Answer: Here's a summary of the types of plate boundaries using the Frayer Model:1. Convergent Plate BoundariesDefinition: Places where two tectonic plates move towards each other.Characteristics: Often leads to subduction (one plate sliding beneath another), mountain formation, and volcanic activity.Examples: The boundary between the Pacific Plate and the North American Plate (Cascadia Subduction Zone), and the boundary between the Indian Plate and the Eurasian Plate (Himalayas).Non-Examples: Divergent or transform-fault boundaries where plates move away from or past each other.2. Divergent Plate BoundariesDefinition: Locations where two tectonic plates move away from each other.Characteristics: Typically results in seafloor spreading, formation of mid-ocean ridges, and rift valleys.Examples: The Mid-Atlantic Ridge and the East African Rift.Non-Examples: Convergent or transform-fault boundaries where plates move towards or past each other.3. Transform-Fault Plate BoundariesDefinition: Zones where two plates slide past each other horizontally.Characteristics: Can cause earthquakes and form transform faults.Examples: The San Andreas Fault in California and the North Anatolian Fault in Turkey.Non-Examples: Convergent or divergent boundaries where plates move towards or away from each other.4. Importance of Understanding Plate BoundariesDefinition: Knowledge of plate boundaries helps us understand geological processes and risks.Characteristics: Essential for predicting earthquakes, volcanic eruptions, and understanding mountain-building processes. Helps in planning and disaster preparedness.Examples: Earthquake forecasting, volcanic eruption prediction, and assessing areas prone to natural disasters.Non-Examples: Unrelated to purely internal processes of a plate or isolated geological features not associated with plate movement.This model organizes the types of plate boundaries, highlights their characteristics, and emphasizes the importance of understanding them in the context of geological and environmental studies.