated minerals</p> Signup and view all the answers

Which of the following is a key feature of a passive continental margin?

<p>A wide continental shelf (A)</p> Signup and view all the answers

The Earth's outer core is solid.

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

What can grain size and shape in sediments tell us about the depositional environment?

<p>Grain size and shape can indicate the energy levels of the environment and the distance the particles have traveled.</p> Signup and view all the answers

Which type of rock is formed from the cooling and solidification of molten magma or lava?

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

The asthenosphere is a rigid layer of the Earth located above the lithosphere.

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

What is the name of the process by which sediments become solid rock?

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

A __ is a deep, underwater feature typically found at subduction zones where one plate is forced beneath the other.

<p>Ocean trench</p> Signup and view all the answers

Match the following plate boundary type with the geological features or activity typically associated with them:

<p>Divergent boundary = Mid-ocean ridges, seafloor spreading Convergent boundary = Ocean trenches, volcanic arcs, mountain ranges Transform boundary = Earthquakes, fault lines</p> Signup and view all the answers

Which of the following is a common feature found at divergent plate boundaries?

<p>Mid-Ocean Ridges (C)</p> Signup and view all the answers

The Wilson Cycle describes the opening and closing of ocean basins.

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

What is the name for a volcano that forms over a relatively stationary mantle plume?

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

Which layer of the Earth is primarily liquid?

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

Oceanic crust is thicker and less dense than continental crust.

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

What is the semi-fluid layer beneath the lithosphere that allows tectonic plate movement?

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

_______ rocks form from the cooling and solidification of molten rock.

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

Match the plate boundary type with its description:

<p>Convergent = Plates move toward each other Divergent = Plates move apart Transform = Plates slide past each other</p> Signup and view all the answers

What is a key piece of evidence supporting continental drift?

<p>Matching rock formations across different continents. (A)</p> Signup and view all the answers

The age of the seafloor is generally older near the mid-ocean ridges.

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

Which theory explains the movement of the Earth's lithospheric plates?

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

Flashcards

Lithosphere

The outermost solid layer of Earth, composed of the crust and upper mantle.

Asthenosphere

The partially molten, flowing layer of the upper mantle, beneath the lithosphere.

Seafloor spreading

The process of new oceanic crust forming at mid-ocean ridges as magma rises and cools.

Plate tectonics

The theory that Earth's outer layer is made up of large, moving plates that interact at their boundaries.

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Convergent boundary

A boundary where two plates move towards each other, causing one to slide under the other.

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Transform boundary

A boundary where two plates slide past each other horizontally.

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Divergent boundary

A boundary where two plates move apart, creating new crust.

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Wilson cycle

The continuous cycle of Earth's crust being created, destroyed, and recycled through plate tectonic activity.

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Cascadia Subduction Zone

A zone where an oceanic plate is sliding beneath a continental plate, causing earthquakes and volcanoes.

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Bathymetry

The study of underwater depths and the topography of the seafloor.

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Continental Margin

The transition zone between the ocean floor and a continent, characterized by distinct features and geological processes.

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Passive Continental Margin

A passive margin forms when tectonic plates are moving apart, resulting in minimal seismic activity and gentle slopes. Examples include the eastern coast of North America.

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Active Continental Margin

An active margin forms at a convergent plate boundary where one plate pushes beneath another, creating high seismic activity and steep slopes. Examples include the western coast of South America.

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Deep Ocean Basins

The largest part of the ocean floor, characterized by flat abyssal plains, trenches, and seamounts.

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Mid-Ocean Ridges

The underwater mountain range where new oceanic crust is formed through volcanic activity and seafloor spreading.

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Weathering

The process of breaking down rocks into smaller particles, creating sediment.

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What is bathymetry?

The study of ocean depths and underwater features.

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What is a mid-ocean ridge?

Areas where tectonic plates are pulling apart, creating new ocean floor.

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What is the lysocline?

The depth at which calcium carbonate starts to dissolve. Below this depth, calcium carbonate doesn't accumulate due to dissolution.

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What is the CCD (carbonate compensation depth)?

The depth at which calcium carbonate completely dissolves, preventing accumulation of calcareous ooze.

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What is a subduction zone?

Areas where tectonic plates are colliding, leading to subduction and mountain formation.

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What is the Earth's crust?

The outermost layer of Earth, composed of solid, thin and brittle rocks. It is broken into tectonic plates.

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What is the Earth's mantle?

The layer beneath the crust, made of semi-solid, dense rock. It is much thicker than the crust.

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What is the Earth's outer core?

The liquid layer of Earth's core, primarily composed of iron and nickel.

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What is the Earth's inner core?

The solid, extremely dense center of the Earth, mainly composed of iron and nickel. The intense pressure keeps it solid.

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What is the lithosphere?

The rigid and strong outer layer of Earth, composed of the crust and upper mantle. It is broken into tectonic plates.

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What is the asthenosphere?

A semi-fluid layer in the upper mantle, where convection currents occur, driving tectonic plate movement.

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What is the rock cycle?

The process of rocks constantly changing from one form to another, driven by geological forces.

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What is the theory of plate tectonics?

The theory that Earth's lithosphere is divided into large plates that move and interact with each other, causing geological phenomena like earthquakes, volcanoes, and mountain building.

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Study Notes

Plate Tectonics and Rock Cycle

  • Earth's layers differ in state (solid, liquid) and thickness
  • Crust is solid and thin, mantle semi-solid and thick, outer core liquid, inner core solid (mostly iron & nickel)
  • Continental crust is thicker and less dense (mostly granite), oceanic crust thinner and denser (mostly basalt)
  • Lithosphere is solid and broken into plates, asthenosphere is semi-fluid and allows for movement
  • Igneous rocks form from cooled molten rock (e.g., basalt, granite)
  • Sedimentary rocks form from compacted & cemented sediments (e.g., sandstone, limestone)
  • Metamorphic rocks form from altered existing rocks under heat & pressure (e.g., marble, slate)

Plate Tectonics and Rock Cycle Relationships

  • Plate tectonics shapes Earth's surface (mountain building, subduction, volcanic activity) influencing rock formation, recycling, and alteration
  • Continental drift evidence includes similar fossils and geological features on different continents; matching rock formations
  • Seafloor spreading evidence includes the age of the seafloor (younger near ridges), magnetic striping patterns, and mid-ocean ridges
  • Plate tectonics theory describes Earth's lithosphere as divided into large plates that move on the semi-fluid asthenosphere, causing geological events (earthquakes, volcanoes, mountain formation)

Types of Plate Boundaries

  • Convergent boundaries: (e.g., subduction zones) plates move toward each other
  • Divergent boundaries: (e.g., mid-ocean ridges) plates move apart
  • Transform boundaries: (e.g., San Andreas Fault) plates slide past each other

Seafloor/Marine Provinces

  • Bathymetry: Measurement of ocean depth and underwater features, studied using sonar and satellite measurements
  • Passive continental margins are tectonically quiet; active margins are tectonically active with frequent earthquakes and volcanoes
  • Mid-ocean ridges have rift valleys, hydrothermal vents and large mountain chains
  • Sediments are particles of rock, minerals, and organic material, classified by source (terrestrial, biogenic, chemical) and size (clay, silt, sand, gravel)
  • Calcareous ooze is made of calcium carbonate (marine organisms); siliceous ooze is made of silica (diatoms and radiolarians)
  • Lysocline is the depth where calcium carbonate starts dissolving; Carbonate compensation depth (CCD) is the depth where calcareous ooze no longer accumulates

Additional Concepts

  • Wilson Cycle: describes the life cycle of ocean basins (opening, closing, supercontinent formation)
  • Studying the seafloor helps understand tectonic processes, ocean circulation, climate history, and marine ecosystems including resources (oil, gas, minerals)

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Unit 1 Study Guide PDF

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