Convergent Boundaries:
Convergent boundaries occur when two tectonic plates collide or move towards each other. There are three types of convergent boundaries:

1. Oceanic-Continental Convergence: This occurs when an oceanic plate collides with a continental plate. The denser oceanic plate subducts beneath the less dense continental plate, forming a trench. This process can lead to the formation of volcanic arcs and mountain ranges, such as the Andes in South America.

2. Oceanic-Oceanic Convergence: In this case, two oceanic plates collide. One plate usually subducts beneath the other, forming a trench. The subduction can lead to the formation of volcanic islands, such as the Japanese archipelago.

3. Continental-Continental Convergence: When two continental plates collide, neither plate subducts because they have similar densities. Instead, the collision leads to the formation of large mountain ranges, such as the Himalayas.

Divergent Boundaries:
Divergent boundaries occur when two tectonic plates move away from each other. This movement creates tension and allows magma to rise from the mantle, creating new crust. There are two types of divergent boundaries:

1. Oceanic Divergence: This occurs when two oceanic plates move apart. As the plates separate, magma rises to fill the gap, creating a mid-ocean ridge. The most well-known example of this is the Mid-Atlantic Ridge.

2. Continental Divergence: When two continental plates move apart, a rift valley is formed. Over time, this rift valley can widen and fill with water, eventually becoming a new ocean. The East African Rift Valley is an example of continental divergence.

Transform Boundaries:
Transform boundaries occur when two tectonic plates slide past each other horizontally. These boundaries are characterized by frequent earthquakes. The most famous example of a transform boundary is the San Andreas Fault in California.

Resurgent Boundaries:
Resurgent boundaries are not an example of plate boundaries formed by the interaction of the Earth's tectonic plates. This term is not commonly used in geology and does not represent a recognized type of plate boundary.