it is the study of making sanwhichs
A subduction zone occurs when one tectonic plate is forced underneath another, leading to the formation of deep oceanic trenches and volcanic arcs. In contrast, a continent-continent collision zone happens when two plates carrying continental crust collide, resulting in the uplift of mountain ranges and intense seismic activity.
A continent-continent collision occurs when two continental plates converge and push against each other. This collision can lead to mountain building, as seen in the collision between the Indian Plate and the Eurasian Plate that formed the Himalayas.
A subduction zone and a collision zone are the same place, a collision just happens earlier, when the crusts of the two plates are interacting. Later, when the crust of one plate is being forced under the crust of another plate into the mantle, it becomes a subduction zone.
Generally, subduction zones are formed when two plates collide and one is heavier than the other. When two continents collide, rather than one sinking, they will both be uplifted because they are light and buoyant.
An example of an active continent-continent collision is the ongoing collision between the Indian Plate and the Eurasian Plate, which has resulted in the formation of the Himalayan mountain range. This collision is causing the crust to thicken and uplift, leading to earthquakes and the continued growth of the Himalayas.
There are two basic types of convergent boundary. The first is a subduction zone, which occurs at a collision between two plates carry oceanic crust or one carrying continental and once carrying oceanic crust. In such a collision, one oceanic plate will subduct under the other and sink into the mantle. Such a collision produces volcanoes on the overriding plate and will produce mountain ranges on a continent. The other type of convergent boundary occurs when two continent collide. These collisions produce high mountains but not volcanoes. No subduction occurs as continental crust is not dense enough to sink into the mantle.
I can't give you a continent to continent but I can give you tectonic plate to tectonic plate. The Indian-Australian Plate is colliding with the Eurasian plate to form the Himalayan Mountains.
A continent-continent collision can produce large mountain ranges, such as the Himalayas formed by the collision between the Indian Plate and the Eurasian Plate. This collision typically results in intense folding and faulting of the Earth's crust, leading to the uplift of rocks and the creation of deep mountain roots.
a continent is made up of countries
Collision protects you and your car if you are in an accident, liability protects whomever you may hit.
collision is when two plates collide conservative is when two plates rub together
a region is a area a continent is a land mass