7 - Tectonics and Internal Earth Processes Flashcards
This part of the deck delves into the theory of plate tectonics, the driving force behind many of Earth's geological processes. You'll learn about the different types of plate boundaries, such as divergent, convergent, and transform boundaries, and how these boundaries influence the formation of mountains, earthquakes, and volcanic eruptions. Additionally, you'll explore the concept of seafloor spreading and continental drift. (39 cards)
Identify:
What theory explains Earth’s plate movement?
plate tectonics
This theory describes the movement of Earth’s tectonic plates, causing geological phenomena like earthquakes, volcanic eruptions, and mountain building.
Define:
lithosphere
The rigid outer layer of Earth, made up of the crust and upper mantle.
The lithosphere is divided into tectonic plates that float on the more fluid asthenosphere beneath.
Define:
tectonic plate
A rigid section of Earth’s lithosphere moving on the asthenosphere.
These plates move due to mantle convection and interact at plate boundaries.
Explain:
3 types of plate boundary interactions
- Divergent Boundaries
- Convergent Boundaries
- Transform Boundaries
Divergent Boundaries: Plates move apart, creating new crust as magma rises to the surface (e.g., mid-ocean ridges).
Convergent Boundaries: Plates move toward each other, causing subduction or mountain formation.
Transform Boundaries: Plates slide past one another, often causing earthquakes.
Explain:
What geological features form at convergent boundaries?
- Mountain Ranges
- Ocean Trenches
- Volcanic Arcs
Mountain Ranges: Formed when continental plates collide and compress.
Ocean Trenches: Formed as an oceanic plate is subducted beneath another plate, creating deep depressions.
Volcanic Arcs: Formed above subduction zones as one plate descends into the mantle, creating chains of volcanoes.
Identify:
What geological feature forms at land-based divergent boundaries?
rift valleys
Rift valleys are formed when tectonic plates separate on land, such as in the East African Rift.
Define:
transform boundary
Type of plate boundary where two tectonic plates slide past each other horizontally.
The San Andreas Fault in California is an example of a transform boundary, causing frequent earthquakes.
Identify:
What geological feature is associated with transform boundaries?
strike-slip faults
These faults occur when plates slide horizontally past each other, often resulting in earthquakes.
Explain:
How do earthquakes occur at transform boundaries?
Friction between sliding plates causes seismic energy release.
At transform boundaries, plates slide past each other, causing friction to build up. This energy is suddenly released along faults, making these areas prone to frequent earthquakes.
Identify:
What is the primary driving force behind tectonic plate movement?
mantle convection
Mantle convection provides the necessary heat and motion to drive the movement of tectonic plates over the Earth’s surface.
Define:
ridge push
The force from elevated mid-ocean ridges pushing plates away.
It occurs as the lithosphere at divergent boundaries is pushed upwards, creating a slope that moves plates outward.
Identify:
What tectonic feature is associated with ridge push?
mid-ocean ridges
Mid-ocean ridges are where seafloor spreading occurs, and ridge push helps to drive plates apart at divergent boundaries.
Identify:
What force pulls a subducting plate into the mantle?
slab pull
Slab pull occurs at convergent boundaries where one plate is subducted beneath another.
Identify:
Where does slab pull primarily occur?
At convergent boundaries, particularly at subduction zones.
Subduction zones are areas where oceanic plates are pulled beneath continental plates, a process that generates significant tectonic forces.
Explain:
How do tectonic plates influence the formation of mountain ranges?
Colliding plates push the crust upward.
Mountain ranges form at convergent boundaries where tectonic plates collide, compressing and uplifting the crust. The Himalayas are an example, created by the collision of the Indian and Eurasian Plates.
Identify:
Which type of plate boundary is most likely to cause mountain building?
convergent boundaries
Convergent boundaries cause compressional stress, leading to the uplift of mountain ranges.
Define:
convection currents
- Process that involves the movement of energy from one place to another.
- Also called convection heat transfer.
These currents transfer heat from the Earth’s core, causing mantle flow and driving plate movements.
Define:
What is a fold in geology?
A bend in rock layers caused by compressional forces.
Folds form when rocks are subjected to stress, causing them to bend without breaking.
Identify:
What fold arches upward with oldest layers at its core?
anticline
Anticlines are typically formed by compressional stress and are found in mountain ranges.
Define:
syncline
A fold that sinks downward with youngest layers at its core.
Synclines are often found alongside anticlines in mountain ranges.
Define:
fault
A crack in Earth’s crust where movement occurs.
Faults form when stress builds up in the crust, causing rocks to break and slide past each other.
Explain:
3 main types of faults
- Normal Fault
- Reverse Fault
- Strike-Slip Fault
Normal Fault: Forms when tension stretches the crust, causing the hanging wall to move downward.
Reverse Fault: Occurs under compression, pushing the hanging wall upward relative to the footwall.
Strike-Slip Fault: Results from shear stress, where blocks slide past each other horizontally.
Explain:
2 characteristics of normal faults
- Vertical Movement
- Hanging Wall and Footwall
Vertical Movement: In a normal fault, the movement is primarily vertical.
Hanging Wall and Footwall: The block of rock above the fault plane is called the hanging wall, and the block below is called the footwall. In a normal fault, the hanging wall moves downward relative to the footwall.
Normal faults typically form at divergent boundaries where plates pull apart.
Explain:
2 characteristics of reverse faults
- Compressional Forces
- Hanging Wall Moves Up
Compressional Forces: Reverse faults are formed by compressional forces, meaning forces that push or squeeze the Earth’s crust together.
Hanging Wall Moves Up: In a reverse fault, the hanging wall (the block of rock above the fault plane) moves upward relative to the footwall (the block of rock below the fault plane).
Reverse faults form under compressional stress, usually at convergent boundaries.