Plate Tectonics and Boundaries Quiz

Plate tectonics is a theory explaining Earth's surface is divided into large and small plates, contributing to geological activity like earthquakes, volcanism, and mountain building.
Plate boundaries are the lines where lithospheric plates meet, with interactions creating various geological phenomena.

Occur when two tectonic plates move apart, creating tension.
New crust forms as magma rises from the mantle and solidifies, also known as constructive boundaries.
Mid-ocean ridges and continental rift valleys are formed through divergence.
Example: Mid-Atlantic Ridge, where the Eurasian and North American plates are moving apart.

Form when two plates move toward each other, resulting in three types:
- Oceanic-Continental Boundary: Oceanic plate subducts beneath continental plate, causing volcanic activity and mountain formation.
- Oceanic-Oceanic Boundary: One oceanic plate subducts under another, resulting in island volcanic chains parallel to trenches.
- Continental-Continental Boundary: Plates collide, causing compression and crumpling, leading to mountain ranges.
Example: Himalayas formed by the collision of the Indian and Eurasian plates.

Occur when two tectonic plates slide past one another, also known as strike-slip faults.
Movement results in splitting rocks along the boundary, forming features like undersea canyons or linear fault valleys.
Example: San Andreas Fault in California, where the Pacific Plate and North American Plate slide past each other.

Different boundary types lead to distinct geological features and processes.
Areas near plate boundaries are more susceptible to earthquakes, volcanic activity, and mountain formation.

Divergent boundaries create new crust as plates separate (e.g., Mid-Atlantic Ridge).
Convergent boundaries involve plates colliding, resulting in subduction or mountain formation.
Transform boundaries involve lateral movement of plates, leading to faults such as the San Andreas Fault.

Understanding the movement direction of plates assists in identifying boundary types:
- Divergent: Plates move apart.
- Convergent: Plates move together.
- Transform: Plates slide past each other.
Key processes: Subduction (downward bending of oceanic plates) and compression (crumpling of continental plates).

Earth's surface is divided into large and small tectonic plates, influencing geological activities like earthquakes, volcanism, and mountain building.
Plate boundaries mark the intersection between lithospheric plates, where various geological phenomena arise from interactions.

Plates move apart, leading to tension and the creation of new crust.
Magma from the mantle rises and solidifies at these boundaries, classified as constructive.
Features include mid-ocean ridges and continental rift valleys.
Example: The Mid-Atlantic Ridge, formed by the divergence of the Eurasian and North American plates.

Plates move toward one another, resulting in three scenarios:
- Oceanic-Continental Boundary: The oceanic plate subducts beneath the continental plate, causing volcanic activity and mountain formation.
- Oceanic-Oceanic Boundary: One oceanic plate subducts under another, forming island volcanic chains parallel to ocean trenches.
- Continental-Continental Boundary: Collision leads to significant compression and the formation of mountain ranges.
Example: The Himalayas, created by the collision of the Indian and Eurasian plates.

Plates slide past one another, producing strike-slip faults.
Movement results in features like undersea canyons and linear fault valleys.
Example: The San Andreas Fault in California, where the Pacific Plate and North American Plate interact.

Unique geological features and processes emerge from different boundary types.
Regions near plate boundaries experience heightened risks of earthquakes, volcanic eruptions, and mountain formation.

Divergent boundaries contribute to new crust formation (e.g., Mid-Atlantic Ridge).
Convergent boundaries involve plate collisions that can lead to subduction or mountain range development.
Transform boundaries facilitate lateral movement resulting in faults like the San Andreas Fault.

Direction of plate movement helps identify boundary types:
- Divergent: Plates separate.
- Convergent: Plates collide.
- Transform: Plates slide laterally.
Key processes include subduction (downward movement of oceanic plates) and compression (crumpling of continental plates).