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These active margins can be convergent or transform margins, and are also places of high tectonic activity, including volcanoes and earthquakes. The West Coast of North America and South America are active margins. [4] Active continental margins are typically narrow from coast to shelf break, with steep descents into trenches. [4] Convergent ...
The continental shelf and the slope are part of the continental margin. [ 6 ] The shelf area is commonly subdivided into the inner continental shelf , mid continental shelf , and outer continental shelf , [ 7 ] each with their specific geomorphology [ 8 ] [ 9 ] and marine biology .
Continental volcanic arc and cordilleran orogen; Adjacent continental masses located along strike (such as Barbados). Material transported into the trench by gravity sliding and debris flow from the forearc ridge (olistostrome) Piggy-back basins, which are small basins located in surface depression on the accretionary prism.
A continental arc is a type of volcanic arc occurring as an "arc-shape" topographic high region along a continental margin.The continental arc is formed at an active continental margin where two tectonic plates meet, and where one plate has continental crust and the other oceanic crust along the line of plate convergence, and a subduction zone develops.
The Cascade Range is formed by an active continental margin. A slice of the Earth from the Pacific Ocean through the Pacific Northwest might look something like the adjacent image. Beneath the Cascades, a dense oceanic plate plunges beneath the North American plate; a process known as subduction. As the oceanic slab sinks deep into the Earth's ...
Since Chile is on an active continental margin, it has many volcanoes. Almost the entire country is subject to earthquakes arising from strains in the Nazca and Antarctic plates or shallow strike-slip faults. Northern Chilean mineral resources are a major economic resource, and the country is the leading producer of copper, lithium and molybdenum.
Orogeny (/ ɒ ˈ r ɒ dʒ ə n i /) is a mountain-building process that takes place at a convergent plate margin when plate motion compresses the margin. An orogenic belt or orogen develops as the compressed plate crumples and is uplifted to form one or more mountain ranges.
Examples of dacitic magmatism in active continental margins are the Cascade Range, Guatemala and the Andes (Ecuador, Peru and Chile). In continental volcanic series, often in association with tholeiitic basalts and intermediary rocks; The type locality of dacite is Gizella quarry near Poieni, Cluj in Romania. [1]