A convergent boundary is where plates move together.
Tectonic plates come together at convergent boundaries. Some examples include the boundary between the Pacific Plate and the North American Plate along the west coast of the United States, where the plates are converging and creating the Cascade Range of mountains. Another example is the boundary between the Indian Plate and the Eurasian Plate, where the plates are colliding and creating the Himalayas.
The mid-ocean ridge is formed along a divergent or constructive plate boundary between two plates of oceanic crust.
Mt. Erubus has tectonic plates made up of parts of the lithosphere. These plates grind together or pull apart and this causes volcanoes to erupt.
A transform boundary. This is where tectonic plates slide horizontally past each other in opposite directions. This movement can cause earthquakes along the boundary.
The Nazca and Caribbean plates share a transform boundary. This boundary is characterized by horizontal motion where the two plates slide past each other in opposite directions. In this case, the plates are moving laterally along the Caribbean Plate's northern edge.
Tectonic plates
A divergent boundary occurs when tectonic plates move apart from one another. This movement creates new crust as magma rises from the mantle to fill the gap, leading to the formation of features like mid-ocean ridges.
That is a Strike-slip fault. This type of plate boundary is a relatively conservative boundary because the plates moves side by side horizontally causing little or no destruction of old plates or creation of new plates, but only causes a kind of boundary known as a Transform Boundary. An example of a transform boundary is the San Andreas fault, in California, USA North America.
tectonic plates?
You would most likely find a reverse fault at a convergent tectonic boundary, where two tectonic plates are colliding and one plate is being forced up and over the other. Reverse faults are characterized by vertical displacement and compression.
The Earth's plates are called tectonic plates.
The Nazca and Antarctic plates share a convergent tectonic boundary where the Nazca Plate is subducting beneath the Antarctic Plate. This results in volcanic activity and the formation of the Andes mountain range along the western coast of South America.