If you're looking at a convection zone along coastal areas you'll look for subduction zones, trenches, accretionary wedges, volcanic activity, seismic activity, mountain building activity, island creation (think Japan), and possibly exotic terrains to name a few. If you're looking at convergent boundaries on continental land you'll generally find mountain building (think Himalayas), faulting, and seismic activity; not as much volcanism here since the crust is even think to support the mountain zone.
There isn't specifically one feature to be found because you have three options for convergent boundaries: continental-oceanic, continental-continental, and oceanic-oceanic.
Generally (I think probably always), a mountain range develops at a convergent boundary.
They can be associated with both, but are most often found near convergent boundaries.
Topographical features that can be found along convergent boundaries include mountain ranges, deep ocean trenches, and volcanic arcs. These features are a result of the intense tectonic forces that push plates together, causing them to collide or subduct beneath one another.
Convergent
There are 3 types of Convergent boundaries, they are; 1. Continental-continental convergent boundary. 2. Continental-oceanic convergent boundary. 3. Oceanic-oceanic convergent boundary.
Convergent boundary.
convergent boundary -rift valley divergent boundary -mid-ocean ridge
Composite cone
A convergent boundary causes compressional stress.
At a convergent boundary, landforms such as mountains, deep ocean trenches, and volcanic arcs can be found. Tectonic activity includes the subduction of one plate under another, leading to the formation of these features. Earthquakes and volcanic eruptions are also common at convergent boundaries.
convergent boundaries are easy to find most of them are found in the ocean. One Famous convergent plate boundary would be the Sunda Double Trench. It is found in the Indian ocean and it reaches a depth of 24,440 feet. It is the deepest trench in the Indian Ocean.
The Himalayas are found at a convergent plate boundary also known as a subduction zone where one plate slips under the other driving the land mass up.