mainly continental volcanic arcs
Ocean convergence occurs when two ocean currents come together. This can lead to the uplift of deep water and the formation of upwelling zones, which can bring nutrients to the surface and support marine productivity.
When tectonic plates move closer together, it is called plate convergence. This can result in the formation of features like mountain ranges and deep ocean trenches.
The three types of convergence are geographic convergence (physical distance), technological convergence (integration of different technologies), and economic convergence (alignment of economies).
Wind stress curl is the change in wind direction and speed over a distance. It affects ocean circulation patterns by creating areas of convergence and divergence in the surface waters. This leads to the formation of ocean currents and the redistribution of heat and nutrients throughout the ocean.
In oceanic-continental convergence, the denser oceanic plate is forced beneath the continental plate in a process called subduction. This creates a deep ocean trench and can lead to volcanic activity and the formation of mountain ranges on the continental plate. The collision can also cause earthquakes.
Parallel belts of folded mountains and volcanic mountains
Parallel belts of folded mountains and volcanic mountains
Where ocean and continents meet
Ocean convergence occurs when two ocean currents come together. This can lead to the uplift of deep water and the formation of upwelling zones, which can bring nutrients to the surface and support marine productivity.
volcanic island arcs
At an ocean ocean convergent boundary, there will be a formation of volcanoes.
Ocean-continental convergent boundaries can produce earthquakes and volcanic activity. As the ocean plates shift under each other they near their melting temperature and can form magma and solidify to form underwater mountain ranges.
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Mountains like the Andes, fold mountains with Volcanoes,.
Ocean-continental convergent boundaries can produce earthquakes and volcanic activity. As the ocean plates shift under each other they near their melting temperature and can form magma and solidify to form underwater mountain ranges.
volcanic island arcs
Parallel belts of folded mountains and volcanic mountains