32. Plate boundaries 33. Convergent 34. Divergent 35 Transform

It seems like you're listing types of plate boundaries in geology. Let's break down each type: ### 1. Plate Boundaries Plate boundaries are the edges where two tectonic plates meet. The interactions at these boundaries are responsible for many geological phenomena, including earthquakes, volcanic activity, and the formation of mountain ranges. ### 2. Convergent Boundaries - **Definition**: Convergent boundaries occur where two tectonic plates move toward each other. - **Characteristics**: - One plate may be forced beneath another in a process called subduction. - This can lead to the formation of mountain ranges, deep ocean trenches, and volcanic arcs. - **Examples**: The Himalayas (formed by the collision of the Indian and Eurasian plates) and the Mariana Trench (formed by the subduction of the Pacific Plate beneath the Mariana Plate). ### 3. Divergent Boundaries - **Definition**: Divergent boundaries occur where two tectonic plates move away from each other. - **Characteristics**: - This movement creates new oceanic crust as magma rises to the surface. - It often results in mid-ocean ridges and rift valleys. - **Examples**: The Mid-Atlantic Ridge (where the Eurasian and North American plates are moving apart) and the East African Rift. ### 4. Transform Boundaries - **Definition**: Transform boundaries occur where two tectonic plates slide past one another horizontally. - **Characteristics**: - This lateral movement can cause earthquakes. - Unlike convergent and divergent boundaries, transform boundaries do not typically create or destroy crust. - **Examples**: The San Andreas Fault in California and the North Anatolian Fault in Turkey. If you have specific questions or need further details about any of these types of plate boundaries, feel free to ask!