two examples are the Juan de fuca and the north American plate.
two examples are the Juan de fuca and the north American plate.
it doesnt
The deepest portions of the subducting plate get pulled under by the subducted plate. This is how the trench is formed. this process is at work when any subduction occurs. An oceanic-continental subduction occurs when ocean crust sinks under continental crust. The oceanic crust sinks because it is colder and denser than the continental crust. At these sites, deep-ocean trenches form, along with coastal mountains.
Occurs when ocean crust sinks under continental crust, it sinks because it's colder and denser,at these sites, deep-ocean trenches also form along with coastal mountains. As the oceanic crust moves, these trenches often causes underwater earthquake, as the crust sinks under a continent, the crust buckles to form a range of mountains, like island arcs, parallel to a deep-ocean trench. Some of the mountains are volcanoes, which form as melted oceaninc crust rises through the top plate. For example: Cascade Mountains in Oregon and Washington.
When an oceanic plate collides with a continental plate, it results in the formation of coastal mountain ranges, such as the Andes in South America and the Cascades in North America. This collision causes the oceanic plate to subduct beneath the continental plate, leading to the uplift and deformation of the continental crust, forming high mountain ranges.
Coastal Mountains.
The Rockie Mountains are 4401 meters high whereas the coastal mountains are 4019 meters high so the Rockies are 382 meters higher than the coastal mountains
Appalachian mountains
applachian mountains
A continental interior refers to the central part of a continent, typically characterized by a lack of significant mountain ranges and a more stable geological structure compared to coastal areas. These regions often have a continental climate, with more extreme temperature variations and less precipitation than coastal areas. The continental interior can include plateaus, plains, and deserts, and is often less populated and developed than coastal regions. Examples include the Great Plains in North America and the Eurasian Steppe.
Volcanic eruptions and earthquakes.
Occurs when ocean crust sinks under continental crust, it sinks because it's colder and denser,at these sites, deep-ocean trenches also form along with coastal mountains. As the oceanic crust moves, these trenches often causes underwater earthquake, as the crust sinks under a continent, the crust buckles to form a range of mountains, like island arcs, parallel to a deep-ocean trench. Some of the mountains are volcanoes, which form as melted oceaninc crust rises through the top plate. For example: Cascade Mountains in Oregon and Washington.