Podcast
Questions and Answers
Which of the following is a characteristic of active continental margins?
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.
The Wilson Cycle describes the life cycle of mountain ranges.
False (B)
What are two ways that sediments can be classified?
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 ______.
The depth at which calcium carbonate starts to dissolve is called the ______.
Match the following sediment types with their primary composition:
Match the following sediment types with their primary composition:
What is the primary force shaping the seabed, alongside erosion and deposition?
What is the primary force shaping the seabed, alongside erosion and deposition?
Passive continental margins are characterized by frequent earthquakes and volcanic activity.
Passive continental margins are characterized by frequent earthquakes and volcanic activity.
What is bathymetry?
What is bathymetry?
The Cascadia Subduction Zone is an example of an ______ plate boundary.
The Cascadia Subduction Zone is an example of an ______ plate boundary.
Match the sediment type with its primary material:
Match the sediment type with its primary material:
Which of the following is a key feature of a passive continental margin?
Which of the following is a key feature of a passive continental margin?
The Earth's outer core is solid.
The Earth's outer core is solid.
What can grain size and shape in sediments tell us about the depositional environment?
What can grain size and shape in sediments tell us about the depositional environment?
Which type of rock is formed from the cooling and solidification of molten magma or lava?
Which type of rock is formed from the cooling and solidification of molten magma or lava?
The asthenosphere is a rigid layer of the Earth located above the lithosphere.
The asthenosphere is a rigid layer of the Earth located above the lithosphere.
What is the name of the process by which sediments become solid rock?
What is the name of the process by which sediments become solid rock?
A __ is a deep, underwater feature typically found at subduction zones where one plate is forced beneath the other.
A __ is a deep, underwater feature typically found at subduction zones where one plate is forced beneath the other.
Match the following plate boundary type with the geological features or activity typically associated with them:
Match the following plate boundary type with the geological features or activity typically associated with them:
Which of the following is a common feature found at divergent plate boundaries?
Which of the following is a common feature found at divergent plate boundaries?
The Wilson Cycle describes the opening and closing of ocean basins.
The Wilson Cycle describes the opening and closing of ocean basins.
What is the name for a volcano that forms over a relatively stationary mantle plume?
What is the name for a volcano that forms over a relatively stationary mantle plume?
Which layer of the Earth is primarily liquid?
Which layer of the Earth is primarily liquid?
Oceanic crust is thicker and less dense than continental crust.
Oceanic crust is thicker and less dense than continental crust.
What is the semi-fluid layer beneath the lithosphere that allows tectonic plate movement?
What is the semi-fluid layer beneath the lithosphere that allows tectonic plate movement?
_______ rocks form from the cooling and solidification of molten rock.
_______ rocks form from the cooling and solidification of molten rock.
Match the plate boundary type with its description:
Match the plate boundary type with its description:
What is a key piece of evidence supporting continental drift?
What is a key piece of evidence supporting continental drift?
The age of the seafloor is generally older near the mid-ocean ridges.
The age of the seafloor is generally older near the mid-ocean ridges.
Which theory explains the movement of the Earth's lithospheric plates?
Which theory explains the movement of the Earth's lithospheric plates?
Flashcards
Lithosphere
Lithosphere
The outermost solid layer of Earth, composed of the crust and upper mantle.
Asthenosphere
Asthenosphere
The partially molten, flowing layer of the upper mantle, beneath the lithosphere.
Seafloor spreading
Seafloor spreading
The process of new oceanic crust forming at mid-ocean ridges as magma rises and cools.
Plate tectonics
Plate tectonics
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Convergent boundary
Convergent boundary
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Transform boundary
Transform boundary
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Divergent boundary
Divergent boundary
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Wilson cycle
Wilson cycle
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Cascadia Subduction Zone
Cascadia Subduction Zone
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Bathymetry
Bathymetry
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Continental Margin
Continental Margin
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Passive Continental Margin
Passive Continental Margin
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Active Continental Margin
Active Continental Margin
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Deep Ocean Basins
Deep Ocean Basins
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Mid-Ocean Ridges
Mid-Ocean Ridges
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Weathering
Weathering
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What is bathymetry?
What is bathymetry?
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What is a mid-ocean ridge?
What is a mid-ocean ridge?
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What is the lysocline?
What is the lysocline?
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What is the CCD (carbonate compensation depth)?
What is the CCD (carbonate compensation depth)?
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What is a subduction zone?
What is a subduction zone?
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What is the Earth's crust?
What is the Earth's crust?
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What is the Earth's mantle?
What is the Earth's mantle?
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What is the Earth's outer core?
What is the Earth's outer core?
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What is the Earth's inner core?
What is the Earth's inner core?
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What is the lithosphere?
What is the lithosphere?
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What is the asthenosphere?
What is the asthenosphere?
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What is the rock cycle?
What is the rock cycle?
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What is the theory of plate tectonics?
What is the theory of plate tectonics?
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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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