Plate boundaries where plates slide past each other are known by what name?
AConvergent Boundary
BDivergent Boundary
CTransform Boundary
DSubduction Zone
Answer:
C. Transform Boundary
Read Explanation:
Transform Boundaries
Transform plate boundaries are one of the three main types of plate boundaries. At these boundaries, tectonic plates slide horizontally past one another.
Key Characteristics:
Sliding Motion: Unlike convergent (colliding) or divergent (separating) boundaries, the movement here is primarily lateral.
No Crust Creation or Destruction: Significant amounts of new crust are not formed, nor is existing crust destroyed.
Faults: These boundaries are characterized by large transform faults, which are zones where the rocks are fractured and displaced.
Earthquakes: Transform boundaries are the sites of frequent and sometimes significant earthquakes. This is because the plates get locked, stress builds up, and then is suddenly released.
Famous Examples:
San Andreas Fault (California, USA): This is the most well-known example, marking the boundary between the Pacific Plate and the North American Plate.
Alpine Fault (New Zealand): A major transform fault that runs through the South Island.
North Anatolian Fault (Turkey): Responsible for numerous earthquakes in Turkey.
Significance in Plate Tectonics:
Transform faults often connect segments of mid-ocean ridges or other plate boundaries.
They play a crucial role in accommodating the differential movement of larger tectonic plates.
Exam Relevance:
Understanding the three types of plate boundaries (convergent, divergent, transform) and their associated geological features (mountains, volcanoes, trenches, earthquakes, faults) is fundamental for geography and earth science exams.
Knowledge of specific examples like the San Andreas Fault is often tested.
